<?xml version='1.0' encoding='UTF-8'?><?xml-stylesheet href="http://www.blogger.com/styles/atom.css" type="text/css"?><feed xmlns='http://www.w3.org/2005/Atom' xmlns:openSearch='http://a9.com/-/spec/opensearchrss/1.0/' xmlns:blogger='http://schemas.google.com/blogger/2008' xmlns:georss='http://www.georss.org/georss' xmlns:gd="http://schemas.google.com/g/2005" xmlns:thr='http://purl.org/syndication/thread/1.0'><id>tag:blogger.com,1999:blog-5371504585591558867</id><updated>2024-10-01T23:32:48.383-07:00</updated><category term="Philippines"/><category term="Philippine Volcanoes"/><category term="active volcano"/><category term="popular hiking destination"/><category term="stratovolcano"/><category term="eruptions"/><category term="island of Luzon"/><category term="island of Mindanao"/><category term="volcano"/><category term="Cagayan"/><category term="Davao City"/><category term="Luzon Island"/><category term="Luzon in the Philippines"/><category term="Republic of the Philippines"/><category term="earthquakes"/><category term="hiking destination"/><category term="hiking trail"/><category term="mountain climbing"/><category term="mountain range"/><category term="volcanic activity"/><category term="Aetas"/><category term="Albay"/><category term="Albay Province"/><category term="Babuyan Channel"/><category term="Babuyan Claro"/><category term="Bacun mountain trio"/><category term="Balintang Channel"/><category term="Bataan Peninsula"/><category term="Benguet"/><category term="Bicol"/><category term="Bicol Region"/><category term="Bulusan Volcano"/><category term="Cagayan Valley"/><category term="Cagua"/><category term="Cagua Volcano"/><category term="Camarines Sur"/><category term="Camiguin"/><category term="Camping"/><category term="Canlaon Volcano"/><category term="Canlaon&#39;s eruption"/><category term="Didicas Volcano"/><category term="Iraya Volcano"/><category term="Iriga Vocano"/><category term="Island of Marinduque"/><category term="K-Ar dates"/><category term="Laguna"/><category term="Lake Buhi"/><category term="Lake Danao"/><category term="Lake Leonard"/><category term="Lenten Season"/><category term="Leonard Kniazeff"/><category term="Leonard Range"/><category term="Luzon"/><category term="Malabsay Falls"/><category term="Mayon Volcano"/><category term="Misamis Occidental"/><category term="Mount Arayat"/><category term="Mount Arayat National Park"/><category term="Mount Asog"/><category term="Mount Bulusan"/><category term="Mount Iriga"/><category term="Mount Isarog"/><category term="Mount Limay"/><category term="Mount Malindang"/><category term="Mount Malindig"/><category term="Mount Slamet"/><category term="Mt. Apo"/><category term="Mt. Babuyan"/><category term="Mt. Banahaw"/><category term="Mt. Didicas"/><category term="Mt. Hibok-Hibok"/><category term="Mt. Iriga"/><category term="Mt. Kabunian"/><category term="Mt. Makiling"/><category term="Mt. Malinao"/><category term="Mt. Mayon"/><category term="Mt. Palali"/><category term="Mt. Palali Volcano"/><category term="Mt. Palali in Nueva Vizcaya"/><category term="Mt. Pinatubo"/><category term="Mt. Pinatubo Lake"/><category term="Nabuntalan Falls"/><category term="Negros Island"/><category term="PHILVOLCS"/><category term="Panicuason Trail"/><category term="Patag-Patag Trail"/><category term="Philippine Fault"/><category term="Pocdol Mountains"/><category term="Taal Lake"/><category term="Taal Volcano"/><category term="Vera Falls"/><category term="White Rock"/><category term="Zambales Mountains"/><category term="Zamboanga del Norte"/><category term="Zamboanga del Sur"/><category term="active"/><category term="ash deposits"/><category term="assymetrical cone"/><category term="burial place"/><category term="catchment"/><category term="climbing destination"/><category term="complex volcano"/><category term="compound volcano"/><category term="crater-lake"/><category term="dormant volcano"/><category term="endemic and endangered species"/><category term="eruption"/><category term="exploring nature"/><category term="forest"/><category term="four craters"/><category term="fumarole"/><category term="geothermal energy"/><category term="geothermal exploration program"/><category term="great challenge to mountain climbers"/><category term="group of volcanic cones"/><category term="highest mountain"/><category term="highest peak"/><category term="horseback riding"/><category term="hot springs"/><category term="inactive volcano"/><category term="island in a like on an island in a lake on an island"/><category term="lahar"/><category term="most active volcano"/><category term="most popular climb and hike on the island"/><category term="mountaineers"/><category term="multiple vents"/><category term="mysterious"/><category term="mystical mountain"/><category term="new island formation"/><category term="perfect cone shape"/><category term="pilgrimage site"/><category term="popular tourist destination"/><category term="potentially active volcano"/><category term="pyroclastic flow"/><category term="sacred volcano"/><category term="spectacular vista of the entire island"/><category term="stratovolcanos"/><category term="sunsets in Manila"/><category term="trekking"/><category term="volcanic complex"/><category term="volcanic edifice"/><category term="volcaninc eruptions"/><category term="volcano with a river"/><category term="volcano-caldera"/><category term="volcanoes in Bicol"/><category term="volcanoes in Laguna"/><category term="volcanoes in Sorsogon"/><category term="volcanologists"/><category term="wild goats"/><category term="wooden coffins"/><category term="world&#39;s smallest sctive volcano"/><title type='text'>VOLCANOES IN THE PHILIPPINES</title><subtitle type='html'>Magnificent and awesome volcanoes in the wonderful country of the Philippines!</subtitle><link rel='http://schemas.google.com/g/2005#feed' type='application/atom+xml' href='http://philippinevolcanoes.blogspot.com/feeds/posts/default'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default?redirect=false'/><link rel='alternate' type='text/html' href='http://philippinevolcanoes.blogspot.com/'/><link rel='hub' href='http://pubsubhubbub.appspot.com/'/><link rel='next' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default?start-index=26&amp;max-results=25&amp;redirect=false'/><author><name>Unknown</name><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='https://img1.blogblog.com/img/b16-rounded.gif'/></author><generator version='7.00' uri='http://www.blogger.com'>Blogger</generator><openSearch:totalResults>27</openSearch:totalResults><openSearch:startIndex>1</openSearch:startIndex><openSearch:itemsPerPage>25</openSearch:itemsPerPage><entry><id>tag:blogger.com,1999:blog-5371504585591558867.post-2232111515292695790</id><published>2017-03-28T14:59:00.000-07:00</published><updated>2017-03-28T14:59:01.840-07:00</updated><category scheme="http://www.blogger.com/atom/ns#" term="hiking destination"/><category scheme="http://www.blogger.com/atom/ns#" term="hiking trail"/><category scheme="http://www.blogger.com/atom/ns#" term="mountain climbing"/><category scheme="http://www.blogger.com/atom/ns#" term="Mt. Palali"/><category scheme="http://www.blogger.com/atom/ns#" term="Mt. Palali in Nueva Vizcaya"/><category scheme="http://www.blogger.com/atom/ns#" term="Mt. Palali Volcano"/><category scheme="http://www.blogger.com/atom/ns#" term="popular hiking destination"/><category scheme="http://www.blogger.com/atom/ns#" term="volcano"/><title type='text'>MT. PALALI IN NUEVA VIZCAYA</title><content type='html'>&lt;div class=&quot;separator&quot; style=&quot;clear: both; text-align: center;&quot;&gt;
&lt;a href=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhfXscXhH7Ood4UVAVjhOXb_OdFw0P14CYxfD5wzbipBm6GaHg7dTk2OBodU5xhVa9VXyz9hq7ql1cbj3Equu4oNzJ_0hwmyHXjnIg2PbZIrhfJiPSipg4Te7pAnyzHxRJaIySdessIB8E/s1600/0+click.jpg&quot; imageanchor=&quot;1&quot; style=&quot;margin-left: 1em; margin-right: 1em;&quot;&gt;&lt;img border=&quot;0&quot; height=&quot;39&quot; src=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhfXscXhH7Ood4UVAVjhOXb_OdFw0P14CYxfD5wzbipBm6GaHg7dTk2OBodU5xhVa9VXyz9hq7ql1cbj3Equu4oNzJ_0hwmyHXjnIg2PbZIrhfJiPSipg4Te7pAnyzHxRJaIySdessIB8E/s320/0+click.jpg&quot; width=&quot;320&quot; /&gt;&lt;/a&gt;&lt;/div&gt;
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&lt;a href=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiLTKfH2mWKX53DRFFysfrONWwOUmiV0LOm6EOUq8CQbEdhe1YeUBt_J0Lem4dQnCaqZKVRus6lRaPZadMBnRmIEJ12161Lya4UtM11R9ZdGMPk_1dFekP_KdIKpsclhb94bXRhgSfM8mU/s1600/Mt.+Palali.jpg&quot; imageanchor=&quot;1&quot; style=&quot;margin-left: 1em; margin-right: 1em;&quot;&gt;&lt;img border=&quot;0&quot; height=&quot;390&quot; src=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiLTKfH2mWKX53DRFFysfrONWwOUmiV0LOm6EOUq8CQbEdhe1YeUBt_J0Lem4dQnCaqZKVRus6lRaPZadMBnRmIEJ12161Lya4UtM11R9ZdGMPk_1dFekP_KdIKpsclhb94bXRhgSfM8mU/s640/Mt.+Palali.jpg&quot; width=&quot;640&quot; /&gt;&lt;/a&gt;&lt;/div&gt;
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&lt;span style=&quot;color: #990000; font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif; font-size: x-small;&quot;&gt;&lt;a href=&quot;https://www.vigattintourism.com/index.php?/tourism/articles/Mount-Palali&quot;&gt;Source&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;A little-known but very beautiful destination in Northern Luzon is Mt. Palali in Nueva Vizcaya. Once the hunting ground of the Bugkalots, Gaddangs, and Ifugaos, this majestic mountain offers a commanding view of the low-lying municipalities of the province.&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;The jump-off point is accessible through tricycles or jeeps less than 30 minutes from Solano. Getting guides, however, seem to be quite a challenge but the risk of going there without prior arrangement is a fair-enough risk, as Mt. Palali gets more and more popular as a climbing destination. The trail begins as a rough road, as in many mountains, and it gives way to a beautiful forest. This forest has recently been declared as a ‘protected area’ and should be respected as such. There are many avian species; indeed the forest is the closest most of us can get to the deep jungles of Palanan, farther east.&amp;nbsp; -&amp;nbsp; &lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif; font-size: x-small;&quot;&gt;&lt;i&gt;&lt;a href=&quot;http://www.pinoymountaineer.com/2007/09/mt-palali-1715.html&quot;&gt;http://www.pinoymountaineer.com/2007/09/mt-palali-1715.html&lt;/a&gt;&lt;/i&gt;&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot;; font-size: x-small;&quot;&gt;&lt;a href=&quot;http://www.traveltothephilippines.info/2013/07/16/the-protected-forests-of-mt-palali-in-nueva-vizcaya/&quot;&gt;Source&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;
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&lt;a href=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgY3QwF172A4bS8HUTwXxYCE7xw3kmKEih15HP3G4CTkc8IhUMnaK_6Hgd4OqdX5J4hNJlxm4oNQvHuY2KLPFmFtHReooXyWgjezcVmZ9WYGyfLR0f218mLHSIsD_lkJcS0X8HQ0NwadQw/s1600/Mt.+Palali3.jpg&quot; imageanchor=&quot;1&quot; style=&quot;margin-left: 1em; margin-right: 1em;&quot;&gt;&lt;img border=&quot;0&quot; height=&quot;480&quot; src=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgY3QwF172A4bS8HUTwXxYCE7xw3kmKEih15HP3G4CTkc8IhUMnaK_6Hgd4OqdX5J4hNJlxm4oNQvHuY2KLPFmFtHReooXyWgjezcVmZ9WYGyfLR0f218mLHSIsD_lkJcS0X8HQ0NwadQw/s640/Mt.+Palali3.jpg&quot; width=&quot;640&quot; /&gt;&lt;/a&gt;&lt;/div&gt;
&lt;a href=&quot;http://www.jovialwanderer.com/2013/03/mt-palali-day-hike.html&quot;&gt;Source&lt;/a&gt;&lt;br /&gt;
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Related Link:&amp;nbsp; &lt;a href=&quot;http://www.traveltothephilippines.info/2013/07/16/the-protected-forests-of-mt-palali-in-nueva-vizcaya/&quot;&gt;&lt;i&gt;http://www.traveltothephilippines.info/2013/07/16/the-protected-forests-of-mt-palali-in-nueva-vizcaya/&lt;/i&gt;&lt;/a&gt;&lt;br /&gt;
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</content><link rel='replies' type='application/atom+xml' href='http://philippinevolcanoes.blogspot.com/feeds/2232111515292695790/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://philippinevolcanoes.blogspot.com/2017/03/mt-palali-in-nueva-vizcaya.html#comment-form' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/2232111515292695790'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/2232111515292695790'/><link rel='alternate' type='text/html' href='http://philippinevolcanoes.blogspot.com/2017/03/mt-palali-in-nueva-vizcaya.html' title='MT. PALALI IN NUEVA VIZCAYA'/><author><name>Unknown</name><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='https://img1.blogblog.com/img/b16-rounded.gif'/></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhfXscXhH7Ood4UVAVjhOXb_OdFw0P14CYxfD5wzbipBm6GaHg7dTk2OBodU5xhVa9VXyz9hq7ql1cbj3Equu4oNzJ_0hwmyHXjnIg2PbZIrhfJiPSipg4Te7pAnyzHxRJaIySdessIB8E/s72-c/0+click.jpg" height="72" width="72"/><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-5371504585591558867.post-1729484951375631853</id><published>2014-02-21T08:58:00.001-08:00</published><updated>2017-03-23T17:36:58.536-07:00</updated><category scheme="http://www.blogger.com/atom/ns#" term="active"/><category scheme="http://www.blogger.com/atom/ns#" term="Cagayan"/><category scheme="http://www.blogger.com/atom/ns#" term="Cagua"/><category scheme="http://www.blogger.com/atom/ns#" term="Cagua Volcano"/><category scheme="http://www.blogger.com/atom/ns#" term="eruptions"/><category scheme="http://www.blogger.com/atom/ns#" term="Philippine Volcanoes"/><category scheme="http://www.blogger.com/atom/ns#" term="Philippines"/><title type='text'>CAGUA VOLCANO IN CAGAYAN</title><content type='html'>&lt;div class=&quot;separator&quot; style=&quot;clear: both; text-align: center;&quot;&gt;
&lt;a href=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhe_GZnWpmvka2QMEQs8pviRDVhH6m-p7C8C5Zuz1drMnn686a7Jqikvr1mYgHcwpLRNVmCwe0UxZrMI1VocNwe2CtNwZwuxsfQy1ER_Kd9HccT59-Yz5SpdRcwX3rYZVlhZ5re6EduMug/s1600/0+click.jpg&quot; imageanchor=&quot;1&quot; style=&quot;margin-left: 1em; margin-right: 1em;&quot;&gt;&lt;img border=&quot;0&quot; src=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhe_GZnWpmvka2QMEQs8pviRDVhH6m-p7C8C5Zuz1drMnn686a7Jqikvr1mYgHcwpLRNVmCwe0UxZrMI1VocNwe2CtNwZwuxsfQy1ER_Kd9HccT59-Yz5SpdRcwX3rYZVlhZ5re6EduMug/s1600/0+click.jpg&quot; /&gt;&lt;/a&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Cagua, one of the active volcanoes in the Philippines, is located in the province of Cagayan. Specifically, it lies in the Cagayan Valley region, of northern Luzon island. Located in the northernmost part of the Sierra Madre mountain range, it lies in a region of active volcanism which probably originates from a fault between Babuyanes and Luzon. Though there is a more evident seismic record between northeast Luzon and the islands, volcanoes occur on the northwestern side of the island. Evidence of a correlation between the two islands includes agglomerates from multiple volcanoes and pebbles of andesitic lava throughout the region. - &lt;a href=&quot;http://en.wikipedia.org/wiki/Cagua_Volcano&quot;&gt;&lt;em&gt;http://en.wikipedia.org/wiki/Cagua_Volcano&lt;/em&gt;&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif; font-size: x-small;&quot;&gt;Photo from:&amp;nbsp; &lt;/span&gt;&lt;a class=&quot;_Nf irc_hol&quot; data-ctbtn=&quot;2&quot; data-cthref=&quot;http://www.google.com/url?sa=i&amp;amp;rct=j&amp;amp;q=&amp;amp;esrc=s&amp;amp;source=images&amp;amp;cd=&amp;amp;cad=rja&amp;amp;docid=kgy-NNjc7uwbCM&amp;amp;tbnid=vMLG8R2MlSnzlM:&amp;amp;ved=0CAQQjB0&amp;amp;url=http%3A%2F%2Fwww.phivolcs.dost.gov.ph%2Fhtml%2Fupdate_VMEPD%2FVolcano%2FVolcanoList%2Fcagua.htm&amp;amp;ei=0IQHU4bqN4jQ2AWm44DADw&amp;amp;psig=AFQjCNGFE5J3XK-z5T5w6aVI-oEhO6kJ_A&amp;amp;ust=1393087875655839&quot; data-ved=&quot;0CAQQjB0&quot; href=&quot;http://www.phivolcs.dost.gov.ph/&quot;&gt;&lt;span class=&quot;irc_ho&quot; dir=&quot;ltr&quot; style=&quot;text-align: left;&quot;&gt;&lt;span style=&quot;color: #1e0fbe; font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif; font-size: x-small;&quot;&gt;&lt;em&gt;www.phivolcs.dost.gov.ph&lt;/em&gt;&lt;/span&gt;&lt;/span&gt;&lt;/a&gt;&lt;span class=&quot;_Do&quot;&gt;&amp;nbsp;&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;This volcano is 3,717 feet high with a distinct summit crater. An explosive eruption was recorded in 1860. Signs of activity were observed in 1907 but no eruptions took place and the volcano has been quiet since.&amp;nbsp; - &lt;/span&gt;&lt;a href=&quot;http://wikimapia.org/1901450/Mt-Cagua-Volcano&quot;&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;&lt;em&gt;http://wikimapia.org/1901450/Mt-Cagua-Volcano&lt;/em&gt;&lt;/span&gt;&lt;/a&gt;&lt;br /&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif; font-size: x-small;&quot;&gt;Photo from:&amp;nbsp; &lt;/span&gt;&lt;a class=&quot;_Nf irc_hol&quot; data-ctbtn=&quot;0&quot; data-cthref=&quot;http://www.google.com/url?sa=i&amp;amp;rct=j&amp;amp;q=&amp;amp;esrc=s&amp;amp;source=images&amp;amp;cd=&amp;amp;docid=kgy-NNjc7uwbCM&amp;amp;tbnid=vMLG8R2MlSnzlM:&amp;amp;ved=0CAQQjB0&amp;amp;url=http%3A%2F%2Fen.wikipedia.org%2Fwiki%2FCagua_Volcano&amp;amp;ei=dYQHU4CsMIn02gWHoYGAAw&amp;amp;psig=AFQjCNGFE5J3XK-z5T5w6aVI-oEhO6kJ_A&amp;amp;ust=1393087875655839&quot; data-ved=&quot;0CAQQjB0&quot; href=&quot;http://en.wikipedia.org/&quot;&gt;&lt;span class=&quot;irc_ho&quot; dir=&quot;ltr&quot; style=&quot;text-align: left;&quot;&gt;&lt;span style=&quot;color: #1e0fbe; font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif; font-size: x-small;&quot;&gt;&lt;em&gt;en.wikipedia.org&lt;/em&gt;&lt;/span&gt;&lt;/span&gt;&lt;/a&gt;&lt;span class=&quot;_Do&quot;&gt;&amp;nbsp;&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Cagua volcano is  located in northern Luzon, Philippines. It is considered part of the Babuya segment because it falls within the N-S trend of the active volcanoes and is east of the trend of the Northern Luzon extinct volcanic centers.&lt;/span&gt;&lt;br /&gt;
&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Mt. Cagua is a calcalkaline basaltic and andesitic stratovolcano, which has been built up by at least three eruptive phases: &lt;/span&gt;&lt;br /&gt;
&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;1) An effusive phase between 1.5 and 1.2 Million years ago.&lt;br /&gt;  2)   Emission of thick andesitic pyroclastic flows at approximately 670,000 years ago.&lt;br /&gt;  3)  Young ash flow deposits, deposits, some of which were phreatomagmatic in origin.&lt;/span&gt;&lt;br /&gt;
&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;- &lt;/span&gt;&lt;a href=&quot;http://www.volcanolive.com/cagua.html&quot;&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;http://www.volcanolive.com/cagua.html&lt;/span&gt;&lt;/a&gt;&lt;br /&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif; font-size: large;&quot;&gt;&lt;strong&gt;Watch the Video:&lt;/strong&gt;&lt;/span&gt;&lt;/div&gt;
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&lt;iframe allowfullscreen=&quot;&quot; frameborder=&quot;0&quot; height=&quot;360&quot; src=&quot;//www.youtube.com/embed/ag5DiRmCA54?rel=0&quot; width=&quot;480&quot;&gt;&lt;/iframe&gt;&lt;br /&gt;&lt;/div&gt;
</content><link rel='replies' type='application/atom+xml' href='http://philippinevolcanoes.blogspot.com/feeds/1729484951375631853/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://philippinevolcanoes.blogspot.com/2014/02/cagua-volcano-in-cagayan.html#comment-form' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/1729484951375631853'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/1729484951375631853'/><link rel='alternate' type='text/html' href='http://philippinevolcanoes.blogspot.com/2014/02/cagua-volcano-in-cagayan.html' title='CAGUA VOLCANO IN CAGAYAN'/><author><name>Unknown</name><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='https://img1.blogblog.com/img/b16-rounded.gif'/></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhe_GZnWpmvka2QMEQs8pviRDVhH6m-p7C8C5Zuz1drMnn686a7Jqikvr1mYgHcwpLRNVmCwe0UxZrMI1VocNwe2CtNwZwuxsfQy1ER_Kd9HccT59-Yz5SpdRcwX3rYZVlhZ5re6EduMug/s72-c/0+click.jpg" height="72" width="72"/><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-5371504585591558867.post-8813037269048715172</id><published>2014-02-16T16:53:00.000-08:00</published><updated>2017-03-23T17:44:56.298-07:00</updated><category scheme="http://www.blogger.com/atom/ns#" term="Iriga Vocano"/><category scheme="http://www.blogger.com/atom/ns#" term="Mount Asog"/><category scheme="http://www.blogger.com/atom/ns#" term="Mount Iriga"/><category scheme="http://www.blogger.com/atom/ns#" term="Mt. Iriga"/><category scheme="http://www.blogger.com/atom/ns#" term="Philippine Volcanoes"/><category scheme="http://www.blogger.com/atom/ns#" term="Philippines"/><category scheme="http://www.blogger.com/atom/ns#" term="volcano"/><title type='text'>IRIGA VOLCANO IN CAMARINES SUR</title><content type='html'>&lt;div class=&quot;separator&quot; style=&quot;clear: both; text-align: center;&quot;&gt;
&lt;a href=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEirhDKdvTJ-D8y_ZNO4IiIgtMBhjnjMYABw4rRv4zgZjA0hTqcYcl20JlyUtnXhAEngz9VpAvzagyqY8DU8Mx_vF1hUzm3kbRFuRtjFd7Nk-NwXFVa3tt7qBhYtxFDDNzMs7BAapMs2xWQ/s1600/0+click.jpg&quot; imageanchor=&quot;1&quot; style=&quot;margin-left: 1em; margin-right: 1em;&quot;&gt;&lt;img border=&quot;0&quot; src=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEirhDKdvTJ-D8y_ZNO4IiIgtMBhjnjMYABw4rRv4zgZjA0hTqcYcl20JlyUtnXhAEngz9VpAvzagyqY8DU8Mx_vF1hUzm3kbRFuRtjFd7Nk-NwXFVa3tt7qBhYtxFDDNzMs7BAapMs2xWQ/s1600/0+click.jpg&quot; /&gt;&lt;/a&gt;&lt;/div&gt;
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&lt;a href=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgJNla4lfMSMg8mQff3GcHe5eXiLSfMT5uHSCuICS-vLpgO4nOumsOIFywu5Tp74O0o7ibpa6eWwt8_8t8Lo3gVBnPEfx_fNq-l-1-idY71yX0dHsqqkFcXp_Np-EpAij7l4bxULgownDk/s1600/Iriga+Volcano3.jpg&quot; imageanchor=&quot;1&quot; style=&quot;margin-left: 1em; margin-right: 1em;&quot;&gt;&lt;img border=&quot;0&quot; height=&quot;253&quot; src=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgJNla4lfMSMg8mQff3GcHe5eXiLSfMT5uHSCuICS-vLpgO4nOumsOIFywu5Tp74O0o7ibpa6eWwt8_8t8Lo3gVBnPEfx_fNq-l-1-idY71yX0dHsqqkFcXp_Np-EpAij7l4bxULgownDk/s1600/Iriga+Volcano3.jpg&quot; width=&quot;400&quot; /&gt;&lt;/a&gt;&lt;/div&gt;
&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif; font-size: x-small;&quot;&gt;Photo from:&amp;nbsp; &lt;/span&gt;&lt;a class=&quot;_Mf irc_hol&quot; data-ctbtn=&quot;2&quot; data-cthref=&quot;http://www.google.com/url?sa=i&amp;amp;rct=j&amp;amp;q=&amp;amp;esrc=s&amp;amp;source=images&amp;amp;cd=&amp;amp;cad=rja&amp;amp;docid=sECoGVauz42AeM&amp;amp;tbnid=Zk-OyHTj2GRFAM:&amp;amp;ved=0CAQQjB0&amp;amp;url=http%3A%2F%2Fjo.ramos.tripod.com%2Fid11.html&amp;amp;ei=SVsBU_WYOoHCywHkkIHADg&amp;amp;psig=AFQjCNHZQ0E40B3yZgi5vovijQJmQWZLEw&amp;amp;ust=1392683856101938&quot; data-ved=&quot;0CAQQjB0&quot; href=&quot;http://www.google.com/url?sa=i&amp;amp;rct=j&amp;amp;q=&amp;amp;esrc=s&amp;amp;source=images&amp;amp;cd=&amp;amp;cad=rja&amp;amp;docid=sECoGVauz42AeM&amp;amp;tbnid=Zk-OyHTj2GRFAM:&amp;amp;ved=0CAQQjB0&amp;amp;url=http%3A%2F%2Fjo.ramos.tripod.com%2Fid11.html&amp;amp;ei=SVsBU_WYOoHCywHkkIHADg&amp;amp;psig=AFQjCNHZQ0E40B3yZgi5vovijQJmQWZLEw&amp;amp;ust=1392683856101938&quot;&gt;&lt;span class=&quot;irc_ho&quot; dir=&quot;ltr&quot; style=&quot;text-align: left;&quot;&gt;&lt;span style=&quot;color: #1e0fbe; font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif; font-size: x-small;&quot;&gt;jo.ramos.tripod.com&lt;/span&gt;&lt;/span&gt;&lt;/a&gt;&lt;span class=&quot;_vo&quot;&gt;&amp;nbsp;&lt;/span&gt;&lt;br /&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Mount Iriga volcano is a small stratovolcano immediately SW of Lake Buhi in southern Luzon, Philippines. &lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;&lt;br /&gt;The volcano is dominantly andesitic in composition, but has several basaltic flank cones. It has a large crater breached to the SE, which formed during a massive flank failure that produced a large debris avalanche which buried several villages and formed a hilly, irregular deposit on the plain south of Lake Buhi 4 km from the summit. &lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif; font-size: small;&quot;&gt;Background:&lt;/span&gt;&lt;/h3&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Iriga is part of the Bicol volcanic arc which comprises at least 12 volcanic vents and complexes and is one of the 3 historically active, but the least active centers of the arc (the other 2 being Mayon and Bulusan). Iriga has only 2 known recorded eruptions in historic times. &lt;/span&gt;&lt;br /&gt;
&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;&lt;br /&gt;The catastrophic debris avalanche of Iriga volcano had been believed to have occurred during the 1628 AD eruption, but later work has now shown that the collapse and eruption occurred earlier at some unknown date in the past few thousands years. The avalanche was followed by phreatic explosions that created a small crater at the base of the scarp. &lt;/span&gt;&lt;br /&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;SOURCE:&amp;nbsp; &lt;/span&gt;&lt;a href=&quot;http://www.volcanodiscovery.com/iriga.html&quot;&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;http://www.volcanodiscovery.com/iriga.html&lt;/span&gt;&lt;/a&gt;&lt;br /&gt;
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&lt;a href=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhCb4A7i5wwiwJHJlYIsOnf8K8s9JWSYUGJuvu2-gGoloSEWsg-b02H_iF8GKD6fDrg1Te_0IIGBjP94lPwrb6hWhTBwe2Iv6Jor0vSz6BfEooNArzvOrhmgTbqQ-MwO6T_EzmuATphdYk/s1600/Iriga+Volcano.jpg&quot; imageanchor=&quot;1&quot; style=&quot;margin-left: 1em; margin-right: 1em;&quot;&gt;&lt;img border=&quot;0&quot; height=&quot;263&quot; src=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhCb4A7i5wwiwJHJlYIsOnf8K8s9JWSYUGJuvu2-gGoloSEWsg-b02H_iF8GKD6fDrg1Te_0IIGBjP94lPwrb6hWhTBwe2Iv6Jor0vSz6BfEooNArzvOrhmgTbqQ-MwO6T_EzmuATphdYk/s1600/Iriga+Volcano.jpg&quot; width=&quot;400&quot; /&gt;&lt;/a&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif; font-size: x-small;&quot;&gt;Photo from:&amp;nbsp; &lt;/span&gt;&lt;a href=&quot;http://www.volcano.si.edu/volcano.cfm?vn=273041&quot;&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif; font-size: x-small;&quot;&gt;http://www.volcano.si.edu/volcano.cfm?vn=273041&lt;/span&gt;&lt;/a&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Mount Iriga, also known as Mount Asog, is one of the active volcanos in the Philippines, in the province of Camarines Sur, in the Philippines.&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Mount Iriga is a stratovolcano about a kilometre from Lake Buhi. It rises 1,196&amp;nbsp;m (3,924&amp;nbsp;ft) with a base diameter of 10 kilometres.&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Iriga erupted in 1628 and 1642. Iriga is generally known for its phreatic explosions.&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;SOURCE:&amp;nbsp; &lt;/span&gt;&lt;a href=&quot;http://wikipedia.org/&quot;&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;http://wikipedia.org&lt;/span&gt;&lt;/a&gt;&lt;br /&gt;
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&lt;a href=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiFEfJOph5dJSisQ3ePIZp7xZM1EjyfcsI4ekvSAiCNd9ZabdquhoUCuUJNaBqQx7a8oae0UVbY6oQAZhSZqBDrldbHerGBkcrmOaGJ5qp-zMCs1lt39Fe26kDCAajpZrr9waz7tFqVQNk/s1600/Iriga+Volcano2.jpg&quot; imageanchor=&quot;1&quot; style=&quot;margin-left: 1em; margin-right: 1em;&quot;&gt;&lt;img border=&quot;0&quot; height=&quot;261&quot; src=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiFEfJOph5dJSisQ3ePIZp7xZM1EjyfcsI4ekvSAiCNd9ZabdquhoUCuUJNaBqQx7a8oae0UVbY6oQAZhSZqBDrldbHerGBkcrmOaGJ5qp-zMCs1lt39Fe26kDCAajpZrr9waz7tFqVQNk/s1600/Iriga+Volcano2.jpg&quot; width=&quot;400&quot; /&gt;&lt;/a&gt;&lt;/div&gt;
&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif; font-size: x-small;&quot;&gt;Photo from:&amp;nbsp; &lt;/span&gt;&lt;a href=&quot;http://www.mnh.si.edu/earth/text/dynamicearth/6_0_0_GeoGallery/geogallery_specimen.cfm?SpecimenID=174&amp;amp;categoryID=5&amp;amp;categoryName=Volcanoes&amp;amp;browseType=volcanoname&amp;amp;volcanoName=Iriga&quot;&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif; font-size: x-small;&quot;&gt;http://www.mnh.si.edu&lt;/span&gt;&lt;/a&gt;&lt;br /&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Iriga volcano is located in southern Luzon, Philippines. The Bicol Arc is composed of at least twelve volcanic centers and complexes that include three active volcanoes (Mayon, Iriga and Bulusan). Iriga is the least active of the three active volcanoes having had only two eruptions recorded throughout its history. &lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;The southern flank of Iriga has collapsed previously, causing a debris avalanche which traveled several kilometres, damming a river and creating a lake.&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;A left-lateral strike-slip fault passes under Iriga volcano. &lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Crater lake Buhi is located 4 km east of the summit. The lake is the home to the world&#39;s smallest edible commercial fish - Sinarapan &lt;em&gt;(Mistichthys luzonensis)&lt;/em&gt;.&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;The hazards at Iriga volcano are lava flows, pyroclastic flows, airfall tephra, debris avalanche and lahars.&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;SOURCE:&amp;nbsp; &lt;/span&gt;&lt;a href=&quot;http://www.volcanolive.com/iriga.html&quot;&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;http://www.volcanolive.com/iriga.html&lt;/span&gt;&lt;/a&gt;&lt;br /&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot;; font-size: x-small;&quot;&gt;Photo from:&amp;nbsp; &lt;/span&gt;&lt;a class=&quot;_Mf irc_hol&quot; data-ctbtn=&quot;2&quot; data-cthref=&quot;http://www.google.com/url?sa=i&amp;amp;rct=j&amp;amp;q=&amp;amp;esrc=s&amp;amp;source=images&amp;amp;cd=&amp;amp;cad=rja&amp;amp;docid=sECoGVauz42AeM&amp;amp;tbnid=Zk-OyHTj2GRFAM:&amp;amp;ved=0CAQQjB0&amp;amp;url=http%3A%2F%2Fmalate.wordpress.com%2F2008%2F04%2F03%2Fa-breather-in-camarines-sur%2F&amp;amp;ei=o1sBU_PpJ-moyAGvxYCgDQ&amp;amp;psig=AFQjCNHZQ0E40B3yZgi5vovijQJmQWZLEw&amp;amp;ust=1392683856101938&quot; data-ved=&quot;0CAQQjB0&quot; href=&quot;http://www.google.com/url?sa=i&amp;amp;rct=j&amp;amp;q=&amp;amp;esrc=s&amp;amp;source=images&amp;amp;cd=&amp;amp;cad=rja&amp;amp;docid=sECoGVauz42AeM&amp;amp;tbnid=Zk-OyHTj2GRFAM:&amp;amp;ved=0CAQQjB0&amp;amp;url=http%3A%2F%2Fmalate.wordpress.com%2F2008%2F04%2F03%2Fa-breather-in-camarines-sur%2F&amp;amp;ei=o1sBU_PpJ-moyAGvxYCgDQ&amp;amp;psig=AFQjCNHZQ0E40B3yZgi5vovijQJmQWZLEw&amp;amp;ust=1392683856101938&quot;&gt;&lt;span class=&quot;irc_ho&quot; dir=&quot;ltr&quot; style=&quot;text-align: left;&quot;&gt;&lt;span style=&quot;color: #1e0fbe; font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif; font-size: x-small;&quot;&gt;malate.wordpress.com&lt;/span&gt;&lt;/span&gt;&lt;/a&gt;&lt;span class=&quot;_vo&quot;&gt;&amp;nbsp;&lt;/span&gt;&lt;br /&gt;
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</content><link rel='replies' type='application/atom+xml' href='http://philippinevolcanoes.blogspot.com/feeds/8813037269048715172/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://philippinevolcanoes.blogspot.com/2014/02/photo-from-jo.html#comment-form' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/8813037269048715172'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/8813037269048715172'/><link rel='alternate' type='text/html' href='http://philippinevolcanoes.blogspot.com/2014/02/photo-from-jo.html' title='IRIGA VOLCANO IN CAMARINES SUR'/><author><name>Unknown</name><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='https://img1.blogblog.com/img/b16-rounded.gif'/></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEirhDKdvTJ-D8y_ZNO4IiIgtMBhjnjMYABw4rRv4zgZjA0hTqcYcl20JlyUtnXhAEngz9VpAvzagyqY8DU8Mx_vF1hUzm3kbRFuRtjFd7Nk-NwXFVa3tt7qBhYtxFDDNzMs7BAapMs2xWQ/s72-c/0+click.jpg" height="72" width="72"/><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-5371504585591558867.post-7203320637329556317</id><published>2014-02-07T10:10:00.000-08:00</published><updated>2017-03-23T17:48:23.766-07:00</updated><category scheme="http://www.blogger.com/atom/ns#" term="active volcano"/><category scheme="http://www.blogger.com/atom/ns#" term="Cagayan"/><category scheme="http://www.blogger.com/atom/ns#" term="Didicas Volcano"/><category scheme="http://www.blogger.com/atom/ns#" term="Mt. Didicas"/><category scheme="http://www.blogger.com/atom/ns#" term="new island formation"/><category scheme="http://www.blogger.com/atom/ns#" term="Philippine Volcanoes"/><title type='text'>MT. DIDICAS IN CAGAYAN</title><content type='html'>&lt;div class=&quot;separator&quot; style=&quot;clear: both; text-align: center;&quot;&gt;
&lt;a href=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhODVZknDGS60O4RroPWOfOeKrNlEDpMKk6EKCy8VyLc6tIGzE4TkDxEX6OL9AvFtZed-ZCtsmX2CnZWSPwWKAul8-1E2CC8xmpkNCS60PbwMbeLsf-KItyOTntqLB-IfMPyay5AzXvGkM/s1600/0+click.jpg&quot; imageanchor=&quot;1&quot; style=&quot;margin-left: 1em; margin-right: 1em;&quot;&gt;&lt;img border=&quot;0&quot; src=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhODVZknDGS60O4RroPWOfOeKrNlEDpMKk6EKCy8VyLc6tIGzE4TkDxEX6OL9AvFtZed-ZCtsmX2CnZWSPwWKAul8-1E2CC8xmpkNCS60PbwMbeLsf-KItyOTntqLB-IfMPyay5AzXvGkM/s1600/0+click.jpg&quot; /&gt;&lt;/a&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Didicas volcano is a small volcanic island 22 km NE of Camiguin Island, 60 km off the northern coast of Luzon, Philippines. &lt;/span&gt;&lt;br /&gt;
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&lt;span style=&quot;font-size: x-small;&quot;&gt;Photo from:&amp;nbsp; &lt;/span&gt;&lt;a href=&quot;http://flickr.com/&quot;&gt;&lt;span style=&quot;font-size: x-small;&quot;&gt;&lt;strong&gt;&lt;em&gt;http://flickr.com&lt;/em&gt;&lt;/strong&gt;&lt;/span&gt;&lt;/a&gt;&lt;/div&gt;
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&lt;b&gt;&lt;/b&gt;&lt;i&gt;&lt;/i&gt;&lt;u&gt;&lt;/u&gt;&lt;sub&gt;&lt;/sub&gt;&lt;sup&gt;&lt;/sup&gt;&lt;strike&gt;&lt;/strike&gt;&lt;br /&gt;
&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Until 1952, it was a submarine volcano that had previously formed temporary islands during eruptions. In the eruption of 1952 the submarine volcano formed a new lava dome that surfaced above sea level and has become now a permanent new island. &lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Didicas volcano now consists of a small, 244-m-high andesitic lava dome about 1.4 km in its longest diameter. &lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;A 400-m-wide crater was formed during the 1952 eruption. The first recorded submarine eruption of Didicas occurred in 1773.&amp;nbsp;&lt;/span&gt;&lt;br /&gt;
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&lt;span style=&quot;font-size: x-small;&quot;&gt;Photo from:&amp;nbsp;&lt;strong&gt;&lt;em&gt; http://&lt;/em&gt;&lt;/strong&gt;&lt;/span&gt;&lt;a class=&quot;_wf irc_hol&quot; data-ctbtn=&quot;2&quot; data-cthref=&quot;http://www.google.com/url?sa=i&amp;amp;rct=j&amp;amp;q=&amp;amp;esrc=s&amp;amp;frm=1&amp;amp;source=images&amp;amp;cd=&amp;amp;cad=rja&amp;amp;docid=k3UkQHN15jYjdM&amp;amp;tbnid=IlSN8mRJz4IFbM:&amp;amp;ved=0CAQQjB0&amp;amp;url=http%3A%2F%2Fsciencythoughts.blogspot.com%2F2012%2F01%2Fearthquake-in-babuyan-islands-of.html&amp;amp;ei=KCD1UtGIFIbSyAGdkYDIBA&amp;amp;psig=AFQjCNEefrARql3DAww78Jso-uDVYwK9Kg&amp;amp;ust=1391882584162464&quot; data-ved=&quot;0CAQQjB0&quot; href=&quot;http://sciencythoughts.blogspot.com/&quot;&gt;&lt;span class=&quot;irc_ho&quot; dir=&quot;ltr&quot; style=&quot;text-align: left;&quot;&gt;&lt;span style=&quot;color: #1e0fbe; font-size: x-small;&quot;&gt;&lt;strong&gt;&lt;em&gt;sciencythoughts.blogspot.com&lt;/em&gt;&lt;/strong&gt;&lt;/span&gt;&lt;/span&gt;&lt;/a&gt;&lt;span class=&quot;_Bn&quot;&gt;&amp;nbsp;&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;In an eruption in 1860, Didicas also built a new island, the first recorded cone of Didicas breaching the sea surface. It reached a height of 213 m in 1860, when the eruption ended, but it was soon eroded beneath the sea, because it mainly consisted of loose tephra. 3 rock masses up to 82 m high were left after an eruption in 1900. 2 more eruptions occurred since 1952 at an explosion crater on the northern side of the island. (Source: GVP volcano information) &lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;- Text above from:&amp;nbsp; &lt;a href=&quot;http://www.volcanodiscovery.com/&quot;&gt;&lt;em&gt;&lt;strong&gt;http://www.volcanodiscovery.com&lt;/strong&gt;&lt;/em&gt;&lt;/a&gt;&lt;/span&gt;&lt;br /&gt;
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&lt;strong&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot;;&quot;&gt;&lt;span style=&quot;font-size: x-small;&quot;&gt;Photos below from:&amp;nbsp; &lt;/span&gt;&lt;a href=&quot;http://www.koreanwaronline.com/NoSweat/Pages/Guam.htm&quot;&gt;&lt;span style=&quot;font-size: x-small;&quot;&gt;&lt;em&gt;http://www.koreanwaronline.com/NoSweat/Pages/Guam.htm&lt;/em&gt;&lt;/span&gt;&lt;/a&gt;&lt;/span&gt;&lt;/strong&gt;&lt;br /&gt;
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</content><link rel='replies' type='application/atom+xml' href='http://philippinevolcanoes.blogspot.com/feeds/7203320637329556317/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://philippinevolcanoes.blogspot.com/2014/02/mt-didicas-in-cagayan.html#comment-form' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/7203320637329556317'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/7203320637329556317'/><link rel='alternate' type='text/html' href='http://philippinevolcanoes.blogspot.com/2014/02/mt-didicas-in-cagayan.html' title='MT. DIDICAS IN CAGAYAN'/><author><name>Unknown</name><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='https://img1.blogblog.com/img/b16-rounded.gif'/></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhODVZknDGS60O4RroPWOfOeKrNlEDpMKk6EKCy8VyLc6tIGzE4TkDxEX6OL9AvFtZed-ZCtsmX2CnZWSPwWKAul8-1E2CC8xmpkNCS60PbwMbeLsf-KItyOTntqLB-IfMPyay5AzXvGkM/s72-c/0+click.jpg" height="72" width="72"/><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-5371504585591558867.post-3815125537018190840</id><published>2013-07-09T22:09:00.001-07:00</published><updated>2017-03-23T18:03:32.362-07:00</updated><category scheme="http://www.blogger.com/atom/ns#" term="active volcano"/><category scheme="http://www.blogger.com/atom/ns#" term="earthquakes"/><category scheme="http://www.blogger.com/atom/ns#" term="eruptions"/><category scheme="http://www.blogger.com/atom/ns#" term="mountain range"/><category scheme="http://www.blogger.com/atom/ns#" term="volcanic activity"/><title type='text'>MOUNT BINULUAN IN KALINGA PROVINCE</title><content type='html'>&lt;br /&gt;
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&lt;span style=&quot;font-size: x-small;&quot;&gt;Source:&amp;nbsp; https://en.wikipedia.org/wiki/Mount_Binuluan&lt;/span&gt;&lt;/div&gt;
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Mount Binuluan is a remote volcano in the Kalinga province of the Cordillera Administrative Region (CAR) Region of the Philippines. The 2,329-metre (7,641&amp;nbsp;ft) high mountain is part of the Cordillera Central mountain range on Luzon island, the largest island in the country. Binuluan exhibits active volcanism through numerous fumarole fields, solfataras and hot springs on its slope. There were reports of possible eruptions in 1952 and 1986 (or 1987), but they are unverified.&lt;br /&gt;
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Mount Binuluan [Bin-oo-loo-ahn (Lubuaganyen dialect)] is one of the highest peaks in the area. The mountain is surrounded by the municipalities of Lubuagan, Pasil and Tinglayan in Kalinga province.&lt;br /&gt;
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Southeast of the mountain is the Chico River flowing from southwest to northeast direction, while due northwest of the mountain is Pasil River, also flowing from southwest to northeast direction merging with Chico River just past the mountain. Mount Binuluan belongs to a range of mountains situated between the two rivers, trending southwest to northeast. Just southwest of Binuluan is Mount Mosimus 2,178&amp;nbsp;m (7,146&amp;nbsp;ft), followed by Mount Cauitan 2,569&amp;nbsp;m (8,428&amp;nbsp;ft) and Mount Alchan (Alchanon) 2,567&amp;nbsp;m (8,422&amp;nbsp;ft), the 19th and 20th tallest mountain in the Philippines. South of this line of mountains are Mount Chumangil 1,996&amp;nbsp;m (6,549&amp;nbsp;ft) and Mount Patoc 1,819&amp;nbsp;m (5,968&amp;nbsp;ft), the other volcano of the Central Cordillera Range displaying strong fumarolic activity.&lt;br /&gt;
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&lt;a href=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiLJyKuT8xU4fNxmZhhMPUFjJEqA0SIV0KG1uvPsNv3lHZd4y0DIbolAlxQFrmad-hOH29DfbV0JTybKiHA-xs4RgBUlp7Ra4rBuhWNi1-W62WfuRGUau7RAuiYOFy4Z_pGF3lBm8D1f1A/s1600/Mt.+Binuluan2.jpg&quot; imageanchor=&quot;1&quot; style=&quot;margin-left: 1em; margin-right: 1em;&quot;&gt;&lt;img border=&quot;0&quot; height=&quot;640&quot; src=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiLJyKuT8xU4fNxmZhhMPUFjJEqA0SIV0KG1uvPsNv3lHZd4y0DIbolAlxQFrmad-hOH29DfbV0JTybKiHA-xs4RgBUlp7Ra4rBuhWNi1-W62WfuRGUau7RAuiYOFy4Z_pGF3lBm8D1f1A/s640/Mt.+Binuluan2.jpg&quot; width=&quot;504&quot; /&gt;&lt;/a&gt;&lt;/div&gt;
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Mount Binuluan is usually covered &lt;nobr&gt;in cloud&lt;/nobr&gt; or mist and so photographs could be difficult to obtain. The village of Bangtitan in Upper Uma in Lubuagan is a good vantage point for views and photography of the mountain on the rare occasions when the primary peak is not mist-enshrouded. It is not known if Binuluan itself has ever been climbed as access to the site is very difficult. The terrain is rugged and undeveloped.&lt;br /&gt;
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Mount Binuluan exhibits a number of active geothermal features. There are a number of sites with strong steam emission, fumarolic activity, surface sulfur deposits, hot fresh water springs, hot sulfurous water springs, sulfur staining of riverine rocks, poisonous gas emissions, recent volcanic gas related deaths (&amp;gt;100 in last 20 years at Batong Buhay mines alone), heat destruction of vegetation, poisonous water, fumarole fields with new and shifting activity. - Wikipedia.org&lt;br /&gt;
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&lt;a href=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjnqi54a-ORhsVz3wJYOzHlQa8LkkbguOTNVnCeKBvH-zsuQNigrLbFXaU3J77L0HtbKZ_aWTHF2-0s645iYGQuod9ZuE9TlSkjm4Rq83T87ofICaMvq1rG0MXTI8mzVd5dEwUVNhg5WKk/s1600/Mt.+Binuluan3.jpg&quot; imageanchor=&quot;1&quot; style=&quot;margin-left: 1em; margin-right: 1em;&quot;&gt;&lt;img border=&quot;0&quot; height=&quot;478&quot; src=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjnqi54a-ORhsVz3wJYOzHlQa8LkkbguOTNVnCeKBvH-zsuQNigrLbFXaU3J77L0HtbKZ_aWTHF2-0s645iYGQuod9ZuE9TlSkjm4Rq83T87ofICaMvq1rG0MXTI8mzVd5dEwUVNhg5WKk/s640/Mt.+Binuluan3.jpg&quot; width=&quot;640&quot; /&gt;&lt;/a&gt;&lt;/div&gt;
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&lt;span style=&quot;font-size: x-small;&quot;&gt;Source: http://peakery.com/mount-binuluan-philippines-2/&lt;/span&gt;&lt;/div&gt;
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</content><link rel='replies' type='application/atom+xml' href='http://philippinevolcanoes.blogspot.com/feeds/3815125537018190840/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://philippinevolcanoes.blogspot.com/2013/07/mount-binuluan-also-known-as-mt.html#comment-form' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/3815125537018190840'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/3815125537018190840'/><link rel='alternate' type='text/html' href='http://philippinevolcanoes.blogspot.com/2013/07/mount-binuluan-also-known-as-mt.html' title='MOUNT BINULUAN IN KALINGA PROVINCE'/><author><name>Unknown</name><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='https://img1.blogblog.com/img/b16-rounded.gif'/></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhN2YP7aWWAV2mwa8LyHKWuLr-aSiY0P25FtokIrlVWa1CFRaaciFtOhBTyCs1eT70AMPI60q3r957uJ47umBb5mMiJdwKKkRbWUkOnZzFV7phSixTnpmQxU7mz_cEO-YKuVu-ocBDgHyA/s72-c/0+click.jpg" height="72" width="72"/><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-5371504585591558867.post-7886405318058611385</id><published>2012-12-05T08:33:00.001-08:00</published><updated>2017-03-23T18:04:49.427-07:00</updated><category scheme="http://www.blogger.com/atom/ns#" term="active volcano"/><category scheme="http://www.blogger.com/atom/ns#" term="complex volcano"/><category scheme="http://www.blogger.com/atom/ns#" term="compound volcano"/><category scheme="http://www.blogger.com/atom/ns#" term="eruptions"/><category scheme="http://www.blogger.com/atom/ns#" term="multiple vents"/><category scheme="http://www.blogger.com/atom/ns#" term="volcano"/><title type='text'>MOUNT BILIRAN IN SAMAR</title><content type='html'>&lt;div class=&quot;separator&quot; style=&quot;clear: both; text-align: center;&quot;&gt;
&lt;a href=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhN2YP7aWWAV2mwa8LyHKWuLr-aSiY0P25FtokIrlVWa1CFRaaciFtOhBTyCs1eT70AMPI60q3r957uJ47umBb5mMiJdwKKkRbWUkOnZzFV7phSixTnpmQxU7mz_cEO-YKuVu-ocBDgHyA/s1600/0+click.jpg&quot; imageanchor=&quot;1&quot; style=&quot;margin-left: 1em; margin-right: 1em;&quot;&gt;&lt;img border=&quot;0&quot; src=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhN2YP7aWWAV2mwa8LyHKWuLr-aSiY0P25FtokIrlVWa1CFRaaciFtOhBTyCs1eT70AMPI60q3r957uJ47umBb5mMiJdwKKkRbWUkOnZzFV7phSixTnpmQxU7mz_cEO-YKuVu-ocBDgHyA/s1600/0+click.jpg&quot; /&gt;&lt;/a&gt;&lt;/div&gt;
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&lt;span style=&quot;font-size: x-small;&quot;&gt;Photo from:&amp;nbsp; &lt;/span&gt;&lt;a href=&quot;http://www.biliranisland.com/photopost/showphoto.php?photo=2171&amp;amp;title=biliran-volcano&amp;amp;cat=504&quot;&gt;&lt;span style=&quot;font-size: x-small;&quot;&gt;&lt;em&gt;biliranisland.com&lt;/em&gt;&lt;/span&gt;&lt;/a&gt;&lt;br /&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;The volcanic island of Biliran, located across the narrow Biliran  Strait from the northern tip of Leyte Island, contains many prominent  andesitic lava domes, the highest of which is 1301 m Surio. Several  Pleistocene K-Ar dates have been obtained from volcanic centers on  northern Biliran Island. Fumarole fields are scattered throughout the  20 x 35 km wide island. The only known historical activity at Biliran  was a phreatic explosive eruption and possible debris avalanche at a  thermal area in 1939. - &lt;em&gt;silent-gardens.com&lt;/em&gt;&lt;/span&gt;&lt;br /&gt;
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&lt;span style=&quot;font-size: x-small;&quot;&gt;Photo from:&amp;nbsp; &lt;em&gt;malapascua.de&lt;/em&gt;&lt;/span&gt;&lt;br /&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Mount Biliran is an active volcano in the Philippines. It is a complex (compound) volcano, meaning that it has more than one feature. These volcanoes form because of changes of their eruptive characteristics or the location of multiple vents in an area. - &lt;em&gt;wiki.answers.com&lt;/em&gt;&lt;/span&gt;&lt;br /&gt;
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&lt;span style=&quot;font-size: x-small;&quot;&gt;Photo from:&amp;nbsp; &lt;em&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot;;&quot;&gt;silent-gardens.com&lt;/span&gt;&lt;/em&gt;&lt;/span&gt;&lt;br /&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Biliran&amp;nbsp;is a &lt;cite title=&quot;A volcano that consists of a complex of two or more vents, or a volcano that has an associated volcanic dome, either in its crater or on its flanks. Examples are Vesuvius and Mont Pelee.
&quot;&gt;compound volcano&lt;/cite&gt; that makes a large mountainous island just north of the island of Leyte.&amp;nbsp;&amp;nbsp;Biliran&#39;s single historic &lt;cite title=&quot;The process by which solid, liquid, and gaseous materials are ejected into the earth&#39;s atmosphere and onto the earth&#39;s surface by volcanic activity. Eruptions range from the quiet overflow of liquid rock to the tremendously violent expulsion of pyroclastics.
&quot;&gt;eruption&lt;/cite&gt; was from a flank &lt;cite title=&quot;The opening at the earth&#39;s surface through which volcanic materials issue forth. &quot;&gt;vent&lt;/cite&gt; in 1939.  There are five solfatara fields on the island.  The solfatara on the west side of Mt. Guinon contained more than 400 tones of sulfur in 1880. - &lt;em&gt;volcano.oregonstate.edu&lt;/em&gt;&lt;/span&gt;&lt;br /&gt;
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</content><link rel='replies' type='application/atom+xml' href='http://philippinevolcanoes.blogspot.com/feeds/7886405318058611385/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://philippinevolcanoes.blogspot.com/2012/12/mount-biliran-in-samar.html#comment-form' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/7886405318058611385'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/7886405318058611385'/><link rel='alternate' type='text/html' href='http://philippinevolcanoes.blogspot.com/2012/12/mount-biliran-in-samar.html' title='MOUNT BILIRAN IN SAMAR'/><author><name>Unknown</name><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='https://img1.blogblog.com/img/b16-rounded.gif'/></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhN2YP7aWWAV2mwa8LyHKWuLr-aSiY0P25FtokIrlVWa1CFRaaciFtOhBTyCs1eT70AMPI60q3r957uJ47umBb5mMiJdwKKkRbWUkOnZzFV7phSixTnpmQxU7mz_cEO-YKuVu-ocBDgHyA/s72-c/0+click.jpg" height="72" width="72"/><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-5371504585591558867.post-7438210187315894952</id><published>2012-10-14T19:25:00.001-07:00</published><updated>2017-03-23T18:06:47.114-07:00</updated><category scheme="http://www.blogger.com/atom/ns#" term="Bataan Peninsula"/><category scheme="http://www.blogger.com/atom/ns#" term="dormant volcano"/><category scheme="http://www.blogger.com/atom/ns#" term="Mount Limay"/><category scheme="http://www.blogger.com/atom/ns#" term="Mount Slamet"/><category scheme="http://www.blogger.com/atom/ns#" term="stratovolcano"/><category scheme="http://www.blogger.com/atom/ns#" term="sunsets in Manila"/><category scheme="http://www.blogger.com/atom/ns#" term="volcano-caldera"/><category scheme="http://www.blogger.com/atom/ns#" term="Zambales Mountains"/><title type='text'>MARIVELES VOLCANO IN BATAAN</title><content type='html'>&lt;div class=&quot;separator&quot; style=&quot;clear: both; text-align: center;&quot;&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif; font-size: x-small;&quot;&gt;Photo from:&amp;nbsp; &lt;em&gt;corregidor.org&lt;/em&gt;&lt;/span&gt;&lt;br /&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;The small, but voluminous Mariveles stratovolcano is located at the southern end of the Bataan Peninsula, on the west side of Manila Bay, Luzon Island, Philippines. &lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Although there are no known eruptions in historic times, it is a still active stratovolcano of andesitic composition. It has a 4-km-wide caldera open to the south. Mount Slamet on the north and Mount Limay on the east are 2 large, young flank cones.&lt;/span&gt;&lt;br /&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot;; font-size: x-small;&quot;&gt;Photo from:&amp;nbsp; &lt;em&gt;malapascua.de&lt;/em&gt;&lt;/span&gt;&lt;br /&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Mount Mariveles is a &lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;dormant&lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt; &lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;volcano&lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt; located in the &lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;province&lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt; of &lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Bataan&lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt; in the &lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Philippines&lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;. Mt. Mariveles and the adjacent &lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Mount Natib&lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt; comprise 80.9 percent of the total land area of the province. The mountain and adjacent cones lie opposite the city of &lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Manila&lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt; across &lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Manila Bay&lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;, providing a beautiful setting for the &lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;sunsets&lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt; seen from Manila.&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Mount Mariveles lies at the southern end of the &lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Zambales Mountains&lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt; in the &lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Bataan Peninsula&lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;, west of &lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Manila Bay&lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;. Bataan province belongs to the &lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Central&lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt; &lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Luzon&lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt; or &lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Region&lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt; III of the Philippines.&lt;/span&gt;&lt;br /&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot;; font-size: x-small;&quot;&gt;Photo from:&amp;nbsp; &lt;em&gt;corregidor.org&lt;/em&gt;&lt;/span&gt;&lt;br /&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Mariveles is a massive &lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;stratovolcano&lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt; topped with a 4-kilometre (2.5 mi) summit caldera which drains to the north. The highest peak, called Mariveles, has an elevation of 1,388 metres (4,554 ft) &lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;asl&lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;. Mounts Pantingan, Bataan, Tarak, and Vintana are the other peaks of the volcano-caldera complex, which has a base diameter of 22 kilometres (14 mi).&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Mount Samat&lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt; on the northern slope and Mount Limay on the eastern slope, are major, youthful-looking &lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;parasitic cones&lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt; of the volcano.&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Mariveles is still thermally active with the following &lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;hot springs&lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt; located within the complex: Tiis Spring, Saysain Spring, and Pucot Spring.&lt;/span&gt;&lt;br /&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot;; font-size: x-small;&quot;&gt;Photo from:&amp;nbsp; &lt;em&gt;panoramio.com&lt;/em&gt;&lt;/span&gt;&lt;br /&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;There are already three peaks familiar to the local mountaineering community namely: Tarak Ridge, Pantingan or Banayan Peak, and Mariveles Ridge. The rest of the peaks in the caldera are still waiting to be explored.&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Tarak Ridge is the more well-known destination on Mount Mariveles with its jump-off point situated at Barangay Alas-asin, &lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Mariveles&lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;, &lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Bataan&lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;.&lt;sup class=&quot;reference&quot; id=&quot;cite_ref-PM_3-0&quot;&gt;&lt;span style=&quot;font-size: small;&quot;&gt;[4]&lt;/span&gt;&lt;/sup&gt; Pantingan Peak (locally called Banayan Peak) can be accessed through Sitio Duhat, Saysain, &lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Bagac&lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;, &lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Bataan&lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;. Mariveles Ridge can be accessed through Sitio Parca, &lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Mariveles&lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;, &lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Bataan&lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;. - &lt;em&gt;wikipedia.org&lt;/em&gt;&lt;/span&gt;&lt;br /&gt;
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&lt;span style=&quot;font-size: x-small;&quot;&gt;Photo from:&amp;nbsp; &lt;em&gt;porkydocs.webs.com&lt;/em&gt;&lt;/span&gt;&lt;br /&gt;
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</content><link rel='replies' type='application/atom+xml' href='http://philippinevolcanoes.blogspot.com/feeds/7438210187315894952/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://philippinevolcanoes.blogspot.com/2012/10/mariveles-volcano-in-bataan.html#comment-form' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/7438210187315894952'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/7438210187315894952'/><link rel='alternate' type='text/html' href='http://philippinevolcanoes.blogspot.com/2012/10/mariveles-volcano-in-bataan.html' title='MARIVELES VOLCANO IN BATAAN'/><author><name>Unknown</name><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='https://img1.blogblog.com/img/b16-rounded.gif'/></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhN2YP7aWWAV2mwa8LyHKWuLr-aSiY0P25FtokIrlVWa1CFRaaciFtOhBTyCs1eT70AMPI60q3r957uJ47umBb5mMiJdwKKkRbWUkOnZzFV7phSixTnpmQxU7mz_cEO-YKuVu-ocBDgHyA/s72-c/0+click.jpg" height="72" width="72"/><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-5371504585591558867.post-1157073509333934993</id><published>2012-10-03T20:57:00.000-07:00</published><updated>2017-03-23T18:07:16.739-07:00</updated><category scheme="http://www.blogger.com/atom/ns#" term="Iraya Volcano"/><category scheme="http://www.blogger.com/atom/ns#" term="pyroclastic flow"/><category scheme="http://www.blogger.com/atom/ns#" term="volcaninc eruptions"/><title type='text'>IRAYA VOLCANO IN BATAN ISLAND</title><content type='html'>&lt;div style=&quot;text-align: justify;&quot;&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Iraya volcano is located on Batan Island, 200 km north of Luzon, Philippines. The volcano belongs to the Babuyan Segment, the least evolved of four segments of the Luzon arc.&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;The Babuyan Segment has developed on the western part of the Philippine Sea plate, which is subducted by the South China Sea plate and the Eurasian plate along the Manila Trench.&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-size: x-small;&quot;&gt;Photo from:&amp;nbsp; &lt;span id=&quot;rg_hr&quot;&gt;&lt;em&gt;phivolcs.dost.gov.ph&lt;/em&gt;&lt;/span&gt;&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;There are three volcanoes on Batan Island. Mahatao volcano is the oldest and is located in central Batan. It last erupted in the Late Miocene. Matarem volcano in the south of the island erupted in the Pliocene to Early Pleistocene. Iraya volcano is located in the north of the island and has been active since Late Pleistocene.&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Eruptions at Iraya volcano have been  Pelean, pyroclastic flows and lava flows. &lt;br /&gt;  In 1998 there was an earthquake swarm  at the volcano. - &lt;em&gt;volcanolive.com&lt;/em&gt;&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-size: x-small;&quot;&gt;Photo from:&amp;nbsp; &lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;&lt;em&gt;inkspiredmusings.blogspot.com&lt;/em&gt;&lt;/span&gt;&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;The morphologically youthful Iraya volcano, at the north end of Batan Island, is the northernmost active volcano in the Philippines.  Iraya is the most prominent feature of the 20-km-long, dumbbell-shaped Batan island, located in the Luzon Strait between Luzon and Taiwan.  The 1009-m-high Quaternary stratovolcano has a 1.5-km-wide summit crater, which is largely filled by a younger cone that forms the summit of the volcano.  Observed late-Pleistocene and Holocene products of Iraya are exclusively explosive.  The youngest dated unit of Iraya is a pyroclastic-flow deposit radiocarbon dated at about 1500 years ago (Richard et al., 1986).  The Philippines Institute of Volcanology and Seismology (2004-) listed an eruption in 1454 AD of unspecified character.- &lt;/span&gt;&lt;em&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;volcano.si.edu&lt;/span&gt;&lt;/em&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot;;&quot;&gt;&lt;span style=&quot;font-size: x-small;&quot;&gt;Photo from:&amp;nbsp; &lt;em&gt;explorevolcanoesnow.com&lt;/em&gt;&lt;/span&gt;&lt;/span&gt;&lt;/div&gt;
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</content><link rel='replies' type='application/atom+xml' href='http://philippinevolcanoes.blogspot.com/feeds/1157073509333934993/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://philippinevolcanoes.blogspot.com/2012/10/iraya-volcano-in-batan-island.html#comment-form' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/1157073509333934993'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/1157073509333934993'/><link rel='alternate' type='text/html' href='http://philippinevolcanoes.blogspot.com/2012/10/iraya-volcano-in-batan-island.html' title='IRAYA VOLCANO IN BATAN ISLAND'/><author><name>Unknown</name><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='https://img1.blogblog.com/img/b16-rounded.gif'/></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhN2YP7aWWAV2mwa8LyHKWuLr-aSiY0P25FtokIrlVWa1CFRaaciFtOhBTyCs1eT70AMPI60q3r957uJ47umBb5mMiJdwKKkRbWUkOnZzFV7phSixTnpmQxU7mz_cEO-YKuVu-ocBDgHyA/s72-c/0+click.jpg" height="72" width="72"/><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-5371504585591558867.post-1224356279210018045</id><published>2012-08-12T14:51:00.001-07:00</published><updated>2012-12-05T08:46:03.291-08:00</updated><category scheme="http://www.blogger.com/atom/ns#" term="active volcano"/><category scheme="http://www.blogger.com/atom/ns#" term="Aetas"/><category scheme="http://www.blogger.com/atom/ns#" term="ash deposits"/><category scheme="http://www.blogger.com/atom/ns#" term="eruption"/><category scheme="http://www.blogger.com/atom/ns#" term="lahar"/><category scheme="http://www.blogger.com/atom/ns#" term="Luzon"/><category scheme="http://www.blogger.com/atom/ns#" term="Mt. Pinatubo"/><category scheme="http://www.blogger.com/atom/ns#" term="Mt. Pinatubo Lake"/><title type='text'>MT. PINATUBO - A dormant volcano came to life</title><content type='html'>&lt;sup class=&quot;reference&quot; id=&quot;cite_ref-Science_News_6-0&quot;&gt;&lt;/sup&gt;&lt;br /&gt;
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&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: small;&quot;&gt;Photo from:&amp;nbsp; &lt;em&gt;volcano.oregonstate.edu&lt;/em&gt;&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif;&quot;&gt;&lt;span style=&quot;font-size: large;&quot;&gt;Mount Pinatubo is an &lt;/span&gt;&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;active&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt; &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;stratovolcano&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt; located on the island of &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;Luzon&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;, near the &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;tripoint&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt; of the &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;Philippine provinces&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt; of &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;Zambales&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;, &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;Tarlac&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;, and &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;Pampanga&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;. It is located in the Cabusilan Mountains separating the west coast of Luzon from the central plains. Before the volcanic activities of 1991, its eruptive history was unknown to most people. It was heavily &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;eroded&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;, inconspicuous and obscured from view. It was covered with dense &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;forest&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt; which supported a population of several thousand indigenous people, the &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;Aetas&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;, who fled to the mountains during the &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;Spanish&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt; &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;conquest&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt; of the Philippines.&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: Arial; font-size: small;&quot;&gt;Photo from:&amp;nbsp; &lt;em&gt;affinitycondoresort.com&lt;/em&gt;&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;The volcano&#39;s &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;Plinian&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt; / &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;Ultra-Plinian&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt; eruption on June 15, 1991 produced the second largest terrestrial eruption of the 20th century after the 1912 eruption of &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;Novarupta&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt; in the &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;Alaska Peninsula&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;. Complicating the eruption was the arrival of Typhoon Yunya bringing a lethal mix of ash and rain. Successful predictions at the onset of the climactic eruption led to the evacuation of tens of thousands of people from the surrounding areas, saving many lives, but the surrounding areas were severely damaged by &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;pyroclastic flows&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;, ash deposits, and subsequently, by the &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;lahars&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif;&quot;&gt;&lt;span style=&quot;font-size: large;&quot;&gt; caused by rainwaters re-mobilizing earlier volcanic deposits destroying thousands of infrastructures and altering the river systems months to years after the eruption.&lt;/span&gt;&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: Arial;&quot;&gt;&lt;span style=&quot;font-size: small;&quot;&gt;Photo from:&amp;nbsp; &lt;span id=&quot;rg_hr&quot;&gt;&lt;em&gt;lakbaypilipinas.com&lt;/em&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;The effects of the eruption were felt worldwide. It ejected roughly 10,000,000,000 &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;tonnes&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt; (1.1&lt;span style=&quot;margin-left: 0.2em;&quot;&gt;×&lt;span style=&quot;margin-left: 0.1em;&quot;&gt;10&lt;/span&gt;&lt;/span&gt;&lt;sup&gt;10&lt;/sup&gt; &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;short tons&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;) or 10 km&lt;sup&gt;3&lt;/sup&gt; (2.4 cu mi) of magma, and 20,000,000 t (22,000,000 short tons) &lt;span class=&quot;chemf&quot; style=&quot;white-space: nowrap;&quot;&gt;SO&lt;sub&gt;2&lt;/sub&gt;&lt;/span&gt;, bringing vast quantities of minerals and metals to the surface environment. It injected large amounts of &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;aerosol&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt; into the &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;stratosphere&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt; – more than any eruption since that of &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;Krakatoa&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt; in 1883. Over the following months, the aerosols formed a global layer of &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;sulfuric acid&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt; haze. Global temperatures dropped by about &lt;span style=&quot;white-space: nowrap;&quot;&gt;0.5 °C&lt;/span&gt; &lt;span style=&quot;white-space: nowrap;&quot;&gt;(0.900 °F)&lt;/span&gt;, and &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;ozone&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt; depletion temporarily increased substantially.&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: Arial;&quot;&gt;&lt;span style=&quot;font-size: small;&quot;&gt;Source:&amp;nbsp; &lt;em&gt;&lt;strong&gt;wikipedia.org&lt;/strong&gt;&lt;/em&gt;&lt;/span&gt;&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-size: small;&quot;&gt;Photo from:&amp;nbsp; &lt;span id=&quot;rg_hr&quot;&gt;&lt;em&gt;en.wikipedia.org&lt;/em&gt;&lt;/span&gt;&lt;/span&gt;&lt;/div&gt;
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&lt;/sup&gt;&lt;br /&gt;</content><link rel='replies' type='application/atom+xml' href='http://philippinevolcanoes.blogspot.com/feeds/1224356279210018045/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://philippinevolcanoes.blogspot.com/2012/08/mt-pinatubo-dormant-vocano-came-to-life.html#comment-form' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/1224356279210018045'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/1224356279210018045'/><link rel='alternate' type='text/html' href='http://philippinevolcanoes.blogspot.com/2012/08/mt-pinatubo-dormant-vocano-came-to-life.html' title='MT. PINATUBO - A dormant volcano came to life'/><author><name>Unknown</name><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='https://img1.blogblog.com/img/b16-rounded.gif'/></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgK1JY9kDlWaJJyPKHTrzJU0ScShyRu02HvdOEhguAXKP5hFU_GUaE56ch4NovXZP3UwyZ_WLZp3NOqmFmZV4kN0rj-xo2NuozTFk7Du-jDL07VKfNX8TqXzuipq5ExO-EUsyMUbkH00Nw/s72-c/Mt.+Pinatubo.jpg" height="72" width="72"/><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-5371504585591558867.post-3253256514405472239</id><published>2012-08-01T22:30:00.002-07:00</published><updated>2012-08-01T22:30:18.840-07:00</updated><category scheme="http://www.blogger.com/atom/ns#" term="forest"/><category scheme="http://www.blogger.com/atom/ns#" term="highest peak"/><category scheme="http://www.blogger.com/atom/ns#" term="Lake Danao"/><category scheme="http://www.blogger.com/atom/ns#" term="sacred volcano"/><category scheme="http://www.blogger.com/atom/ns#" term="stratovolcano"/><title type='text'>BALATUKAN VOLCANO</title><content type='html'>&lt;center&gt;
&lt;a href=&quot;http://gan.doubleclick.net/gan_click?lid=41000613802261325&amp;amp;pubid=21000000000548237&quot;&gt;&lt;img alt=&quot;525970_Magnetic Bracelets (Large)&quot; border=&quot;0&quot; src=&quot;http://gan.doubleclick.net/gan_impression?lid=41000613802261325&amp;amp;pubid=21000000000548237&quot; /&gt;&lt;/a&gt;&lt;/center&gt;
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&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif;&quot;&gt;&lt;span style=&quot;font-size: large;&quot;&gt;Mount Balatukan Range (also known as Balingoan or Balatocan) is a massive compound stratovolcano that rises above northwest shore of Gingoog Bay Misamis Oriental, Philippines. It is the highest peak in the city of Gingoog and the Municipalities of Claveria, Balingasag and Medina. It is sacred to the Higaonons and in the olden times their ancestors made pilgrimages to its peak. A lake called Danao is on its &lt;span class=&quot;IL_AD&quot; id=&quot;IL_AD6&quot;&gt;caldera&lt;/span&gt; or mouth. The mountain is an old volcano, said to have erupted in the 17th century.&lt;/span&gt;&lt;/span&gt;&lt;/div&gt;
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&lt;span id=&quot;more-812&quot;&gt;&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;It rises steeply to a long ridge with several peaks of almost 2,000 m and one of 2,442 m. The mountains retain extensive forest cover, and old growth forest is estimated to cover 6,500 ha. This is mainly montane forest, including mossy forest. The extent of primary lowland forest has been greatly reduced by logging and kaingin activities, and in 1997 this forest type was reported to be almost absent from the mountain. There are some areas of residual forest and cogon grassland.&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt; Today it looks over Gingoog City like a watchful sentry, guarding Gingoog from typhoons and strong winds. Three planes perished in its vicinity, the last one being the jet of defense secretary Devilla. Fortunately he was not on &lt;span class=&quot;IL_AD&quot; id=&quot;IL_AD3&quot;&gt;board&lt;/span&gt; when the plane crashed. The ill-fated &lt;span class=&quot;IL_AD&quot; id=&quot;IL_AD1&quot;&gt;Flight&lt;/span&gt; 387 of Cebu &lt;span class=&quot;IL_AD&quot; id=&quot;IL_AD8&quot;&gt;Pacific&lt;/span&gt; perished in its adjacent mountain: Mt. Lumot as impact point and Mt. Somagaya the final resting place of the unfortunate air &lt;span class=&quot;IL_AD&quot; id=&quot;IL_AD4&quot;&gt;transport&lt;/span&gt;.&lt;/span&gt;&lt;/div&gt;
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Source:&amp;nbsp;&lt;em&gt; &lt;/em&gt;&lt;em&gt;&lt;strong&gt;pinoyphotoblog.com&lt;/strong&gt;&lt;/em&gt;&lt;/div&gt;
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&lt;a href=&quot;http://gan.doubleclick.net/gan_click?lid=41000613802260266&amp;amp;pubid=21000000000548237&quot;&gt;&lt;img alt=&quot;524631_Karmic Balance™ Super Cleanse supplement! 20% off new orders, Use Code: KB20OFFNEW&quot; border=&quot;0&quot; src=&quot;http://gan.doubleclick.net/gan_impression?lid=41000613802260266&amp;amp;pubid=21000000000548237&quot; /&gt;&lt;/a&gt;&lt;/center&gt;
&lt;br /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://philippinevolcanoes.blogspot.com/feeds/3253256514405472239/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://philippinevolcanoes.blogspot.com/2012/08/balatukan-volcano.html#comment-form' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/3253256514405472239'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/3253256514405472239'/><link rel='alternate' type='text/html' href='http://philippinevolcanoes.blogspot.com/2012/08/balatukan-volcano.html' title='BALATUKAN VOLCANO'/><author><name>Unknown</name><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='https://img1.blogblog.com/img/b16-rounded.gif'/></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhYPjHD892A7VdR20RaeZqXLSS9jDDyHd5Rp82XP5KXAblTAsMmHaOJxmGcwZSe481aJjJTslBkbYpSO_Ke5dxuXMP3QQx0deLtIJ6xLocxWZiidZmWVOc3AuJzV_-UNYLVBcAanqERJF0/s72-c/Mt.+Balatukan.jpg" height="72" width="72"/><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-5371504585591558867.post-771631054135443700</id><published>2012-07-30T12:39:00.000-07:00</published><updated>2012-07-30T12:46:12.227-07:00</updated><category scheme="http://www.blogger.com/atom/ns#" term="Albay Province"/><category scheme="http://www.blogger.com/atom/ns#" term="Bicol Region"/><category scheme="http://www.blogger.com/atom/ns#" term="Mt. Malinao"/><category scheme="http://www.blogger.com/atom/ns#" term="Philippine Volcanoes"/><category scheme="http://www.blogger.com/atom/ns#" term="potentially active volcano"/><category scheme="http://www.blogger.com/atom/ns#" term="Vera Falls"/><category scheme="http://www.blogger.com/atom/ns#" term="volcano with a river"/><category scheme="http://www.blogger.com/atom/ns#" term="volcanoes in Bicol"/><title type='text'>MT. MALINAO IN ALBAY, BICOL REGION</title><content type='html'>&lt;div style=&quot;text-align: justify;&quot;&gt;
&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;Malinao is one of the three peaks of Albay, together with the famous Mt. Mayon and the little-known Mt. Masaraga. &lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: Arial;&quot;&gt;&lt;span style=&quot;font-size: x-small;&quot;&gt;Photo from:&lt;em&gt;&amp;nbsp; &lt;span id=&quot;rg_hr&quot;&gt;panoramio.com&lt;/span&gt;&lt;/em&gt;&lt;/span&gt;&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;Mt. Malinao is located south of Luzon and northeast of the Bicol Region particularly in the municipality of Malinao in Albay Province. It is a mountain range with an estimated altitude of 1,584 meters above sea level. It is&amp;nbsp; a potentially active volcano, with Mayon Volcano&amp;nbsp;in its southwest.&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: Arial;&quot;&gt;&lt;span style=&quot;font-size: x-small;&quot;&gt;Photo from:&amp;nbsp; &lt;span id=&quot;rg_hr&quot;&gt;&lt;em&gt;viewphotos.org&lt;/em&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: Arial;&quot;&gt;Text below from:&amp;nbsp; &lt;em&gt;&lt;strong&gt;pinoymountaineer.com&lt;/strong&gt;&lt;/em&gt;&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: x-small;&quot;&gt;Photo from:&amp;nbsp; &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: x-small;&quot;&gt;&lt;em&gt;ooohneh.blogspot.com&lt;/em&gt;&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;Mt. Malinao is the second of the &#39;Magayon Trio&#39; - the three beautiful mountains of the province of Albay. Of course, the first and by far the most famous is no less than the famous Mayon, where the very concept of Bicolano beauty derives. Malinao, as its name in various Filipino languages denote, means &#39;clear&#39; and likely it is the clarity of the mountain&#39;s waters that is described in the appellation. A striking example is Vera Falls, at the slopes of Mt. Malinao, itself a beautiful destination.&lt;/span&gt;&lt;br /&gt;
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&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;A lush forest surrounds Mt. Malinao, but prior to this, abaca plantations are encountered, a sight very typical of the hinterlands of Bicol. The forest is quite dense, reminiscent of Mt. Isarog. Although there are several peaks on the caldera rim of Mt. Malinao (being an old volcano), the usual trek only goes to the first peak, because of security concerns. &lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: Arial; font-size: x-small;&quot;&gt;Photo from:&amp;nbsp; &lt;em&gt;scrapercity.com&lt;/em&gt;&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-size: x-small;&quot;&gt;&lt;span style=&quot;font-family: Arial;&quot;&gt;Photo from:  &lt;em&gt;ooohneh.blogspot.com&lt;/em&gt;&lt;/span&gt;&lt;/span&gt;&lt;/div&gt;
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&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://philippinevolcanoes.blogspot.com/feeds/771631054135443700/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://philippinevolcanoes.blogspot.com/2012/07/mt-malinao-in-bicol.html#comment-form' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/771631054135443700'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/771631054135443700'/><link rel='alternate' type='text/html' href='http://philippinevolcanoes.blogspot.com/2012/07/mt-malinao-in-bicol.html' title='MT. MALINAO IN ALBAY, BICOL REGION'/><author><name>Unknown</name><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='https://img1.blogblog.com/img/b16-rounded.gif'/></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgrnlfzizT4NDo2nosJG-VSzVfwRtoTIso3mv5q3eLNY4IwxU7SBe35QI4ZJtPGWufHLQ8v8g562FZAFXbOxL2WR2zPgBhf__g2ObbDWILiy0qbCFFVa2WYk8yn6wKfDBEvZRnavh5k_2c/s72-c/Mt.+Malinao.jpg" height="72" width="72"/><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-5371504585591558867.post-7333873778804635271</id><published>2012-07-09T18:09:00.000-07:00</published><updated>2012-12-05T08:52:28.294-08:00</updated><category scheme="http://www.blogger.com/atom/ns#" term="inactive volcano"/><category scheme="http://www.blogger.com/atom/ns#" term="Laguna"/><category scheme="http://www.blogger.com/atom/ns#" term="Mt. Makiling"/><category scheme="http://www.blogger.com/atom/ns#" term="mystical mountain"/><category scheme="http://www.blogger.com/atom/ns#" term="Philippine Volcanoes"/><category scheme="http://www.blogger.com/atom/ns#" term="Philippines"/><category scheme="http://www.blogger.com/atom/ns#" term="popular hiking destination"/><category scheme="http://www.blogger.com/atom/ns#" term="volcanoes in Laguna"/><title type='text'>MT. MAKILING IN LAGUNA</title><content type='html'>&lt;div style=&quot;text-align: justify;&quot;&gt;
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&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;The mystical Mount  Makiling is the home of over a thousand diverse species of flora and fauna. Just a two-hour drive from Manila, this legendary mountain towering over Los Baños, Laguna and Sto Tomas, Batangas offers an ideal respite to commune with nature, experience the vanishing rainforest, and embark on a multitude of different adventures. It offers varied activities including simple nature tripping at the Botanical Garden and Pook ni Mariang Makiling, bird and butterfly watching, camping and trekking on its network of trails, swimming in its numerous hot springs, and mountain biking. This inactive volcano rises 1109 meters above sea level and offers a glimpse of some geological wonders like the Mud Spring – a sulfuric vent just 692m trek off the main trail, and the Flat Rocks – where you can swim in refreshing mini-sized water falls or just enjoy the lush greenery&lt;/span&gt;.&lt;/div&gt;
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&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: x-small;&quot;&gt;Photo from:&amp;nbsp; &lt;em&gt;&lt;a href=&quot;http://philippine-evolution.com/&quot;&gt;philippine-evolution.com&lt;/a&gt;&lt;/em&gt;&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif;&quot;&gt;&lt;span style=&quot;font-size: large;&quot;&gt;Mount Makiling is a potentially active &lt;/span&gt;&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;volcano&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt; in &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;Laguna province&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt; on the island of &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;Luzon&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;, &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;Philippines&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;. It rises to 1,090 m &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;above mean sea level&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;.&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: Arial; font-size: x-small;&quot;&gt;Photo from:&amp;nbsp; &lt;em&gt;travel.webshots.com&lt;/em&gt;&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;Mt. Makiling is a popular hiking destination. The two major trails begin at the UPLB College of Forestry and Brgy. San Miguel, &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;Sto. Tomas, Batangas&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;. The UPLB trail is more commonly used, taking 4–5 hours to reach the summit (Peak 2). However, this trail is closed as of October 2007 due to trail damage wrought by &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;Typhoon Xangsane&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif;&quot;&gt;&lt;span style=&quot;font-size: large;&quot;&gt; on September 2006. The other trail from Sto. Tomas passes by other peaks, is more difficult, and requires 6–7 hours to reach the summit. Both trails are generally established and safe, although throughout the years there have been occasional reports of fatal accidents and injuries, especially on the Sto. Tomas side. Climbers also frequently encounter leeches along the way.&lt;/span&gt;&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-size: x-small;&quot;&gt;&lt;span style=&quot;font-family: Arial;&quot;&gt;Photo from:  &lt;em&gt;&lt;a href=&quot;http://philippine-evolution.com/&quot;&gt;philippine-evolution.com&lt;/a&gt;&lt;/em&gt;&lt;/span&gt;&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: x-small;&quot;&gt;Photo from:&amp;nbsp; &lt;em&gt;panoramio.com&lt;/em&gt;&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-size: x-small;&quot;&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif;&quot;&gt;Sources:&amp;nbsp; &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif;&quot;&gt;&lt;strong&gt;&lt;em&gt;lakwatseradeprimera.com&lt;/em&gt;&lt;/strong&gt;&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif;&quot;&gt;&amp;nbsp;&amp;amp; &lt;strong&gt;&lt;em&gt;wikipedia.org&lt;/em&gt;&lt;/strong&gt;&lt;/span&gt;&lt;/span&gt;&lt;br /&gt;
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&lt;br /&gt;</content><link rel='replies' type='application/atom+xml' href='http://philippinevolcanoes.blogspot.com/feeds/7333873778804635271/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://philippinevolcanoes.blogspot.com/2012/07/mystical-mount-makiling-is-home-of-over.html#comment-form' title='1 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/7333873778804635271'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/7333873778804635271'/><link rel='alternate' type='text/html' href='http://philippinevolcanoes.blogspot.com/2012/07/mystical-mount-makiling-is-home-of-over.html' title='MT. MAKILING IN LAGUNA'/><author><name>Unknown</name><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='https://img1.blogblog.com/img/b16-rounded.gif'/></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhkDAX4P2rkxCdLMb3FfGUj4emOzOhB2Cj0PZsZFxK4OTCVDI_hyphenhyphenjKMob7FX8sGAyx9-1hnJr6oUCCd8oZ3kBAmZSNImtqkOf-wIxZPcKTnEESvFme8dOOtyxLurGqhXIeD73OPIGL28us/s72-c/Laguna+Mt.+Makiling.jpg" height="72" width="72"/><thr:total>1</thr:total></entry><entry><id>tag:blogger.com,1999:blog-5371504585591558867.post-6375091216896076035</id><published>2012-06-10T11:58:00.001-07:00</published><updated>2012-06-10T13:22:28.891-07:00</updated><category scheme="http://www.blogger.com/atom/ns#" term="hiking destination"/><category scheme="http://www.blogger.com/atom/ns#" term="Lenten Season"/><category scheme="http://www.blogger.com/atom/ns#" term="Mt. Banahaw"/><category scheme="http://www.blogger.com/atom/ns#" term="mysterious"/><category scheme="http://www.blogger.com/atom/ns#" term="pilgrimage site"/><title type='text'>Mt. Banahaw in Quezon</title><content type='html'>&lt;div style=&quot;text-align: justify;&quot;&gt;
&lt;span style=&quot;font-family: Verdana, sans-serif;&quot;&gt;Mount Banahaw&amp;nbsp; is a dormant volcano located on the boundary of Majayjay, Laguna and Lucban, Quezon in Luzon, Philippines. It is considered to be sacred by the local residents. It is adjacent to another mountain named Mount Banahaw de Lucban.&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: Verdana, sans-serif;&quot;&gt;Mt. Banahaw is one of the most frequented hiking destinations and pilgrimage sites in the Philippines. It has been gaining attractions not only for its natural beauty but also for its religious and cultural significance to Filipinos. &lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: Verdana, sans-serif;&quot;&gt;A significant number of tourists and religious devotees increase visits to Mt. Banahaw usually during the &lt;/span&gt;&lt;a href=&quot;http://en.wikipilipinas.org/index.php?title=Holy_Week&quot; title=&quot;Holy Week&quot;&gt;&lt;span style=&quot;font-family: Verdana, sans-serif;&quot;&gt;Lenten season&lt;/span&gt;&lt;/a&gt;&lt;span style=&quot;font-family: Verdana, sans-serif;&quot;&gt;. A climb to Mt. Banahaw takes a 2-3-day trek with different waterfalls and caves en route to the summit. There are at least four different trails from Dolores, Sariaya, and nearby towns of Quezon. Pilgrims and hikers usually take the trail of Cristalino and of Tatlong Tangke from Brgy. Kinabuhayan, Dolores reaching the Durungawan I, II, and III viewpoints atop the summit.&lt;/span&gt; &lt;/div&gt;
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&lt;span style=&quot;font-family: Verdana, sans-serif;&quot;&gt;Among the popular destinations in Mt. Banahaw include &quot;Kalbaryo&quot; (Calvary), &quot;Kweba ng Diyos Ama&quot; (Cave of God the Father), &quot;Husgado&quot; (Cave of Judgement), and the allegedly curative spring at Brgy. Kinabuhayan. Aside from the three Durungawan viewpoints at the summit, hikers can also explore the cave and the crater view overlooking Guis-guis and Tubig ng Gatas and Tubig ng Dugo rivers.&lt;/span&gt;&amp;nbsp; &lt;br /&gt;
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&lt;a href=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhMQuX56_4UO3QngZ8fr8wDZI7xWb4Stv-csG7EyPTiBU8N6pv7uOO1dc9HJXUx9MVBE1alD7XTqt61pCnp2l95Itq80ADevZRbgohN-tHr5uZ84nb7sTReEeCPhUumNUorrMiknCJ8qcU/s1600/Mt.+Banahaw4.jpg&quot; imageanchor=&quot;1&quot; style=&quot;margin-left: 1em; margin-right: 1em;&quot;&gt;&lt;img border=&quot;0&quot; height=&quot;300&quot; src=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhMQuX56_4UO3QngZ8fr8wDZI7xWb4Stv-csG7EyPTiBU8N6pv7uOO1dc9HJXUx9MVBE1alD7XTqt61pCnp2l95Itq80ADevZRbgohN-tHr5uZ84nb7sTReEeCPhUumNUorrMiknCJ8qcU/s400/Mt.+Banahaw4.jpg&quot; width=&quot;400&quot; /&gt;&lt;/a&gt;&lt;/div&gt;
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&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://philippinevolcanoes.blogspot.com/feeds/6375091216896076035/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://philippinevolcanoes.blogspot.com/2012/06/mount-banahaw-is-dormant-volcano.html#comment-form' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/6375091216896076035'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/6375091216896076035'/><link rel='alternate' type='text/html' href='http://philippinevolcanoes.blogspot.com/2012/06/mount-banahaw-is-dormant-volcano.html' title='Mt. Banahaw in Quezon'/><author><name>Unknown</name><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='https://img1.blogblog.com/img/b16-rounded.gif'/></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgwzhleqA5cSsSTx1l2fICsp0z__3-cq13lRTukM1iqWG3kh-TUtJQIMtJQKp8jKzxZ7nsaP6WH6-MlYGiSwAqRmRSVFRyD-ytknxLCktxtV-85UagM1DUk5WKeAEqlJihmxwc_yZ4d87Y/s72-c/Mt.+Banahaw.jpg" height="72" width="72"/><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-5371504585591558867.post-4880774952242788134</id><published>2012-04-21T18:02:00.001-07:00</published><updated>2012-04-21T18:02:39.442-07:00</updated><category scheme="http://www.blogger.com/atom/ns#" term="Bacun mountain trio"/><category scheme="http://www.blogger.com/atom/ns#" term="Benguet"/><category scheme="http://www.blogger.com/atom/ns#" term="burial place"/><category scheme="http://www.blogger.com/atom/ns#" term="hiking trail"/><category scheme="http://www.blogger.com/atom/ns#" term="mountain climbing"/><category scheme="http://www.blogger.com/atom/ns#" term="Mt. Kabunian"/><category scheme="http://www.blogger.com/atom/ns#" term="wild goats"/><category scheme="http://www.blogger.com/atom/ns#" term="wooden coffins"/><title type='text'>Mt. Kabunian in Benguet</title><content type='html'>&lt;div class=&quot;separator&quot; style=&quot;clear: both; text-align: center;&quot;&gt;
&lt;a href=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEh5S7SSIeDNZQCY0CYsQ17im96I1orB9XcKU_K3m6eT72z6eM-l02kJ-DFpowMvJiS8Q_pDnNm1LrWpR7otnuR3-87vQ4ciMZWeZrKJh1KLWAJrMxVkAb6CbIdidopvdgZrnUx1uJS1qxQ/s1600/Mount+Kabunian.jpg&quot; imageanchor=&quot;1&quot; style=&quot;margin-left: 1em; margin-right: 1em;&quot;&gt;&lt;img border=&quot;0&quot; height=&quot;201&quot; src=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEh5S7SSIeDNZQCY0CYsQ17im96I1orB9XcKU_K3m6eT72z6eM-l02kJ-DFpowMvJiS8Q_pDnNm1LrWpR7otnuR3-87vQ4ciMZWeZrKJh1KLWAJrMxVkAb6CbIdidopvdgZrnUx1uJS1qxQ/s320/Mount+Kabunian.jpg&quot; width=&quot;320&quot; /&gt;&lt;/a&gt;&lt;/div&gt;
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&lt;span class=&quot;Apple-style-span&quot; style=&quot;font-family: georgia;&quot;&gt;&lt;span style=&quot;color: #222222; font-size: large;&quot;&gt;The mountain is as 
majestic as its namesake, and über beautiful. Mt. Kabunian is the most popular 
among the Bacun trio, and it is named after the highest deity in the mythology 
of the Kankana-eys.&lt;/span&gt;&lt;/span&gt;&lt;br /&gt;
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&lt;a href=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiysiErRj6vb5N308qhrOCyye-3zb5sMLvbv8ekvuPOeyL3np9BOrn5sJRPS0jpWTZCFjBO55FErYk9xWK9u_M7sKrSn7MM7jjWQe_z9cS13nRcqauuGCbtlEHTtqX98ouwY5M0Zn8LYL0/s1600/Mount+Kabunian2.jpg&quot; imageanchor=&quot;1&quot; style=&quot;margin-left: 1em; margin-right: 1em;&quot;&gt;&lt;img border=&quot;0&quot; height=&quot;241&quot; src=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiysiErRj6vb5N308qhrOCyye-3zb5sMLvbv8ekvuPOeyL3np9BOrn5sJRPS0jpWTZCFjBO55FErYk9xWK9u_M7sKrSn7MM7jjWQe_z9cS13nRcqauuGCbtlEHTtqX98ouwY5M0Zn8LYL0/s320/Mount+Kabunian2.jpg&quot; width=&quot;320&quot; /&gt;&lt;/a&gt;&lt;/div&gt;
&lt;br /&gt;&lt;br /&gt;They believe that Kabunian resides in this mountain, 
so this is a very sacred place. Near the top, wooden coffins can be seen 
clinging on the side of the summit’s walls.&lt;br /&gt;
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&lt;a href=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhy7KuYC14v3PxeeqnhBKJfGr0ngwTmBSWLVvahFR62xVbz5AcZhpxyw6rfe5ep7aC4IsFsNTIhYDDvFNe0bEEh9zUGHwcFvtRJgD6rJjCfvMcKgXGTTyB1UkR0XOFG7FAdJI6jSKiB1Zw/s1600/Mount+Kabunian3.jpg&quot; imageanchor=&quot;1&quot; style=&quot;margin-left: 1em; margin-right: 1em;&quot;&gt;&lt;img border=&quot;0&quot; height=&quot;320&quot; src=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhy7KuYC14v3PxeeqnhBKJfGr0ngwTmBSWLVvahFR62xVbz5AcZhpxyw6rfe5ep7aC4IsFsNTIhYDDvFNe0bEEh9zUGHwcFvtRJgD6rJjCfvMcKgXGTTyB1UkR0XOFG7FAdJI6jSKiB1Zw/s320/Mount+Kabunian3.jpg&quot; width=&quot;240&quot; /&gt;&lt;/a&gt;&lt;/div&gt;
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&lt;br /&gt;We also saw some wild goats 
and a small forest fire. The view from the trail is expansive, the mountain 
breeze so cool.&lt;br /&gt;
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&lt;br /&gt;&lt;br /&gt;Bacun is far from Baguio, five to six hours ride on 
rented jeep, most of it on rough roads. The sight from the jump-off point is 
already magnificent that many who found the ride exhausting have been tempted to 
just stay here, have coffee and soak in the view. But for the hardy souls who 
leave the comfort of the village, the rewards are overwhelming.&lt;br /&gt;
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&lt;a href=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgdORgz7Is7KD9xuF_hKkTen9-qrxg_XFxrmDIbgtMS0TQHYDf4ws7GUu2smuFXkkpzXOzHZQoCzp5f95OTrIdsplKv-lCRBt6BmH987GAIQLsvCYCHiFtbp9gKwGw_4hyVr-oDvIbf4Ko/s1600/Mount+Kabunian5.jpg&quot; imageanchor=&quot;1&quot; style=&quot;margin-left: 1em; margin-right: 1em;&quot;&gt;&lt;img border=&quot;0&quot; height=&quot;240&quot; src=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgdORgz7Is7KD9xuF_hKkTen9-qrxg_XFxrmDIbgtMS0TQHYDf4ws7GUu2smuFXkkpzXOzHZQoCzp5f95OTrIdsplKv-lCRBt6BmH987GAIQLsvCYCHiFtbp9gKwGw_4hyVr-oDvIbf4Ko/s320/Mount+Kabunian5.jpg&quot; width=&quot;320&quot; /&gt;&lt;/a&gt;&lt;/div&gt;
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&lt;/span&gt;</content><link rel='replies' type='application/atom+xml' href='http://philippinevolcanoes.blogspot.com/feeds/4880774952242788134/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://philippinevolcanoes.blogspot.com/2012/04/mt-kabunian-in-benguet.html#comment-form' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/4880774952242788134'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/4880774952242788134'/><link rel='alternate' type='text/html' href='http://philippinevolcanoes.blogspot.com/2012/04/mt-kabunian-in-benguet.html' title='Mt. Kabunian in Benguet'/><author><name>Unknown</name><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='https://img1.blogblog.com/img/b16-rounded.gif'/></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEh5S7SSIeDNZQCY0CYsQ17im96I1orB9XcKU_K3m6eT72z6eM-l02kJ-DFpowMvJiS8Q_pDnNm1LrWpR7otnuR3-87vQ4ciMZWeZrKJh1KLWAJrMxVkAb6CbIdidopvdgZrnUx1uJS1qxQ/s72-c/Mount+Kabunian.jpg" height="72" width="72"/><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-5371504585591558867.post-5760798409007510047</id><published>2011-11-25T13:23:00.000-08:00</published><updated>2012-08-01T21:43:34.165-07:00</updated><category scheme="http://www.blogger.com/atom/ns#" term="Davao City"/><category scheme="http://www.blogger.com/atom/ns#" term="geothermal exploration program"/><category scheme="http://www.blogger.com/atom/ns#" term="island of Mindanao"/><category scheme="http://www.blogger.com/atom/ns#" term="Lake Leonard"/><category scheme="http://www.blogger.com/atom/ns#" term="Leonard Kniazeff"/><category scheme="http://www.blogger.com/atom/ns#" term="Leonard Range"/><category scheme="http://www.blogger.com/atom/ns#" term="Philippine Fault"/><title type='text'>LEONARD RANGE IN DAVAO</title><content type='html'>&lt;center&gt;
&lt;a href=&quot;http://gan.doubleclick.net/gan_click?lid=41000613802355078&amp;amp;pubid=21000000000548237&quot;&gt;&lt;img alt=&quot;&quot; border=&quot;0&quot; src=&quot;http://gan.doubleclick.net/gan_impression?lid=41000613802355078&amp;amp;pubid=21000000000548237&quot; /&gt;&lt;/a&gt;&lt;/center&gt;
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&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif;&quot;&gt;&lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/11/leonard-range-in-davao.html&quot;&gt;&lt;span style=&quot;font-size: large;&quot;&gt;Leonard Range&lt;/span&gt;&lt;/a&gt;&lt;span style=&quot;font-size: large;&quot;&gt; (also known as&lt;/span&gt;&lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/11/leonard-range-in-davao.html&quot;&gt;&lt;span style=&quot;font-size: large;&quot;&gt; Leonard Kniazeff&lt;/span&gt;&lt;/a&gt;&lt;span style=&quot;font-size: large;&quot;&gt;) volcano is an andesitic-dacitic volcanic complex with a 4x5 km caldera. It is located east of &lt;/span&gt;&lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/11/leonard-range-in-davao.html&quot;&gt;&lt;span style=&quot;font-size: large;&quot;&gt;Davao &lt;/span&gt;&lt;/a&gt;&lt;span style=&quot;font-size: large;&quot;&gt;Gulf in SE &lt;/span&gt;&lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/11/leonard-range-in-davao.html&quot;&gt;&lt;span style=&quot;font-size: large;&quot;&gt;Mindanao&lt;/span&gt;&lt;/a&gt;&lt;span style=&quot;font-size: large;&quot;&gt;, east of the major N-S-trending &lt;/span&gt;&lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/11/leonard-range-in-davao.html&quot;&gt;&lt;span style=&quot;font-size: large;&quot;&gt;Philippine Fault&lt;/span&gt;&lt;/a&gt;&lt;span style=&quot;font-size: large;&quot;&gt; and belongs to the East Mindanao Arc. &lt;/span&gt;&lt;/span&gt;&lt;/div&gt;
&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif;&quot;&gt;&lt;/span&gt;&lt;br /&gt;
&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif;&quot;&gt;&lt;br /&gt;&amp;nbsp;&lt;/span&gt;&lt;br /&gt;
&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif;&quot;&gt;&lt;/span&gt;&lt;br /&gt;
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&lt;span style=&quot;font-size: large;&quot;&gt;
The last activity of Leonard Range probably occurred about 1800 years ago, indicated by radiocarbon dating of charred wood found in a pyroclastic flow deposit on the edge of the caldera.&lt;br /&gt;
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Several thermal areas and solfataras occur at Leonard Range.&lt;/span&gt;&lt;br /&gt;
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&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif;&quot;&gt;&lt;/span&gt;&lt;br /&gt;
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&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif;&quot;&gt;&lt;span style=&quot;font-size: large;&quot;&gt;The Leonard Range (or North Davao) area is the site of a &lt;/span&gt;&lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/11/leonard-range-in-davao.html&quot;&gt;&lt;span style=&quot;font-size: large;&quot;&gt;geothermal exploration program&lt;/span&gt;&lt;/a&gt;&lt;span style=&quot;font-size: large;&quot;&gt;. &lt;/span&gt;&lt;/span&gt;&lt;br /&gt;
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Manat thermal area is located north of Lake Leonard, solfataras occur its SW rim, and active solfataras, fumaroles, and hot springs are found in the Amacan-Gopod thermal area south of the lake.&lt;br /&gt;
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&lt;/span&gt;&lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/11/leonard-range-in-davao.html&quot;&gt;&lt;span style=&quot;font-size: large;&quot;&gt;Lake Leonard&lt;/span&gt;&lt;/a&gt;&lt;span style=&quot;font-size: large;&quot;&gt; is located inside the caldera and contains freshwater with fish species including Anguila pacifica, Clarias batrachus, Glossogobius giurus, Ophicephalus striatus and Tilapia mossambica. It is also home to the the endangered Philippine crocodile Crocodylus mindorensis which is found at the lake during the breeding season in July-September.&lt;/span&gt; &lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;Another hour’s drive from Mainit is the majestic Lake Leonard. The caldera lake formed from the crater of the active volcano Leonard Kniaseff stretches 203 km in diameter against a mountain range coated in lush green.&lt;/span&gt;

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&lt;br /&gt;</content><link rel='replies' type='application/atom+xml' href='http://philippinevolcanoes.blogspot.com/feeds/5760798409007510047/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://philippinevolcanoes.blogspot.com/2011/11/leonard-range-in-davao.html#comment-form' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/5760798409007510047'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/5760798409007510047'/><link rel='alternate' type='text/html' href='http://philippinevolcanoes.blogspot.com/2011/11/leonard-range-in-davao.html' title='LEONARD RANGE IN DAVAO'/><author><name>Unknown</name><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='https://img1.blogblog.com/img/b16-rounded.gif'/></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiyOZahfSLeu1VJki7BarhkCFPBozXCMiHt8MSnjT0CSpLPncMt7lbaBGT1C_vRY9AaMjvuiQViclAulsCRc_qnF_VOaajkOfQ81KymBe591wJwUP64I-xDZIlfOdKERxi4TGIefcW1WC0/s72-c/Leonard+Range.jpg" height="72" width="72"/><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-5371504585591558867.post-6515057729120184305</id><published>2011-11-21T16:57:00.000-08:00</published><updated>2012-08-01T21:28:22.138-07:00</updated><category scheme="http://www.blogger.com/atom/ns#" term="Camarines Sur"/><category scheme="http://www.blogger.com/atom/ns#" term="island of Luzon"/><category scheme="http://www.blogger.com/atom/ns#" term="Lake Buhi"/><category scheme="http://www.blogger.com/atom/ns#" term="Malabsay Falls"/><category scheme="http://www.blogger.com/atom/ns#" term="Mount Isarog"/><category scheme="http://www.blogger.com/atom/ns#" term="Mt. Mayon"/><category scheme="http://www.blogger.com/atom/ns#" term="Nabuntalan Falls"/><category scheme="http://www.blogger.com/atom/ns#" term="Panicuason Trail"/><category scheme="http://www.blogger.com/atom/ns#" term="Patag-Patag Trail"/><category scheme="http://www.blogger.com/atom/ns#" term="Philippines"/><category scheme="http://www.blogger.com/atom/ns#" term="stratovolcano"/><title type='text'>MT. ISAROG IN CAMARINES SUR</title><content type='html'>&lt;center&gt;
&lt;a href=&quot;http://gan.doubleclick.net/gan_click?lid=41000613802180813&amp;amp;pubid=21000000000548237&quot;&gt;&lt;img alt=&quot;238038_Enjoy Romantic Miami Vacation&quot; border=&quot;0&quot; src=&quot;http://gan.doubleclick.net/gan_impression?lid=41000613802180813&amp;amp;pubid=21000000000548237&quot; /&gt;&lt;/a&gt;&lt;/center&gt;
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&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif;&quot;&gt;&lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/11/mt-isarog-in-camarines-sur.html&quot;&gt;Mount Isarog&lt;/a&gt; is a &lt;/span&gt;&lt;span style=&quot;color: black; font-family: Arial, Helvetica, sans-serif;&quot;&gt;potentially active&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif;&quot;&gt; &lt;/span&gt;&lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/11/mt-isarog-in-camarines-sur.html&quot; title=&quot;Stratovolcano&quot;&gt;&lt;span style=&quot;color: #0645ad; font-family: Arial, Helvetica, sans-serif;&quot;&gt;stratovolcano&lt;/span&gt;&lt;/a&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif;&quot;&gt; located in the province of &lt;/span&gt;&lt;span style=&quot;color: #0645ad; font-family: Arial, Helvetica, sans-serif;&quot;&gt;&lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/11/mt-isarog-in-camarines-sur.html&quot;&gt;Camarines Sur&lt;/a&gt;&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif;&quot;&gt;, Island of &lt;/span&gt;&lt;span style=&quot;color: #0645ad; font-family: Arial, Helvetica, sans-serif;&quot;&gt;&lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/11/mt-isarog-in-camarines-sur.html&quot;&gt;Luzon&lt;/a&gt;&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif;&quot;&gt;, &lt;/span&gt;&lt;span style=&quot;color: #0645ad; font-family: Arial, Helvetica, sans-serif;&quot;&gt;&lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/11/mt-isarog-in-camarines-sur.html&quot;&gt;Philippines&lt;/a&gt;&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif;&quot;&gt;.&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif;&quot;&gt;A paradise at the heart of &lt;/span&gt;&lt;span style=&quot;color: black; font-family: Arial, Helvetica, sans-serif;&quot;&gt;Camarines Sur&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif;&quot;&gt; is lotfy Mt. Isarog, rising to 1966 MASL. This mountain has a rich biodiversity and beautiful views: its very own mossy forests and verdant crater, an overview of Bicol Peninsula, and a glimpse of majestic &lt;/span&gt;&lt;span style=&quot;color: #006699; font-family: Arial, Helvetica, sans-serif;&quot;&gt;&lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/11/mt-isarog-in-camarines-sur.html&quot;&gt;Mt. Mayon&lt;/a&gt;&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif;&quot;&gt;. It abundance of water is refreshing, with streams and waterfalls encountered along the trails, and sulfuric springs beckon to relax weary mountaineers and other visitors. Its dubbing as &quot;Vulcan de Agua&quot; lives up to expectations: Isarog has 16 major rivers that provide potable water to 15 of the 35 towns of Camarines Sur and irrigate some 67,400 hectares of rice lands at its foot.&lt;/span&gt;&lt;br /&gt;
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&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif;&quot;&gt;There is a cornucopia of species in Mt. Isarog, and most distinguished in the list are the endemic ones: the Mt. Isarog Shrew Mouse, Isarog Striped Shrew Rat, the Isarog Shrew Rat and the Isolated Forest Frog. In all, there are 143 species of birds. Mammals found in the area include, among others, the Philippine deer, monkeys, bats, wildcat and wild pig. There is also a snake that is endemic to Mt. Isarog, but don&#39;t worry, it&#39;s blind! (Typhlops jagorii). These animal species find refuge in a forest that has more than 1300 species of plants including hardwood trees, mosses, ferns and orchids. Rafflesia, the largest flower genus in the world, have also been sighted in this mountain. You would also encounter mushrooms and a number of colorful insects.&lt;br /&gt;
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Three trails in Mt. Isarog lead to two different destinations. The commonly used trail, leading to the summit, is the &lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/11/mt-isarog-in-camarines-sur.html&quot;&gt;Panicuason trail&lt;/a&gt;, which starts at DENR station in Brgy. Panicuason, Naga City. A second trail is the &lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/11/mt-isarog-in-camarines-sur.html&quot;&gt;Patag-Patag trail&lt;/a&gt; (said to be a misnomer because the trail is far from &#39;patag&#39; (flat) but steep and challenging, will be discussed on a separate itinerary. Finally, there&#39;s the trail from Goa, Camarines Sur, which takes four days.&lt;/div&gt;
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&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif;&quot;&gt;The initial highlight of a climb in the Panicuason trail are the waterfalls: &lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/11/mt-isarog-in-camarines-sur.html&quot;&gt;Malabsay Falls&lt;/a&gt;, with its large catchbasin and &lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/11/mt-isarog-in-camarines-sur.html&quot;&gt;Nabuntalan Falls&lt;/a&gt; which will be visited before reaching Camp 1, around 2 hours away from the jump-off. A series of campsites ensue until the summit, for a total of 8-10 hours trekking time from jump-off. However, usually the trek is interrupted before sundown in what is simply known as &#39;Campsite&#39;, from which the assault to the summit is done the next day. Throughout the trails, you will be surrounded by the mossy forest of Isarog. The trails are described as moderate in difficulty, with ample cover from the trees, an abundance of water sources, and reasonable slopes. Campsites are available as rest stations.&lt;br /&gt;
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From the Campsite, it takes 90-100 minutes to reach the summit. It is usually started very early morning. At this point, beyond 1500 MASL, the trees become stunted and covered with mosses and liverworts, characteristic of the mossy forest. At the summit viewdeck, a distant Mt. Mayon with its perfect cone shape rises south, and the verdant crater of Isarog can be seen- a vast expanse of land. You can see the waters bounding the Bicol peninsula, as well as the towns of Camarines Sur. It is a rewarding array of sights after a thoroughly challenging trek.&lt;br /&gt;
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After descent, to make the trip to Bicol worthwhile, favorite sidetrips include a stay at the Camsur Wakeboarding Complex, and the nearby Mt. Asog (Iriga). You may also stay at Consocep Mountain Resort but this is more accessible through the Patag-Patag itinerary since it&#39;s in Tigaon. Take time also to visit &lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/11/mt-isarog-in-camarines-sur.html&quot;&gt;Lake Buhi&lt;/a&gt;, another famous feature of the province.&lt;/div&gt;
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Source: pinoymountaineer.com

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&lt;br /&gt;</content><link rel='replies' type='application/atom+xml' href='http://philippinevolcanoes.blogspot.com/feeds/6515057729120184305/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://philippinevolcanoes.blogspot.com/2011/11/mt-isarog-in-camarines-sur.html#comment-form' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/6515057729120184305'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/6515057729120184305'/><link rel='alternate' type='text/html' href='http://philippinevolcanoes.blogspot.com/2011/11/mt-isarog-in-camarines-sur.html' title='MT. ISAROG IN CAMARINES SUR'/><author><name>Unknown</name><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='https://img1.blogblog.com/img/b16-rounded.gif'/></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEh2NKjV3fZznUKYZ3R34ceTYweGHgoriV2TwxoNu-PtIGxvhuaAxzenTDbwEe8MsoYzjHyEOeGkqb3PySqVI3Eiezdzk3yk7NOJ3Zz18-RXgRnOjt8HnJ6FyVYOcpYuvchBG6NMDbFnWnA/s72-c/Mt.+Isarog" height="72" width="72"/><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-5371504585591558867.post-6298798619199274044</id><published>2011-11-14T18:23:00.000-08:00</published><updated>2017-03-23T17:34:20.114-07:00</updated><category scheme="http://www.blogger.com/atom/ns#" term="Camiguin"/><category scheme="http://www.blogger.com/atom/ns#" term="great challenge to mountain climbers"/><category scheme="http://www.blogger.com/atom/ns#" term="island of Mindanao"/><category scheme="http://www.blogger.com/atom/ns#" term="Luzon in the Philippines"/><category scheme="http://www.blogger.com/atom/ns#" term="Mt. Hibok-Hibok"/><category scheme="http://www.blogger.com/atom/ns#" term="popular hiking destination"/><category scheme="http://www.blogger.com/atom/ns#" term="spectacular vista of the entire island"/><title type='text'>MT. HIBOK-HIBOK IN CAMIGUIN</title><content type='html'>&lt;center&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Hibok-hibok (also called Catarman) is a stratovolcano and makes the island of  Camiguin, about 12 miles (20 km) north of Mindanao, Philippines. The  summit is covered with loose ejecta and four small craters are nearby. &lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Mt. Hibok-Hibok is the lone active volcano in the island of Camiguin Philippines.  After its last eruption, the Philippine &lt;span class=&quot;IL_AD&quot; id=&quot;IL_AD3&quot;&gt;Government&lt;/span&gt; created the Commission on Volcanology known as PHIVOLCS (Philippine Institute of Volcanology &amp;amp; Seismology) and a PHIVOLCS Observatory Station was established in order to monitor any unusual seismic activities for the safety of visitors and residents of the island. &lt;/span&gt;&lt;br /&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;The furrowed flank of Mt. Hibok-Hibok rises majestically behind the capital town of Mambajao.&amp;nbsp; &lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Mt. Hibok-Hibok is a popular &lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;hiking&lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt; destination in Camiguin island.&amp;nbsp; &lt;/span&gt;The sharp-edged ridges, down whose sides run deeply cut channels from past magma flows, pose a great challenge to mountain climbers.  One has to be seasoned enough to climb and manoeuvre over loose rocks and boulders in order to reach the volcano’s peak and be rewarded with the sight of its crater lake and a spectacular vista of the entire island of Camiguin.  On a clear day, one can see on the horizon the silhouette of its neighbours, the island of Bohol, Cebu and Negros. &lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Around the summit of Mt. Hibok-Hibok are several small craters filled with water.  These craters were small cracks in the volcano’s peak, where once lava flowed, and which hardened into bowl shapes and eventually filled with water and formed shallow lakes.  Being active, numerous steam vents and outlets are at the sides and apex of the volcano.&lt;/span&gt; &lt;/div&gt;
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&lt;br /&gt;</content><link rel='replies' type='application/atom+xml' href='http://philippinevolcanoes.blogspot.com/feeds/6298798619199274044/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://philippinevolcanoes.blogspot.com/2011/11/mt-hibok-hibok-in-camiguin.html#comment-form' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/6298798619199274044'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/6298798619199274044'/><link rel='alternate' type='text/html' href='http://philippinevolcanoes.blogspot.com/2011/11/mt-hibok-hibok-in-camiguin.html' title='MT. HIBOK-HIBOK IN CAMIGUIN'/><author><name>Unknown</name><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='https://img1.blogblog.com/img/b16-rounded.gif'/></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhe_GZnWpmvka2QMEQs8pviRDVhH6m-p7C8C5Zuz1drMnn686a7Jqikvr1mYgHcwpLRNVmCwe0UxZrMI1VocNwe2CtNwZwuxsfQy1ER_Kd9HccT59-Yz5SpdRcwX3rYZVlhZ5re6EduMug/s72-c/0+click.jpg" height="72" width="72"/><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-5371504585591558867.post-7622724782276093159</id><published>2011-11-09T18:27:00.000-08:00</published><updated>2011-11-09T19:31:02.867-08:00</updated><category scheme="http://www.blogger.com/atom/ns#" term="Camping"/><category scheme="http://www.blogger.com/atom/ns#" term="exploring nature"/><category scheme="http://www.blogger.com/atom/ns#" term="horseback riding"/><category scheme="http://www.blogger.com/atom/ns#" term="island in a like on an island in a lake on an island"/><category scheme="http://www.blogger.com/atom/ns#" term="Luzon in the Philippines"/><category scheme="http://www.blogger.com/atom/ns#" term="Taal Lake"/><category scheme="http://www.blogger.com/atom/ns#" term="Taal Volcano"/><category scheme="http://www.blogger.com/atom/ns#" term="trekking"/><category scheme="http://www.blogger.com/atom/ns#" term="world&#39;s smallest sctive volcano"/><title type='text'>TAAL VOLCANO</title><content type='html'>&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif;&quot;&gt;&lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/11/taal-volcano-is-located-in-southern.html&quot;&gt;Taal volcano&lt;/a&gt; is located in the southern part of &lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/11/taal-volcano-is-located-in-southern.html&quot;&gt;Luzon in the Philippines&lt;/a&gt;. It is  about 50km from the capital, Manila. Right in the center of the island is the  main crater that holds a sulfuric lake. It is famous for having an &lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/11/taal-volcano-is-located-in-southern.html&quot;&gt;island in a  lake on an island in a lake on an island&lt;/a&gt; in the Pacific Ocean.  &lt;/span&gt;&lt;br /&gt;
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&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif;&quot;&gt;The place&lt;strong&gt; &lt;/strong&gt;offers adventurers the unique thrill of &lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/11/taal-volcano-is-located-in-southern.html&quot;&gt;exploring  nature&lt;/a&gt; and experiencing the attractions of the &lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/11/taal-volcano-is-located-in-southern.html&quot;&gt;world&#39;s smallest active volcano&lt;/a&gt;.  There are a host of activities that can be enjoyed on the island. Among them are  &lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/11/taal-volcano-is-located-in-southern.html&quot;&gt;horseback riding&lt;/a&gt; going to the crater, &lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/11/taal-volcano-is-located-in-southern.html&quot;&gt;trekking&lt;/a&gt; and &lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/11/taal-volcano-is-located-in-southern.html&quot;&gt;camping&lt;/a&gt;. &lt;/span&gt;&lt;br /&gt;
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&lt;span style=&quot;font-size: small;&quot;&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif;&quot;&gt; &lt;/span&gt;&lt;/span&gt;&lt;small&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: small;&quot;&gt;Tall Volcano in the Philippines, was originally a huge volcano, that towered 18,000 feet up into the sky.&amp;nbsp; It has been called the smallest active volcano because it seems small now, but many people don&#39;t realize that it is one of the largest volcanoes in the world.&amp;nbsp; It is located about 70-km south of Manila on &quot;volcano island&quot; inside a lade called &lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/11/taal-volcano-is-located-in-southern.html&quot;&gt;Taal lake&lt;/a&gt; or Lake Taal.&lt;/span&gt;&lt;/small&gt;&lt;br /&gt;
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&lt;div class=&quot;separator&quot; style=&quot;clear: both; text-align: center;&quot;&gt;&lt;a href=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgBJHtMNrZEdni2CTevkFzBrHIlftqFvGRp-3gHFekDLqEf0craRtVOGCtRwVXfEnaUCZsYZyEVIqAZWgjbzQ4O_ixOHEJPa5opJbFy7iQz1YSDFF01KS_lJcNhvol5Qds9ZsuXPif9nuY/s1600/taal+volcano3.jpg&quot; imageanchor=&quot;1&quot; style=&quot;margin-left: 1em; margin-right: 1em;&quot;&gt;&lt;img border=&quot;0&quot; height=&quot;298&quot; src=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgBJHtMNrZEdni2CTevkFzBrHIlftqFvGRp-3gHFekDLqEf0craRtVOGCtRwVXfEnaUCZsYZyEVIqAZWgjbzQ4O_ixOHEJPa5opJbFy7iQz1YSDFF01KS_lJcNhvol5Qds9ZsuXPif9nuY/s400/taal+volcano3.jpg&quot; width=&quot;400&quot; /&gt;&lt;/a&gt;&lt;/div&gt;&lt;br /&gt;
&lt;/div&gt;&lt;div style=&quot;font-family: verdana;&quot;&gt;&lt;small&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: small;&quot;&gt;This  picture of Taal volcano , was taken  from Tagaytay ridge. Actually, &lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/11/taal-volcano-is-located-in-southern.html&quot;&gt;Tagaytay Ridge&lt;/a&gt; is the rim of the volcano! When  the volcano was 18,000 feet high, Tagaytay ridge would have been only about a  sixth of the way to the top of the volcano!! In the distance, Mt. Makulot forms  part of the other side of the rim, and it is a &lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/11/taal-volcano-is-located-in-southern.html&quot;&gt;favorite trek&lt;/a&gt; for climbers.&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp; &lt;/span&gt;&lt;/small&gt;&lt;br /&gt;
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&lt;div class=&quot;separator&quot; style=&quot;clear: both; text-align: center;&quot;&gt;&lt;a href=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhjIGWPLlK3rQ_29XDDMYdv6eQyRB8bPFjYSpWmrMsg45Mjq-_O8JyU7Ow6FesVprVtBdk9idtLP7C5DOHPH6dCrr5wp3peHvUJTqm4FpQAw6i3O1n41r3Bfw_0cQSWWyirH65y3JFdQgc/s1600/taal+volcano4.jpg&quot; imageanchor=&quot;1&quot; style=&quot;margin-left: 1em; margin-right: 1em;&quot;&gt;&lt;img border=&quot;0&quot; height=&quot;274&quot; src=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhjIGWPLlK3rQ_29XDDMYdv6eQyRB8bPFjYSpWmrMsg45Mjq-_O8JyU7Ow6FesVprVtBdk9idtLP7C5DOHPH6dCrr5wp3peHvUJTqm4FpQAw6i3O1n41r3Bfw_0cQSWWyirH65y3JFdQgc/s320/taal+volcano4.jpg&quot; width=&quot;320&quot; /&gt;&lt;/a&gt;&lt;/div&gt;&lt;br /&gt;
&lt;/div&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif;&quot;&gt;Taal Lake itself, has a sulfur  content that is higher than normal, and it is good for swimming.&lt;/span&gt;</content><link rel='replies' type='application/atom+xml' href='http://philippinevolcanoes.blogspot.com/feeds/7622724782276093159/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://philippinevolcanoes.blogspot.com/2011/11/taal-volcano-is-located-in-southern.html#comment-form' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/7622724782276093159'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/7622724782276093159'/><link rel='alternate' type='text/html' href='http://philippinevolcanoes.blogspot.com/2011/11/taal-volcano-is-located-in-southern.html' title='TAAL VOLCANO'/><author><name>Unknown</name><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='https://img1.blogblog.com/img/b16-rounded.gif'/></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiOqEn9KIQmhikEAW6pc6CtwAmPYj_LTNSi3PN5zVFuPjQY0T-ANbSOCuiMq-Le2KuLWPX5qoxo2mJCKyJJ05h2x5qc6ZWuzhS6BBDz1Ekbgvir5AgNgIj8lUGFEibwbtWzWFfwn-4CPtA/s72-c/taal+volcano2.jpg" height="72" width="72"/><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-5371504585591558867.post-4974077783230921040</id><published>2011-11-06T11:03:00.000-08:00</published><updated>2011-11-06T11:18:45.902-08:00</updated><category scheme="http://www.blogger.com/atom/ns#" term="fumarole"/><category scheme="http://www.blogger.com/atom/ns#" term="group of volcanic cones"/><category scheme="http://www.blogger.com/atom/ns#" term="island of Luzon"/><category scheme="http://www.blogger.com/atom/ns#" term="K-Ar dates"/><category scheme="http://www.blogger.com/atom/ns#" term="Philippines"/><category scheme="http://www.blogger.com/atom/ns#" term="Pocdol Mountains"/><category scheme="http://www.blogger.com/atom/ns#" term="stratovolcanos"/><category scheme="http://www.blogger.com/atom/ns#" term="volcanic complex"/><title type='text'>Mt. POCDOL VOLCANIC CONES IN ALBAY</title><content type='html'>&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;The volcanic &lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/11/mt-pocdol-volcanic-cones-in-albay.html&quot;&gt;Pocdol Mountains&lt;/a&gt; (also known as Bacon-Manito complex) are a &lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/11/mt-pocdol-volcanic-cones-in-albay.html&quot;&gt;group of volcanic cones&lt;/a&gt; between Saragon Bay and Albay Gulf in southern Luzon. &lt;/span&gt;&lt;br /&gt;
&lt;div class=&quot;separator&quot; style=&quot;clear: both; text-align: center;&quot;&gt;&lt;a href=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhOJ7DxVQtgcOJcF8bh-KCQhfjx3JoQP6DQkI8ANB3AyTyrxUvWJ5Zx01zwu8QAonQPc-TcCm57zef8r3-lsu3vtlxHWZD45jLz5qRpfJCJktRNCcqz3OZ3VE-e-aJU4SzoSZ7WEJXH0y4/s1600/pocdol+mountains&quot; imageanchor=&quot;1&quot; style=&quot;margin-left: 1em; margin-right: 1em;&quot;&gt;&lt;img border=&quot;0&quot; height=&quot;261&quot; src=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhOJ7DxVQtgcOJcF8bh-KCQhfjx3JoQP6DQkI8ANB3AyTyrxUvWJ5Zx01zwu8QAonQPc-TcCm57zef8r3-lsu3vtlxHWZD45jLz5qRpfJCJktRNCcqz3OZ3VE-e-aJU4SzoSZ7WEJXH0y4/s400/pocdol+mountains&quot; width=&quot;400&quot; /&gt;&lt;/a&gt;&lt;/div&gt;&lt;br /&gt;
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&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;The Pocdol Mountains form part of the boundary between the &lt;/span&gt;&lt;span style=&quot;color: black;&quot;&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;provinces&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt; of &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;Albay&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt; and &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;Sorsogon&lt;/span&gt;&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;&lt;span style=&quot;color: black;&quot;&gt;, in&lt;/span&gt; Region V, on&amp;nbsp;the &lt;/span&gt;&lt;span style=&quot;color: #0645ad; font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;&lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/11/mt-pocdol-volcanic-cones-in-albay.html&quot;&gt;island of Luzon&lt;/a&gt;&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;, in the &lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/11/mt-pocdol-volcanic-cones-in-albay.html&quot;&gt;Philippines&lt;/a&gt;.&lt;/span&gt;&lt;br /&gt;
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&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;The Pocdol Mountains are a &lt;/span&gt;&lt;span style=&quot;color: black; font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;volcanic group&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt; of &lt;/span&gt;&lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/11/mt-pocdol-volcanic-cones-in-albay.html&quot; title=&quot;Stratovolcano&quot;&gt;&lt;span style=&quot;color: #0645ad; font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;stratovolcanos&lt;/span&gt;&lt;/a&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt; in the &lt;/span&gt;&lt;span style=&quot;color: black; font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;Philippines&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;.The Pocdol Mountains have a triangular footprint of about 225 square kilometres (87 sq mi). &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;The highest point is reported as 1102 metres (3,615 ft) above sea level. &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;A &lt;/span&gt;&lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/11/mt-pocdol-volcanic-cones-in-albay.html&quot; title=&quot;Fumarole&quot;&gt;&lt;span style=&quot;color: #0645ad; font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;fumarole&lt;/span&gt;&lt;/a&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt; field that contains sulfataras and chloride hot springs, is reported to be located near the summit of the volcanic group.&lt;/span&gt;&lt;br /&gt;
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&lt;div class=&quot;separator&quot; style=&quot;clear: both; text-align: center;&quot;&gt;&lt;a href=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjxYz-g7RBfh9dqNYuH4USOGmSNG0iqixQTe4TNVrVfq0j5JmQ1DNjTCblqfYntG2v_5dwC1uZUcUyK526tD5QEgHQmPMrFVd6mXwY4xNQI2HhEA19XJCl2H9wqWicc_wlHiLKBRu0al-8/s1600/pocdol+mountains2&quot; imageanchor=&quot;1&quot; style=&quot;margin-left: 1em; margin-right: 1em;&quot;&gt;&lt;img border=&quot;0&quot; height=&quot;300&quot; src=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjxYz-g7RBfh9dqNYuH4USOGmSNG0iqixQTe4TNVrVfq0j5JmQ1DNjTCblqfYntG2v_5dwC1uZUcUyK526tD5QEgHQmPMrFVd6mXwY4xNQI2HhEA19XJCl2H9wqWicc_wlHiLKBRu0al-8/s400/pocdol+mountains2&quot; width=&quot;400&quot; /&gt;&lt;/a&gt;&lt;/div&gt;&lt;br /&gt;
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&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;The group is described by the Smithsonian Institution&#39;s Global Volcanism Program as &lt;/span&gt;&lt;span style=&quot;color: black;&quot;&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;fumarolic&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;.&lt;/span&gt;&lt;/span&gt;&lt;br /&gt;
&lt;h2&gt;&amp;nbsp;&lt;/h2&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;There are no reports of eruptions.&lt;/span&gt;&lt;br /&gt;
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&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;Several Pleistocene &lt;/span&gt;&lt;a class=&quot;mw-redirect&quot; href=&quot;http://philippinevolcanoes.blogspot.com/2011/11/mt-pocdol-volcanic-cones-in-albay.html&quot; title=&quot;Potassium-argon dating&quot;&gt;&lt;span style=&quot;color: #0645ad; font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;K-Ar dates&lt;/span&gt;&lt;/a&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt; have been obtained from the &lt;/span&gt;&lt;a class=&quot;mw-redirect&quot; href=&quot;http://philippinevolcanoes.blogspot.com/2011/11/mt-pocdol-volcanic-cones-in-albay.html&quot; title=&quot;Volcanic complex&quot;&gt;&lt;span style=&quot;color: #0645ad; font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;volcanic complex&lt;/span&gt;&lt;/a&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;. Most igneous rocks in the Pocdol Mountains consist of pyroxene andesites with minor amounts of dacite and basalts. The area is traversed by the San Vicente-Linao Fault, a splay of the Philippine Fault.&lt;/span&gt;&lt;br /&gt;
&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;Volcanic cones in the western part of the complex are dissected, but those in the eastern part are morphologically youthful.&lt;/span&gt;&lt;br /&gt;
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&lt;div class=&quot;separator&quot; style=&quot;clear: both; text-align: center;&quot;&gt;&lt;a href=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjN3c_DD634-Cf8c7bFC6asJ8WriFb0BGx-9qdSRLDnugMGTPwH78rfFgM6scV-oAdbanPBOqtFIHPoWgRBUXjyJQo9Tk5j-gThT6WB_zfBMtzyZT7bLV9znwR21RSrndo6q0Iyd11OoSY/s1600/Pocdol-Mountains3.jpg&quot; imageanchor=&quot;1&quot; style=&quot;margin-left: 1em; margin-right: 1em;&quot;&gt;&lt;img border=&quot;0&quot; height=&quot;265&quot; src=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjN3c_DD634-Cf8c7bFC6asJ8WriFb0BGx-9qdSRLDnugMGTPwH78rfFgM6scV-oAdbanPBOqtFIHPoWgRBUXjyJQo9Tk5j-gThT6WB_zfBMtzyZT7bLV9znwR21RSrndo6q0Iyd11OoSY/s400/Pocdol-Mountains3.jpg&quot; width=&quot;400&quot; /&gt;&lt;/a&gt;&lt;/div&gt;&lt;br /&gt;
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&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;The volcanic area is the host of various geothermal systems collectively called the Bacon-Manito geothermal field.&lt;/span&gt;&lt;br /&gt;
&lt;h2&gt;&lt;span class=&quot;editsection&quot;&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif;&quot;&gt;&lt;/span&gt;&lt;/span&gt;&amp;nbsp;&lt;/h2&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;The Global Volcanism Program lists the Pocdol Mountains as Fumarolic.&lt;/span&gt;&lt;br /&gt;
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Source: wikipedia.org</content><link rel='replies' type='application/atom+xml' href='http://philippinevolcanoes.blogspot.com/feeds/4974077783230921040/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://philippinevolcanoes.blogspot.com/2011/11/mt-pocdol-volcanic-cones-in-albay.html#comment-form' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/4974077783230921040'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/4974077783230921040'/><link rel='alternate' type='text/html' href='http://philippinevolcanoes.blogspot.com/2011/11/mt-pocdol-volcanic-cones-in-albay.html' title='Mt. POCDOL VOLCANIC CONES IN ALBAY'/><author><name>Unknown</name><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='https://img1.blogblog.com/img/b16-rounded.gif'/></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhOJ7DxVQtgcOJcF8bh-KCQhfjx3JoQP6DQkI8ANB3AyTyrxUvWJ5Zx01zwu8QAonQPc-TcCm57zef8r3-lsu3vtlxHWZD45jLz5qRpfJCJktRNCcqz3OZ3VE-e-aJU4SzoSZ7WEJXH0y4/s72-c/pocdol+mountains" height="72" width="72"/><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-5371504585591558867.post-8569337531394415290</id><published>2011-10-31T19:15:00.000-07:00</published><updated>2011-10-31T21:01:53.860-07:00</updated><category scheme="http://www.blogger.com/atom/ns#" term="active volcano"/><category scheme="http://www.blogger.com/atom/ns#" term="Island of Marinduque"/><category scheme="http://www.blogger.com/atom/ns#" term="most popular climb and hike on the island"/><category scheme="http://www.blogger.com/atom/ns#" term="Mount Malindig"/><category scheme="http://www.blogger.com/atom/ns#" term="mountaineers"/><title type='text'>MOUNT MALINDIG IN MARINDUQUE</title><content type='html'>&lt;center&gt;&lt;div style=&quot;text-align: justify;&quot;&gt;&lt;script type=&quot;text/javascript&quot;&gt;
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&lt;/div&gt;&lt;div style=&quot;text-align: justify;&quot;&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif;&quot;&gt;&lt;span style=&quot;font-size: large;&quot;&gt;&lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/10/mount-malindig-in-marinduque.html&quot;&gt;Mount Malindig&lt;/a&gt;&lt;span style=&quot;color: black;&quot;&gt; is considered a potentially &lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/10/mount-malindig-in-marinduque.html&quot;&gt;active volcano&lt;/a&gt;, in part because of the solfataric springs of Malbog. Its unique location, at the heart of Southern Tagalog, creates a panorama that encompasses Mindoro, Verde Island, and Southern Luzon all the way to Bicol and Burias Island. &lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style=&quot;text-align: justify;&quot;&gt;&lt;br /&gt;
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&lt;/div&gt;&lt;div style=&quot;text-align: justify;&quot;&gt;&lt;span style=&quot;color: black; font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;The Mountain is the largest on the &lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/10/mount-malindig-in-marinduque.html&quot;&gt;Island of Marinduque&lt;/a&gt; and the &lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/10/mount-malindig-in-marinduque.html&quot;&gt;most popular climb and hike on the island&lt;/a&gt; for &lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/10/mount-malindig-in-marinduque.html&quot;&gt;mountaineers&lt;/a&gt; and alike, known for its unique environmental biodiversity. It is the home of different species of wild orchids and other endemic wildlife. &lt;/span&gt;&lt;/div&gt;&lt;div style=&quot;text-align: justify;&quot;&gt;&lt;br /&gt;
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&lt;/div&gt;&lt;div style=&quot;text-align: justify;&quot;&gt;&lt;span style=&quot;color: black; font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;Due to its height above 1,000 meters above sea level, by law is has been identified as a protected area. The dormant volcano has three peaks, the Trek and climb to the peak is rated as easy to moderate. After passing the Radio Station base on the mountain, it has been known to be a mossy and closed canopy forest trek with regular foggy surroundings. It is also used by the Buenavista townfolks as a cattle grazing area.&lt;/span&gt;&lt;/div&gt;&lt;div style=&quot;text-align: justify;&quot;&gt;&lt;br /&gt;
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&lt;/div&gt;&lt;div style=&quot;text-align: justify;&quot;&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;The age of the most recent eruptions of Malindig volcano is not known, but hot springs are located at its western foot.&lt;/span&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://philippinevolcanoes.blogspot.com/feeds/8569337531394415290/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://philippinevolcanoes.blogspot.com/2011/10/mount-malindig-in-marinduque.html#comment-form' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/8569337531394415290'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/8569337531394415290'/><link rel='alternate' type='text/html' href='http://philippinevolcanoes.blogspot.com/2011/10/mount-malindig-in-marinduque.html' title='MOUNT MALINDIG IN MARINDUQUE'/><author><name>Unknown</name><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='https://img1.blogblog.com/img/b16-rounded.gif'/></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgZvQMzbvYJ5-jIfdydt0bOZ5HFWyflSNkPvfirrWis83jvxTes06AKj9ib58_qWVBOeWKTyB63eXj6UAVU33RFZUDfHXJsdDZ-19dwLo1-JWMYyJ93z0kicrpeUwlQUkHjWNRT2tg4b_Y/s72-c/Mt.+Malindig3.jpg" height="72" width="72"/><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-5371504585591558867.post-6429335645971553690</id><published>2011-10-25T21:54:00.000-07:00</published><updated>2012-12-05T09:22:42.970-08:00</updated><category scheme="http://www.blogger.com/atom/ns#" term="catchment"/><category scheme="http://www.blogger.com/atom/ns#" term="endemic and endangered species"/><category scheme="http://www.blogger.com/atom/ns#" term="island of Mindanao"/><category scheme="http://www.blogger.com/atom/ns#" term="Misamis Occidental"/><category scheme="http://www.blogger.com/atom/ns#" term="Mount Malindang"/><category scheme="http://www.blogger.com/atom/ns#" term="mountain range"/><category scheme="http://www.blogger.com/atom/ns#" term="Philippines"/><category scheme="http://www.blogger.com/atom/ns#" term="Zamboanga del Norte"/><category scheme="http://www.blogger.com/atom/ns#" term="Zamboanga del Sur"/><title type='text'>MOUNT MALINDANG</title><content type='html'>&lt;center&gt;
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&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif;&quot;&gt;Mount Malindang is a complex volcano located in the province of Misamis Occidental in the southern island of Mindanao, Philippines. The least studied mountain range was formed through several volcanic activities some of which could be historical, evident by the presence of two calderas, surrounded by high rock walls, cinder cones, dome volcano plugs, two sulfurous hot springs, and a crater lake named Lake Duminagat. The amphitheater structures have extensive distribution of volcanic rocks, carbonized wood that are found in pyroclastic deposits. The entire mountain range is dissected by several canyons and ravines making its terrain very rugged and the forested slopes covered with beautiful scenery.&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif;&quot;&gt;The mountain and its outlying areas, some are unexplored, are home to some of the endemic and endangered species in the Philippines, which include:&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;color: black; font-family: Arial, Helvetica, sans-serif;&quot;&gt;Philippine Eagle&lt;/span&gt;&lt;span style=&quot;color: black; font-family: Arial, Helvetica, sans-serif;&quot;&gt; &lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;color: black; font-family: Arial, Helvetica, sans-serif;&quot;&gt;Rufous Hornbill&lt;/span&gt;&lt;span style=&quot;color: black; font-family: Arial, Helvetica, sans-serif;&quot;&gt; &lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;color: black; font-family: Arial, Helvetica, sans-serif;&quot;&gt;Tarsier&lt;/span&gt;&lt;span style=&quot;color: black; font-family: Arial, Helvetica, sans-serif;&quot;&gt; &lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;color: black; font-family: Arial, Helvetica, sans-serif;&quot;&gt;Flying Lemur&lt;/span&gt;&lt;span style=&quot;color: black; font-family: Arial, Helvetica, sans-serif;&quot;&gt; &lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;color: black; font-family: Arial, Helvetica, sans-serif;&quot;&gt;Philippine Deer&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;color: black; font-family: Arial, Helvetica, sans-serif;&quot;&gt;Long-tailed Macaque&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;color: black; font-family: Arial, Helvetica, sans-serif;&quot;&gt;Asian Palm Civet&lt;/span&gt;&lt;span style=&quot;color: black; font-family: Arial, Helvetica, sans-serif;&quot;&gt; &lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;color: black; font-family: Arial, Helvetica, sans-serif;&quot;&gt;Philippine Hawk-eagle&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;color: black; font-family: Arial, Helvetica, sans-serif;&quot;&gt;Rough-armored tree frog&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;color: black; font-family: Arial, Helvetica, sans-serif;&quot;&gt;Water monitor lizard&lt;/span&gt;&lt;span style=&quot;color: black; font-family: Arial, Helvetica, sans-serif;&quot;&gt; &lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;color: black; font-family: Arial, Helvetica, sans-serif;&quot;&gt;Philippine warty pig&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;color: black; font-family: Arial, Helvetica, sans-serif;&quot;&gt;Philippine hanging parakeet&lt;/span&gt;&lt;span style=&quot;color: black; font-family: Arial, Helvetica, sans-serif;&quot;&gt;/&lt;/span&gt;&lt;span style=&quot;color: black; font-family: Arial, Helvetica, sans-serif;&quot;&gt;Colasisi&lt;/span&gt;&lt;span style=&quot;color: black; font-family: Arial, Helvetica, sans-serif;&quot;&gt; &lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;color: black; font-family: Arial, Helvetica, sans-serif;&quot;&gt;Philippine Woodpecker&lt;/span&gt;&lt;span style=&quot;color: black; font-family: Arial, Helvetica, sans-serif;&quot;&gt; &lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;color: black;&quot;&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif;&quot;&gt;Greater Mindanao Shrew&lt;span style=&quot;font-size: large;&quot;&gt; &lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif;&quot;&gt;&lt;span style=&quot;color: black;&quot;&gt;Mount Malindang and its adjoining mountain range is a &lt;/span&gt;&lt;span style=&quot;color: black;&quot;&gt;catchment&lt;/span&gt;&lt;span style=&quot;color: black;&quot;&gt; area which drains water through 49 rivers and streams, and numerous creeks. It provides potable water for domestic, agricultural and other uses to more than one million inhabitants of &lt;/span&gt;&lt;span style=&quot;color: black;&quot;&gt;Misamis Occidental&lt;/span&gt;&lt;span style=&quot;color: black;&quot;&gt; and the eastern parts of &lt;/span&gt;&lt;span style=&quot;color: black;&quot;&gt;Zamboanga del Norte&lt;/span&gt;&lt;span style=&quot;color: black;&quot;&gt; and Zamboanga del Sur.&lt;/span&gt;&lt;/span&gt;&lt;br /&gt;
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&lt;br /&gt;</content><link rel='replies' type='application/atom+xml' href='http://philippinevolcanoes.blogspot.com/feeds/6429335645971553690/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://philippinevolcanoes.blogspot.com/2011/10/mount-malindang.html#comment-form' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/6429335645971553690'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/6429335645971553690'/><link rel='alternate' type='text/html' href='http://philippinevolcanoes.blogspot.com/2011/10/mount-malindang.html' title='MOUNT MALINDANG'/><author><name>Unknown</name><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='https://img1.blogblog.com/img/b16-rounded.gif'/></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjA1gCTBHeopWoYpo9-7uEGOaEciGNuUflG3T-qAMeAQ6bIW2Us0lUPdGW_TB3VzgxL2Q-DyWC1_P1JxYmTj-c7RAE-6NzQa0M4rLL36VUaJVl7ij18cGXeTWtvLTFaQREkHWQ5D7oJFYE/s72-c/Mt+malindang3.jpg" height="72" width="72"/><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-5371504585591558867.post-2172698801269067267</id><published>2011-10-21T17:33:00.000-07:00</published><updated>2011-10-25T10:48:45.521-07:00</updated><category scheme="http://www.blogger.com/atom/ns#" term="Luzon Island"/><category scheme="http://www.blogger.com/atom/ns#" term="Mount Arayat"/><category scheme="http://www.blogger.com/atom/ns#" term="Mount Arayat National Park"/><category scheme="http://www.blogger.com/atom/ns#" term="popular tourist destination"/><category scheme="http://www.blogger.com/atom/ns#" term="Republic of the Philippines"/><category scheme="http://www.blogger.com/atom/ns#" term="stratovolcano"/><category scheme="http://www.blogger.com/atom/ns#" term="White Rock"/><title type='text'>MT. ARAYAT IN PAMPANGA</title><content type='html'>&lt;center&gt;&lt;p style=&quot;text-align: justify;&quot;&gt;&lt;script type=&quot;text/javascript&quot;&gt;// &lt;![CDATA[
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&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif;&quot;&gt;&lt;span style=&quot;font-size: large;&quot;&gt;&lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/10/mt-arayat-in-pampanga.html&quot;&gt;Mount Arayat&lt;/a&gt; is an extinct &lt;/span&gt;&lt;/span&gt;&lt;span style=&quot;color: #0645ad; font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;&lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/10/mt-arayat-in-pampanga.html&quot;&gt;stratovolcano&lt;/a&gt;&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt; on &lt;/span&gt;&lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/10/mt-arayat-in-pampanga.html&quot;&gt;&lt;span style=&quot;color: #0645ad; font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;Luzon Island&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;, &lt;/span&gt;&lt;span style=&quot;color: #0645ad; font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;Philippines&lt;/span&gt;&lt;/a&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;, rising to a height of 1,026 metres (3,366 ft) There is no recorded eruption of the volcano, and its last activity probably dates to the &lt;/span&gt;&lt;span style=&quot;color: black;&quot;&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;Holocene&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif;&quot;&gt;&lt;span style=&quot;font-size: large;&quot;&gt; era.&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br /&gt;
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&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;The volcano is located in a flat agricultural region. &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;The Volcano is a &lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/10/mt-arayat-in-pampanga.html&quot;&gt;popular tourist destination&lt;/a&gt; for people visiting the central plains.&lt;/span&gt;&lt;br /&gt;
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&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;Two trails lead to the peaks of Mount Arayat. &lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/10/mt-arayat-in-pampanga.html&quot;&gt;Mount Arayat National Park&lt;/a&gt; Located at San Juan Baño in &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;Arayat, Pampanga&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt; has a trail to the southern Peak, taking around 3–4 hours to reach the peak. The Southern Peak offers views of Central Luzon, including a view of &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;Pampanga River&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;. &lt;/span&gt;&lt;br /&gt;
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&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;The collapsed western Slope that forms the other half of its Caldera like crater can also be seen. It offers a view of the mountains of &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;Zambales&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt; and &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;Bataan&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt; (to the west), and the mountains of the Sierra Madre range (to the east). The northern or higher Peak can be accessed on a route from Pampanga Agricultural College in &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;Magalang, Pampanga&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif;&quot;&gt;&lt;span style=&quot;font-size: large;&quot;&gt;, taking a similar time to reach the peak, however, this route takes you through the Arayat Ampitheatre and the so-called &lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/10/mt-arayat-in-pampanga.html&quot;&gt;White Rock&lt;/a&gt; .&lt;/span&gt;&lt;/span&gt;&lt;br /&gt;
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&lt;sup&gt;&lt;span style=&quot;font-family: Arial; font-size: small;&quot;&gt;Source: wikipedia.org&lt;/span&gt;&lt;/sup&gt;</content><link rel='replies' type='application/atom+xml' href='http://philippinevolcanoes.blogspot.com/feeds/2172698801269067267/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://philippinevolcanoes.blogspot.com/2011/10/mt-arayat-in-pampanga.html#comment-form' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/2172698801269067267'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/2172698801269067267'/><link rel='alternate' type='text/html' href='http://philippinevolcanoes.blogspot.com/2011/10/mt-arayat-in-pampanga.html' title='MT. ARAYAT IN PAMPANGA'/><author><name>Unknown</name><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='https://img1.blogblog.com/img/b16-rounded.gif'/></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgUOK647RHCvEE0kRgPCMI1dV5Ov9QMxu0hrwCeeJBReTZYj2ffZyvRh3nw7CWYSxTk-ocFakg9U5rsQQqQYsc2VuIyHWzTIiXLeaXOfrQl0aZvQDcHI0Z5iKMF4cqd7V7te7hIu9Drfu4/s72-c/Mt.+Arayat.jpg" height="72" width="72"/><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-5371504585591558867.post-4403927193258697219</id><published>2011-10-16T20:08:00.001-07:00</published><updated>2017-03-28T14:26:14.061-07:00</updated><category scheme="http://www.blogger.com/atom/ns#" term="Bulusan Volcano"/><category scheme="http://www.blogger.com/atom/ns#" term="four craters"/><category scheme="http://www.blogger.com/atom/ns#" term="hot springs"/><category scheme="http://www.blogger.com/atom/ns#" term="Mount Bulusan"/><category scheme="http://www.blogger.com/atom/ns#" term="Philippine Volcanoes"/><category scheme="http://www.blogger.com/atom/ns#" term="Republic of the Philippines"/><category scheme="http://www.blogger.com/atom/ns#" term="volcanoes in Sorsogon"/><title type='text'>MT. BULUSAN IN SORSOGON</title><content type='html'>&lt;center&gt;
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&lt;a href=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgeAPAcvi8xXSedZX7IXNnJ_uJ_xbgrX-C41ujaOQqAg8ydp9j3yjZRQIMpqTfF2AgOdzyluT7E-_ZsxibLZ9e7Cew5jGfaNapgaFlY3z81lo4kV8VZstcHSgmVGz6jMWs6K33Qkx3uVkk/s1600/BULUSAN3.jpg&quot; imageanchor=&quot;1&quot; style=&quot;margin-left: 1em; margin-right: 1em;&quot;&gt;&lt;img border=&quot;0&quot; height=&quot;359&quot; src=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgeAPAcvi8xXSedZX7IXNnJ_uJ_xbgrX-C41ujaOQqAg8ydp9j3yjZRQIMpqTfF2AgOdzyluT7E-_ZsxibLZ9e7Cew5jGfaNapgaFlY3z81lo4kV8VZstcHSgmVGz6jMWs6K33Qkx3uVkk/s640/BULUSAN3.jpg&quot; width=&quot;640&quot; /&gt;&lt;/a&gt;&lt;/div&gt;
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&lt;span style=&quot;font-size: x-small;&quot;&gt;Photo from:&amp;nbsp; &lt;em&gt;panoramio.com&lt;/em&gt;&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Mount Bulusan, or Bulusan Volcano, is the southernmost volcano on Luzon Island in the Republic of the Philippines. It is situated in the province of Sorsogon in the Bicol region, 70 km (43 mi) southeast of Mayon Volcano and approximately 250 km (160 mi) southeast of the Philippine capital of Manila.&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif; font-size: large;&quot;&gt;&lt;span style=&quot;font-size: x-small;&quot;&gt;Photo from:&amp;nbsp; &lt;span id=&quot;rg_hr&quot;&gt;&lt;em&gt;commons.wikimedia.org&lt;/em&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-size: small;&quot;&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Mount Bulusan is an active stratovolcano located at the south central part of &lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Sorsogon&lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt; province. It is basically made up of lava flows and domes. It forms part of the &lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Bicol&lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt; Volcanic Chain that stretches from &lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Camarines Norte&lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt; in the north and &lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Sorsogon&lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt; in the south. It is 280 km North Northeast of Canlaon and South Southeast of &lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Mayon Volcano&lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;.&lt;/span&gt;&lt;/span&gt;&lt;/div&gt;
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&lt;a href=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhSsdCLij7VFD6Go9nuywn0-nk_0ZzdrQ8vvCpQr3cK9zxfiqCIuw3bZcUECUUC5rNS8hEIG5ImRV01E_YTac1i5XMozGsoYqR3EzYMkgdcsvWspjLfU8hKAA11GwA7OC-TayJ2cv81eBs/s1600/BULUSAN8.jpg&quot; imageanchor=&quot;1&quot; style=&quot;margin-left: 1em; margin-right: 1em;&quot;&gt;&lt;img border=&quot;0&quot; src=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhSsdCLij7VFD6Go9nuywn0-nk_0ZzdrQ8vvCpQr3cK9zxfiqCIuw3bZcUECUUC5rNS8hEIG5ImRV01E_YTac1i5XMozGsoYqR3EzYMkgdcsvWspjLfU8hKAA11GwA7OC-TayJ2cv81eBs/s1600/BULUSAN8.jpg&quot; /&gt;&lt;/a&gt;&lt;/div&gt;
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&lt;span style=&quot;font-size: x-small;&quot;&gt;Photo from:&amp;nbsp; &lt;em&gt;panoramio.com&lt;/em&gt;&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;&lt;span style=&quot;font-size: small;&quot;&gt;Mount Bulusan is about 1559 m above sea level and covers about 400 sq km. Its summit crater is 1000 feet (300 m) in diameter. There are numerous lava flows on its flanks. There are three craters on the southeast flank, its lower two are crater lakes.  - &lt;em&gt;wikipilipinas.org&lt;/em&gt;&lt;/span&gt;&lt;/span&gt;&lt;/div&gt;
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&lt;a href=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEijBPEhlFrxszlAMvMhsSolbuy4RGf5YFUkgnQ2W1yWfpq8LBiABdsUYx-loMG_PCJB_kfhMq5AFnj798taHqEQ9as6daPiOOElzHCEF7y9LWKM82h-jlSTlH4UsnALUQSm0i9TtQNhsJQ/s1600/BULUSAN4.jpg&quot; imageanchor=&quot;1&quot; style=&quot;margin-left: 1em; margin-right: 1em;&quot;&gt;&lt;img border=&quot;0&quot; src=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEijBPEhlFrxszlAMvMhsSolbuy4RGf5YFUkgnQ2W1yWfpq8LBiABdsUYx-loMG_PCJB_kfhMq5AFnj798taHqEQ9as6daPiOOElzHCEF7y9LWKM82h-jlSTlH4UsnALUQSm0i9TtQNhsJQ/s1600/BULUSAN4.jpg&quot; /&gt;&lt;/a&gt;&lt;/div&gt;
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&lt;span style=&quot;font-size: x-small;&quot;&gt;Photo from:&amp;nbsp;&lt;em&gt; tripadvisor.com&lt;/em&gt;&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-size: small;&quot;&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Bulusan is classified by &lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;volcanologists&lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt; as a &lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;stratovolcano&lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt; (composite volcano) and covers the northeast rim of Irosin &lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;caldera&lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt; that was formed about 40,000 years before present. It has a peak elevation of 1,565 m (5,135 ft) above sea level with a base diameter of 15 km (9.3 mi).&lt;/span&gt;&lt;/span&gt;&lt;/div&gt;
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&lt;a href=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEi3gqHnLsxOspwPmv9OdsLyV6VHyxlZW9VtaTOPXRhYpWs4QaML0v7wjfumyUaJ9AERbwVFRlQ7lDV2unvVb9Ttgbk5zF8TgtSXjQAwVUZ4HvobdoLXqf6EauVsJmGyQ9tni4MIDpANfo4/s1600/BULUSAN7.jpg&quot; imageanchor=&quot;1&quot; style=&quot;margin-left: 1em; margin-right: 1em;&quot;&gt;&lt;img border=&quot;0&quot; src=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEi3gqHnLsxOspwPmv9OdsLyV6VHyxlZW9VtaTOPXRhYpWs4QaML0v7wjfumyUaJ9AERbwVFRlQ7lDV2unvVb9Ttgbk5zF8TgtSXjQAwVUZ4HvobdoLXqf6EauVsJmGyQ9tni4MIDpANfo4/s1600/BULUSAN7.jpg&quot; /&gt;&lt;/a&gt;&lt;/div&gt;
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&lt;span style=&quot;font-size: x-small;&quot;&gt;Photo from:&amp;nbsp; &lt;/span&gt;&lt;span style=&quot;font-size: x-small;&quot;&gt;&lt;em&gt;skyscrapercity.com&lt;/em&gt;&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-size: small;&quot;&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Located around the mountain are four craters and four &lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;hot springs&lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;. Crater No. 1, called Blackbird Lake, is 20 m (66 ft) in diameter and 15 m (49 ft) deep. The oval Crater No. 2 is 60 by 30 m (200 by 98 ft) and 15 m (49 ft). Crater No. 3 is about 90 m (300 ft) in diameter and 20 m (66 ft) deep and Crater No. 4, which is near the northeastern, rim opened during the 1981 eruption. There is a&lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;lso a 100-metre (330 ft) fissure measuring 5 to 8 m (16 to 26 ft) wide below Crater No. 4.&lt;/span&gt;&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-size: x-small;&quot;&gt;Photo from:&amp;nbsp; &lt;em&gt;panoramio.com&lt;/em&gt;&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif; font-size: small;&quot;&gt;Its hot springs are San Benon Springs, Mapaso Springs, San Vicente Springs, Masacrot Springs.&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif; font-size: small;&quot;&gt;Its adjacent volcanic edifices are Mt. Homahan, Mt. Binitacan, Mt. Batuan, Mt. Calungalan, Mt. Calaunan, Mt. Tabon-Tabon, Mt. Juban, and Mt. Jormajan.&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;&lt;/span&gt;&lt;span style=&quot;font-size: small;&quot;&gt; &lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-size: small;&quot;&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;Bulusan is generally known for its sudden steam-driven or &lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;phreatic&lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt; explosions. It has erupted 15 times since 1885 and is considered as the 4th most &lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt;active volcano&lt;/span&gt;&lt;span style=&quot;font-family: &amp;quot;arial&amp;quot; , &amp;quot;helvetica&amp;quot; , sans-serif;&quot;&gt; in the Philippines after Mayon, Taal, and Kanlaon. - &lt;em&gt;wikipedia.org&lt;/em&gt;&lt;/span&gt;&lt;/span&gt;&lt;/div&gt;
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&lt;span style=&quot;font-size: x-small;&quot;&gt;Photo from:&amp;nbsp; &lt;em&gt;backpackingphilippines.com&lt;/em&gt;&lt;/span&gt;&lt;/div&gt;
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&amp;nbsp;&lt;b&gt;&lt;span style=&quot;color: #990000;&quot;&gt;Related Link:&lt;/span&gt;&lt;/b&gt;&amp;nbsp; &lt;i&gt;&lt;a href=&quot;http://www.traveltothephilippines.info/2017/01/31/the-mighty-bulusan-volcano-in-sorsogon/&quot;&gt;http://www.traveltothephilippines.info/2017/01/31/the-mighty-bulusan-volcano-in-sorsogon/&lt;/a&gt;&lt;/i&gt;&lt;br /&gt;
&lt;i&gt;&lt;br /&gt;&lt;/i&gt;
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</content><link rel='replies' type='application/atom+xml' href='http://philippinevolcanoes.blogspot.com/feeds/4403927193258697219/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://philippinevolcanoes.blogspot.com/2011/10/mt-bulusan-in-sorsogon.html#comment-form' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/4403927193258697219'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/4403927193258697219'/><link rel='alternate' type='text/html' href='http://philippinevolcanoes.blogspot.com/2011/10/mt-bulusan-in-sorsogon.html' title='MT. BULUSAN IN SORSOGON'/><author><name>Unknown</name><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='https://img1.blogblog.com/img/b16-rounded.gif'/></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgeAPAcvi8xXSedZX7IXNnJ_uJ_xbgrX-C41ujaOQqAg8ydp9j3yjZRQIMpqTfF2AgOdzyluT7E-_ZsxibLZ9e7Cew5jGfaNapgaFlY3z81lo4kV8VZstcHSgmVGz6jMWs6K33Qkx3uVkk/s72-c/BULUSAN3.jpg" height="72" width="72"/><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-5371504585591558867.post-2977932631028330479</id><published>2011-10-11T13:35:00.000-07:00</published><updated>2011-10-25T10:46:10.643-07:00</updated><category scheme="http://www.blogger.com/atom/ns#" term="Canlaon Volcano"/><category scheme="http://www.blogger.com/atom/ns#" term="Canlaon&#39;s eruption"/><category scheme="http://www.blogger.com/atom/ns#" term="crater-lake"/><category scheme="http://www.blogger.com/atom/ns#" term="most active volcano"/><category scheme="http://www.blogger.com/atom/ns#" term="Negros Island"/><category scheme="http://www.blogger.com/atom/ns#" term="volcanic edifice"/><title type='text'>CANLAON VOLCANO</title><content type='html'>&lt;center&gt;&lt;br /&gt;
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&lt;div style=&quot;text-align: justify;&quot;&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;&lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/10/canlaon-volcano.html&quot;&gt;Canlaon Volcano&lt;/a&gt;, a large stratovolcano, is located in the north central  portion of &lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/10/canlaon-volcano.html&quot;&gt;Negros Island&lt;/a&gt;. &lt;/span&gt;&lt;/div&gt;&lt;div style=&quot;text-align: justify;&quot;&gt;&lt;br /&gt;
&lt;div class=&quot;separator&quot; style=&quot;clear: both; text-align: center;&quot;&gt;&lt;a href=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEizROJklkDnpuUkXNQdrj0BjAghUh3DTYcYfEi5qhpFiAFqAgiEhjb01LF9e-q2nGTqyTDdvQpko6SuzgPHUAWYBexyqp4thOenOg7UzHcaRaxEvyM9uUI08fW9UJzwGyChsTnB6LxxALw/s1600/Canlaon+Volcano2.jpg&quot; imageanchor=&quot;1&quot; style=&quot;margin-left: 1em; margin-right: 1em;&quot;&gt;&lt;img border=&quot;0&quot; height=&quot;244&quot; src=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEizROJklkDnpuUkXNQdrj0BjAghUh3DTYcYfEi5qhpFiAFqAgiEhjb01LF9e-q2nGTqyTDdvQpko6SuzgPHUAWYBexyqp4thOenOg7UzHcaRaxEvyM9uUI08fW9UJzwGyChsTnB6LxxALw/s320/Canlaon+Volcano2.jpg&quot; width=&quot;320&quot; /&gt;&lt;/a&gt;&lt;/div&gt;&lt;br /&gt;
&lt;/div&gt;&lt;div style=&quot;text-align: justify;&quot;&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;Canlaon has a maximum elevation of 2435 m and a basal diameter of 30 km. &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;Canlaon consists of a multitude of craters and parasitic cones aligned  linearly, with an older caldera in its central portion. Most of the older  cratershave formed lakes or lagoons. The &lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/10/canlaon-volcano.html&quot;&gt;volcanic edifice&lt;/a&gt; has been built by  airfall deposits, lava agglutinates and lava flows, pyroclastic flows and lahar. &lt;/span&gt;&lt;/div&gt;&lt;div style=&quot;text-align: justify;&quot;&gt;&lt;br /&gt;
&lt;div class=&quot;separator&quot; style=&quot;clear: both; text-align: center;&quot;&gt;&lt;a href=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjBHLBOXBgfMYEccbPXyR5_G4dGJE3vhxP-SZ-xYXBiP6_8xfUb2RY-KAhj3QgWuuSVGgUyZ5heAgrCwsiYEbYU-TkJXNGSRxwZTELm6K4ErQtqXkLsDg5uZn9m1R3Dhz5N0iNzbPjSaS0/s1600/Canlaon+Volcano.jpg&quot; imageanchor=&quot;1&quot; style=&quot;margin-left: 1em; margin-right: 1em;&quot;&gt;&lt;img border=&quot;0&quot; height=&quot;213&quot; src=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjBHLBOXBgfMYEccbPXyR5_G4dGJE3vhxP-SZ-xYXBiP6_8xfUb2RY-KAhj3QgWuuSVGgUyZ5heAgrCwsiYEbYU-TkJXNGSRxwZTELm6K4ErQtqXkLsDg5uZn9m1R3Dhz5N0iNzbPjSaS0/s320/Canlaon+Volcano.jpg&quot; width=&quot;320&quot; /&gt;&lt;/a&gt;&lt;/div&gt;&lt;br /&gt;
&lt;/div&gt;&lt;div style=&quot;text-align: justify;&quot;&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;The earliest record of &lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/10/canlaon-volcano.html&quot;&gt;Canlaon&#39;s eruption&lt;/a&gt; dates back to 1866. Since then, it  has had at least 15 eruption periods, the latest occuring&amp;nbsp;in 1988.&lt;/span&gt;&lt;/div&gt;&lt;div style=&quot;text-align: justify;&quot;&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt; &lt;/span&gt;&lt;br /&gt;
&lt;div class=&quot;separator&quot; style=&quot;clear: both; text-align: center;&quot;&gt;&lt;a href=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhKiIVziGw6Svh74RjD8TkJI-2TcfFkPWZ6ptG3qesi9kMkJsOLeJQJSNGm1gD7y_TYv_NSk7NXH5Bx6C7VoiOQkH8OsjiqcnzzI3h8k4oEgKDxpUdm0AiqnhgOLaWeEP6wGXKPOrmuF9A/s1600/Canlaon+Volcano3.jpg&quot; imageanchor=&quot;1&quot; style=&quot;margin-left: 1em; margin-right: 1em;&quot;&gt;&lt;img border=&quot;0&quot; height=&quot;213&quot; src=&quot;https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhKiIVziGw6Svh74RjD8TkJI-2TcfFkPWZ6ptG3qesi9kMkJsOLeJQJSNGm1gD7y_TYv_NSk7NXH5Bx6C7VoiOQkH8OsjiqcnzzI3h8k4oEgKDxpUdm0AiqnhgOLaWeEP6wGXKPOrmuF9A/s320/Canlaon+Volcano3.jpg&quot; width=&quot;320&quot; /&gt;&lt;/a&gt;&lt;/div&gt;&lt;br /&gt;
&lt;/div&gt;&lt;div style=&quot;text-align: justify;&quot;&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;Canlaon volcano (also spelled Kanlaon), the &lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/10/canlaon-volcano.html&quot;&gt;most active&amp;nbsp;volcano&lt;/a&gt; in&amp;nbsp;&amp;nbsp;the central  Philippines, forms the highest point on the island of Negros. &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;The summit of Canlaon contains a broad northern crater with  a &lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;&lt;span id=&quot;goog_293331054&quot;&gt;&lt;/span&gt;&lt;a href=&quot;http://www.blogger.com/&quot;&gt;crater-lake&lt;/a&gt;&lt;/span&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt; &lt;span id=&quot;goog_293331055&quot;&gt;&lt;/span&gt;and a  smaller, but higher, historically active crater to the south. &lt;/span&gt;&lt;/div&gt;&lt;div style=&quot;text-align: justify;&quot;&gt;&lt;br /&gt;
&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://philippinevolcanoes.blogspot.com/feeds/2977932631028330479/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://philippinevolcanoes.blogspot.com/2011/10/canlaon-volcano.html#comment-form' title='2 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/2977932631028330479'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/2977932631028330479'/><link rel='alternate' type='text/html' href='http://philippinevolcanoes.blogspot.com/2011/10/canlaon-volcano.html' title='CANLAON VOLCANO'/><author><name>Unknown</name><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='https://img1.blogblog.com/img/b16-rounded.gif'/></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEizROJklkDnpuUkXNQdrj0BjAghUh3DTYcYfEi5qhpFiAFqAgiEhjb01LF9e-q2nGTqyTDdvQpko6SuzgPHUAWYBexyqp4thOenOg7UzHcaRaxEvyM9uUI08fW9UJzwGyChsTnB6LxxALw/s72-c/Canlaon+Volcano2.jpg" height="72" width="72"/><thr:total>2</thr:total></entry><entry><id>tag:blogger.com,1999:blog-5371504585591558867.post-3642609465037654538</id><published>2011-10-06T10:38:00.000-07:00</published><updated>2011-11-09T18:11:55.614-08:00</updated><category scheme="http://www.blogger.com/atom/ns#" term="Babuyan Channel"/><category scheme="http://www.blogger.com/atom/ns#" term="Babuyan Claro"/><category scheme="http://www.blogger.com/atom/ns#" term="Balintang Channel"/><category scheme="http://www.blogger.com/atom/ns#" term="Cagayan Valley"/><category scheme="http://www.blogger.com/atom/ns#" term="earthquakes"/><category scheme="http://www.blogger.com/atom/ns#" term="Luzon Island"/><category scheme="http://www.blogger.com/atom/ns#" term="Mt. Babuyan"/><category scheme="http://www.blogger.com/atom/ns#" term="Philippines"/><category scheme="http://www.blogger.com/atom/ns#" term="PHILVOLCS"/><category scheme="http://www.blogger.com/atom/ns#" term="volcanic activity"/><category scheme="http://www.blogger.com/atom/ns#" term="volcanologists"/><title type='text'>BABUYAN CLARO</title><content type='html'>&lt;center&gt;&lt;div style=&quot;text-align: justify;&quot;&gt;&lt;script type=&quot;text/javascript&quot;&gt;
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&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;&lt;b&gt;&lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/10/babuyan-claro.html&quot;&gt;Babuyan Claro&lt;/a&gt;&lt;/b&gt; is a&lt;span style=&quot;color: black;&quot;&gt; volcano located in the Babuyan Islands, an archipelago in the Luzon Strait north of &lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/10/babuyan-claro.html&quot;&gt;Luzon Island&lt;/a&gt;, in the &lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/10/babuyan-claro.html&quot;&gt;Philippines&lt;/a&gt;. It is separated from Luzon by the &lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/10/babuyan-claro.html&quot;&gt;Babuyan Channel&lt;/a&gt;, and from the Batanes Islands to the north by the &lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/10/babuyan-claro.html&quot;&gt;Balintang Channel&lt;/a&gt;.&amp;nbsp;  It is in the province of Cagayan in the &lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/10/babuyan-claro.html&quot;&gt;Cagayan Valley&lt;/a&gt; Region.&lt;/span&gt; &lt;/span&gt;&lt;br /&gt;
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Babuyan Claro has erupted four times: in 1831, 1860, 1913 and 1917. All eruptions were either strombolian or phreatomagmatic.&lt;/span&gt;&lt;br /&gt;
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&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;Babuyan island consists of five &lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/10/babuyan-claro.html&quot;&gt;volcanic centers&lt;/a&gt; ranging in age from 1.7 Million years to present. &lt;/span&gt;&lt;br /&gt;
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&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;Mt. Babuyan is the &lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/10/babuyan-claro.html&quot;&gt;youngest volcano&lt;/a&gt; on the island and has a volume of 3 cubic km. Eruptions at Babuyan Claro are strombolian  and phreatomagmatic. &lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/10/babuyan-claro.html&quot;&gt;Askedna hot springs&lt;/a&gt; are located on  the southern slopes of the volcano. &lt;/span&gt;&lt;br /&gt;
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&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;In July 1993, there were reports of &lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/10/babuyan-claro.html&quot;&gt;earthquakes&lt;/a&gt; and an alleged  drying up of vegetation at the upper slopes and summit area of the  volcano but volcanologists said the earthquakes were of tectonic origins and there was no significant change in the &lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/10/babuyan-claro.html&quot;&gt;volcanic activity&lt;/a&gt;.&lt;/span&gt;&lt;br /&gt;
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&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif;&quot;&gt;&lt;span style=&quot;font-size: large;&quot;&gt;In February 2004, there were reports of grayish steam clouds  hovering above the summit but &lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/10/babuyan-claro.html&quot;&gt;volcanologists&lt;/a&gt;&lt;span style=&quot;color: black;&quot;&gt; from &lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;strong&gt;&lt;span style=&quot;color: black; font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt;&lt;a href=&quot;http://philippinevolcanoes.blogspot.com/2011/10/babuyan-claro.html&quot;&gt;Phivolcs&lt;/a&gt;&lt;/span&gt;&lt;/strong&gt;&lt;span style=&quot;font-family: Arial, Helvetica, sans-serif; font-size: large;&quot;&gt; said the seismic  swarm was of tectonic origin and the steaming activity was only wispy  to weak.&lt;/span&gt;</content><link rel='replies' type='application/atom+xml' href='http://philippinevolcanoes.blogspot.com/feeds/3642609465037654538/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://philippinevolcanoes.blogspot.com/2011/10/babuyan-claro.html#comment-form' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/3642609465037654538'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5371504585591558867/posts/default/3642609465037654538'/><link rel='alternate' type='text/html' href='http://philippinevolcanoes.blogspot.com/2011/10/babuyan-claro.html' title='BABUYAN CLARO'/><author><name>Unknown</name><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='https://img1.blogblog.com/img/b16-rounded.gif'/></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgDvzGGoSYf_Wn43sDOiiTdjC8uQlIfWfze6v1jB43YGUUGhkkyjtu7VzqkioyHXqieNBA39MCW1EGFxD-xrwheZz3yQxilArzAT0Tdlpntegw8jO78I-jL4dvNfVouiXX7uOTeI8la784/s72-c/Babuyan+Claro.jpg" height="72" width="72"/><thr:total>0</thr:total></entry></feed>