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<?xml-stylesheet type="text/xsl" media="screen" href="/~d/styles/atom10full.xsl"?><?xml-stylesheet type="text/css" media="screen" href="http://feeds.feedburner.com/~d/styles/itemcontent.css"?><feed xmlns="http://www.w3.org/2005/Atom" xmlns:openSearch="http://a9.com/-/spec/opensearch/1.1/" 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" xmlns:feedburner="http://rssnamespace.org/feedburner/ext/1.0" gd:etag="W/&quot;DkEBSHY4fSp7ImA9WhBUF0g.&quot;"><id>tag:blogger.com,1999:blog-609124123307797670</id><updated>2013-05-05T06:50:59.835-05:00</updated><title>MINERALOGY</title><subtitle type="html">MINERALOGY. The most beautiful specimens from all over the world, from pyrite to rubies, a little bit about their name and common location, general narrative about Mineralogy from Mexican Geologist | Mineralogist Oscar Garcia Shelly.&lt;br&gt;&lt;p&gt;&lt;p&gt;
Fluorite crystals on micro-Quartz covered matrix!
from the Octahedron Pocket, From the Denton Mine, Hardin County, Illinois.
Size: 12.7 by 13 by 3.3 cm. 
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There is a new mineral name I discover frequently, so, I am happy to share some of those hereby. Thanks to&amp;nbsp;&lt;a href="http://kristalle.com/premier-minerals.php"&gt;Kristalle&lt;/a&gt;&amp;nbsp;for offering these specimens since 1971&lt;/div&gt;
&lt;br /&gt;&lt;/div&gt;
&lt;img src="http://feeds.feedburner.com/~r/Mineralogy/~4/SwzDyISCj3E" height="1" width="1"/&gt;</content><link rel="replies" type="application/atom+xml" href="http://ogshelly.blogspot.com/feeds/5190636006328054082/comments/default" title="Post Comments" /><link rel="replies" type="text/html" href="http://www.blogger.com/comment.g?blogID=609124123307797670&amp;postID=5190636006328054082" title="3 Comments" /><link rel="edit" type="application/atom+xml" href="http://www.blogger.com/feeds/609124123307797670/posts/default/5190636006328054082?v=2" /><link rel="self" type="application/atom+xml" href="http://www.blogger.com/feeds/609124123307797670/posts/default/5190636006328054082?v=2" /><link rel="alternate" type="text/html" href="http://feedproxy.google.com/~r/Mineralogy/~3/SwzDyISCj3E/rare-minerals-others-not-so-much-all.html" title="Rare minerals, others not so much, all beautiful though!" /><author><name>Oscar Garcia</name><uri>https://plus.google.com/100300946102962552972</uri><email>noreply@blogger.com</email><gd:image rel="http://schemas.google.com/g/2005#thumbnail" width="32" height="32" src="//lh4.googleusercontent.com/-bTyqdIBIO4E/AAAAAAAAAAI/AAAAAAAAAAA/flc2ZUO4-D0/s512-c/photo.jpg" /></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="http://2.bp.blogspot.com/-VXYS4k2UqoA/URaZjCVghNI/AAAAAAAAK1c/MQcIH2ATm_Y/s72-c/CRONSTEDTITE+on+SIDERITE.jpg" height="72" width="72" /><thr:total>3</thr:total><feedburner:origLink>http://ogshelly.blogspot.com/2013/02/rare-minerals-others-not-so-much-all.html</feedburner:origLink></entry><entry gd:etag="W/&quot;CEABRX84eyp7ImA9WhNSE0g.&quot;"><id>tag:blogger.com,1999:blog-609124123307797670.post-4929097978276555387</id><published>2012-10-27T09:10:00.004-05:00</published><updated>2012-10-27T10:45:54.133-05:00</updated><app:edited xmlns:app="http://www.w3.org/2007/app">2012-10-27T10:45:54.133-05:00</app:edited><title>Oranges? no, Cacoxenite, as seen through a microscope 18x</title><content type="html">&lt;div dir="ltr" style="text-align: left;" trbidi="on"&gt;
&lt;div class="separator" style="clear: both; text-align: center;"&gt;
&lt;a href="http://2.bp.blogspot.com/-MxJqBJvuTH8/UIvrUzD3CEI/AAAAAAAAJNc/N8sEFnZovV8/s1600/50F864DF-8574-4E8A-B63E-A48565AABADC.JPG" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"&gt;&lt;img border="0" height="213" src="http://2.bp.blogspot.com/-MxJqBJvuTH8/UIvrUzD3CEI/AAAAAAAAJNc/N8sEFnZovV8/s320/50F864DF-8574-4E8A-B63E-A48565AABADC.JPG" width="320" /&gt;&lt;/a&gt;&lt;/div&gt;
&lt;br /&gt;
&lt;table class="mindatatable"&gt;&lt;tbody&gt;
&lt;tr&gt;&lt;th&gt;Formula:&lt;/th&gt;&lt;td class="m2"&gt;&lt;table class="ft2"&gt;&lt;tbody&gt;
&lt;tr&gt;&lt;td&gt;Fe&lt;/td&gt;&lt;td&gt;&lt;table class="ft2"&gt;&lt;tbody&gt;
&lt;tr&gt;&lt;td class="ftsup2"&gt;3+&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class="ftsub2"&gt;24&lt;/td&gt;&lt;/tr&gt;
&lt;/tbody&gt;&lt;/table&gt;
&lt;/td&gt;&lt;td&gt;Al (PO&lt;/td&gt;&lt;td&gt;&lt;table class="ft2"&gt;&lt;tbody&gt;
&lt;tr&gt;&lt;td class="ftsup2"&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class="ftsub2"&gt;4&lt;/td&gt;&lt;/tr&gt;
&lt;/tbody&gt;&lt;/table&gt;
&lt;/td&gt;&lt;td&gt;)&lt;/td&gt;&lt;td&gt;&lt;table class="ft2"&gt;&lt;tbody&gt;
&lt;tr&gt;&lt;td class="ftsup2"&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class="ftsub2"&gt;17&lt;/td&gt;&lt;/tr&gt;
&lt;/tbody&gt;&lt;/table&gt;
&lt;/td&gt;&lt;td&gt;O&lt;/td&gt;&lt;td&gt;&lt;table class="ft2"&gt;&lt;tbody&gt;
&lt;tr&gt;&lt;td class="ftsup2"&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class="ftsub2"&gt;6&lt;/td&gt;&lt;/tr&gt;
&lt;/tbody&gt;&lt;/table&gt;
&lt;/td&gt;&lt;td&gt;(OH)&lt;/td&gt;&lt;td&gt;&lt;table class="ft2"&gt;&lt;tbody&gt;
&lt;tr&gt;&lt;td class="ftsup2"&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class="ftsub2"&gt;12&lt;/td&gt;&lt;/tr&gt;
&lt;/tbody&gt;&lt;/table&gt;
&lt;/td&gt;&lt;td&gt;· 17H&lt;/td&gt;&lt;td&gt;&lt;table class="ft2"&gt;&lt;tbody&gt;
&lt;tr&gt;&lt;td class="ftsup2"&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class="ftsub2"&gt;2&lt;/td&gt;&lt;/tr&gt;
&lt;/tbody&gt;&lt;/table&gt;
&lt;/td&gt;&lt;td style="text-align: center;"&gt;O&lt;/td&gt;&lt;/tr&gt;
&lt;/tbody&gt;&lt;/table&gt;
&lt;/td&gt;&lt;td class="m2"&gt;&lt;table class="ft2"&gt;&lt;tbody&gt;
&lt;tr&gt;&lt;td style="text-align: center;"&gt;&lt;/td&gt;&lt;td style="text-align: center;"&gt;&lt;/td&gt;&lt;td style="text-align: center;"&gt;&lt;/td&gt;&lt;td style="text-align: center;"&gt;&lt;/td&gt;&lt;td style="text-align: center;"&gt;&lt;/td&gt;&lt;td style="text-align: center;"&gt;&lt;/td&gt;&lt;td style="text-align: center;"&gt;&lt;/td&gt;&lt;td style="text-align: center;"&gt;&lt;/td&gt;&lt;td style="text-align: center;"&gt;&lt;/td&gt;&lt;td style="text-align: center;"&gt;&lt;/td&gt;&lt;td style="text-align: center;"&gt;&lt;/td&gt;&lt;td style="text-align: center;"&gt;&lt;/td&gt;&lt;td style="text-align: center;"&gt;&lt;/td&gt;&lt;td style="text-align: center;"&gt;&lt;/td&gt;&lt;td style="text-align: center;"&gt;&lt;/td&gt;&lt;td style="text-align: center;"&gt;&lt;/td&gt;&lt;td style="text-align: center;"&gt;&lt;/td&gt;&lt;td style="text-align: center;"&gt;&lt;/td&gt;&lt;td style="text-align: center;"&gt;&lt;/td&gt;&lt;td style="text-align: center;"&gt;&lt;/td&gt;&lt;td style="text-align: center;"&gt;&lt;/td&gt;&lt;td style="text-align: center;"&gt;&lt;/td&gt;&lt;td style="text-align: center;"&gt;&lt;/td&gt;&lt;td style="text-align: center;"&gt;&lt;/td&gt;&lt;td style="text-align: center;"&gt;&lt;/td&gt;&lt;td style="text-align: center;"&gt;&lt;/td&gt;&lt;td style="text-align: center;"&gt;&lt;/td&gt;&lt;td style="text-align: center;"&gt;&lt;/td&gt;&lt;td style="text-align: center;"&gt;&lt;/td&gt;&lt;td style="text-align: center;"&gt;&lt;/td&gt;&lt;td style="text-align: center;"&gt;&lt;/td&gt;&lt;td style="text-align: center;"&gt;&lt;/td&gt;&lt;td style="text-align: center;"&gt;&lt;/td&gt;&lt;td style="text-align: center;"&gt;&lt;/td&gt;&lt;td style="text-align: center;"&gt;&lt;/td&gt;&lt;td style="text-align: center;"&gt;&lt;/td&gt;&lt;td style="text-align: center;"&gt;&lt;/td&gt;&lt;td style="text-align: center;"&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/tbody&gt;&lt;/table&gt;
&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;th&gt;&lt;br /&gt;&lt;/th&gt;&lt;td class="m2"&gt;&lt;br /&gt;&lt;/td&gt;&lt;td class="m2"&gt;&lt;/td&gt;&lt;td class="m2"&gt;&lt;/td&gt;&lt;td class="m2"&gt;&lt;/td&gt;&lt;td class="m2"&gt;&lt;/td&gt;&lt;td class="m2"&gt;&lt;/td&gt;&lt;td class="m2"&gt;&lt;/td&gt;&lt;td class="m2"&gt;&lt;/td&gt;&lt;td class="m2"&gt;&lt;/td&gt;&lt;td class="m2"&gt;&lt;/td&gt;&lt;td class="m2"&gt;&lt;/td&gt;&lt;td class="m2"&gt;&lt;/td&gt;&lt;td class="m2"&gt;&lt;/td&gt;&lt;td class="m2"&gt;&lt;/td&gt;&lt;td class="m2"&gt;&lt;/td&gt;&lt;td class="m2"&gt;&lt;/td&gt;&lt;td class="m2"&gt;&lt;/td&gt;&lt;td class="m2"&gt;&lt;/td&gt;&lt;td class="m2"&gt;&lt;/td&gt;&lt;td class="m2"&gt;&lt;/td&gt;&lt;td class="m2"&gt;&lt;/td&gt;&lt;td class="m2"&gt;&lt;/td&gt;&lt;td class="m2"&gt;&lt;/td&gt;&lt;td class="m2"&gt;&lt;/td&gt;&lt;td class="m2"&gt;&lt;/td&gt;&lt;td class="m2"&gt;&lt;/td&gt;&lt;td class="m2"&gt;&lt;/td&gt;&lt;td class="m2"&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;th&gt;&lt;/th&gt;&lt;td class="m2"&gt;&lt;table border="0" cellpadding="0" cellspacing="0" style="width: 504px;"&gt;&lt;colgroup&gt;&lt;col style="mso-width-alt: 4973; mso-width-source: userset; width: 102pt;" width="136"&gt;&lt;/col&gt;
 &lt;col style="mso-width-alt: 13458; mso-width-source: userset; width: 276pt;" width="368"&gt;&lt;/col&gt;
 &lt;/colgroup&gt;&lt;tbody&gt;
&lt;tr height="63" style="height: 47.25pt;"&gt;
  &lt;td class="xl65" height="63" style="height: 47.25pt; width: 102pt;" width="136"&gt;Name:&lt;/td&gt;
  &lt;td class="xl67" style="width: 276pt;" width="368"&gt;From the Greek κακός for
  "bad" and ξένος for "guest" due to the fact that the
  phosphorous content of cacoxenite lessens the quality of iron smelted from
  ore containing it.&lt;/td&gt;
 &lt;/tr&gt;
&lt;tr height="21" style="height: 15.75pt;"&gt;
  &lt;td class="xl65" height="21" style="height: 15.75pt; width: 102pt;" width="136"&gt;System:&lt;/td&gt;
  &lt;td class="xl67" style="width: 276pt;" width="368"&gt;Hexagonal&lt;/td&gt;
 &lt;/tr&gt;
&lt;tr height="21" style="height: 15.75pt;"&gt;
  &lt;td class="xl65" height="21" style="height: 15.75pt; width: 102pt;" width="136"&gt;Colour:&lt;/td&gt;
  &lt;td class="xl67" style="width: 276pt;" width="368"&gt;Yellow to brownish ...&lt;/td&gt;
 &lt;/tr&gt;
&lt;tr height="60" style="height: 45.0pt;"&gt;
  &lt;td class="xl65" height="60" style="height: 45.0pt; width: 102pt;" width="136"&gt;&lt;span style="mso-fareast-font-family: &amp;quot;Times New Roman&amp;quot;;"&gt;Type Locality:&lt;/span&gt;&lt;/td&gt;
  &lt;td class="xl66" style="padding-bottom: .75pt; padding-top: .75pt; width: 276pt;" width="368"&gt;&lt;span style="mso-fareast-font-family: &amp;quot;Times New Roman&amp;quot;;"&gt;&lt;a href="http://www.mindat.org/loc-762.html"&gt;Hrbek Mine, Svatá Dobrotivá (St
  Benigna), Beroun (Beraun), Central Bohemia Region, Bohemia (Böhmen; Boehmen),
  Czech Republic | This particular one from La Paloma, Spain&lt;/a&gt;&lt;/span&gt;&lt;/td&gt;
 &lt;/tr&gt;
&lt;tr height="21" style="height: 15.75pt; mso-yfti-irow: 1;"&gt;
  &lt;td class="xl65" height="21" style="height: 15.75pt; padding-bottom: .75pt; padding-top: .75pt; width: 102pt;" width="136"&gt;&lt;span style="mso-fareast-font-family: &amp;quot;Times New Roman&amp;quot;;"&gt;Year of Discovery:&lt;/span&gt;&lt;/td&gt;
  &lt;td class="xl69" style="padding-bottom: .75pt; padding-top: .75pt; width: 276pt;" width="368"&gt;&lt;span style="mso-fareast-font-family: &amp;quot;Times New Roman&amp;quot;;"&gt;1825&lt;/span&gt;&lt;/td&gt;
 &lt;/tr&gt;
&lt;tr height="63" style="height: 47.25pt; mso-yfti-irow: 3;"&gt;
  &lt;td class="xl65" height="63" style="height: 47.25pt; padding-bottom: .75pt; padding-top: .75pt; width: 102pt;" width="136"&gt;&lt;span style="mso-fareast-font-family: &amp;quot;Times New Roman&amp;quot;;"&gt;Geological Setting:&lt;/span&gt;&lt;/td&gt;
  &lt;td class="xl67" style="padding-bottom: .75pt; padding-top: .75pt; width: 276pt;" width="368"&gt;&lt;span style="mso-fareast-font-family: &amp;quot;Times New Roman&amp;quot;;"&gt;Common
  accessory mineral in oxidation zone of magnetic and limonite iron ores,
  novaculites, rarely in iron rich sediments and soils.&lt;/span&gt;&lt;/td&gt;
 &lt;/tr&gt;
&lt;tr height="21" style="height: 15.75pt; mso-yfti-irow: 5;"&gt;
  &lt;td class="xl65" height="21" style="height: 15.75pt; padding-bottom: .75pt; padding-top: .75pt; width: 102pt;" width="136"&gt;&lt;span style="mso-fareast-font-family: &amp;quot;Times New Roman&amp;quot;;"&gt;Luster:&lt;/span&gt;&lt;/td&gt;
  &lt;td class="xl67" style="padding-bottom: .75pt; padding-top: .75pt; width: 276pt;" width="368"&gt;&lt;span style="mso-fareast-font-family: &amp;quot;Times New Roman&amp;quot;;"&gt;Silky&lt;/span&gt;&lt;/td&gt;
 &lt;/tr&gt;
&lt;tr height="42" style="height: 31.5pt; mso-yfti-irow: 6;"&gt;
  &lt;td class="xl65" height="42" style="height: 31.5pt; padding-bottom: .75pt; padding-top: .75pt; width: 102pt;" width="136"&gt;&lt;span style="mso-fareast-font-family: &amp;quot;Times New Roman&amp;quot;;"&gt;Diaphaneity (Transparency):&lt;/span&gt;&lt;/td&gt;
  &lt;td class="xl67" style="padding-bottom: .75pt; padding-top: .75pt; width: 276pt;" width="368"&gt;&lt;span style="mso-fareast-font-family: &amp;quot;Times New Roman&amp;quot;;"&gt;Translucent&lt;/span&gt;&lt;/td&gt;
 &lt;/tr&gt;
&lt;tr height="42" style="height: 31.5pt; mso-yfti-irow: 7;"&gt;
  &lt;td class="xl65" height="42" style="height: 31.5pt; padding-bottom: .75pt; padding-top: .75pt; width: 102pt;" width="136"&gt;&lt;span style="mso-fareast-font-family: &amp;quot;Times New Roman&amp;quot;;"&gt;Colour:&lt;/span&gt;&lt;/td&gt;
  &lt;td class="xl67" style="padding-bottom: .75pt; padding-top: .75pt; width: 276pt;" width="368"&gt;&lt;span style="mso-fareast-font-family: &amp;quot;Times New Roman&amp;quot;;"&gt;Yellow to
  brownish yellow, reddish orange, golden yellow, deep orange, green; yellow in
  transmitted light&lt;/span&gt;&lt;/td&gt;
 &lt;/tr&gt;
&lt;tr height="21" style="height: 15.75pt; mso-yfti-irow: 8;"&gt;
  &lt;td class="xl65" height="21" style="height: 15.75pt; padding-bottom: .75pt; padding-top: .75pt; width: 102pt;" width="136"&gt;&lt;span style="mso-fareast-font-family: &amp;quot;Times New Roman&amp;quot;;"&gt;Hardness (Mohs):&lt;/span&gt;&lt;/td&gt;
  &lt;td class="xl68" style="padding-bottom: .75pt; padding-top: .75pt; width: 276pt;" width="368"&gt;&lt;span style="mso-fareast-font-family: &amp;quot;Times New Roman&amp;quot;;"&gt;4-Mar&lt;/span&gt;&lt;/td&gt;
 &lt;/tr&gt;
&lt;tr height="25" style="height: 18.75pt; mso-yfti-irow: 9;"&gt;
  &lt;td class="xl65" height="25" style="height: 18.75pt; padding-bottom: .75pt; padding-top: .75pt; width: 102pt;" width="136"&gt;&lt;span style="mso-fareast-font-family: &amp;quot;Times New Roman&amp;quot;;"&gt;Density&lt;span style="mso-spacerun: yes;"&gt;&amp;nbsp;&amp;nbsp;&lt;/span&gt;&lt;/span&gt;&lt;/td&gt;
  &lt;td class="xl67" style="padding-bottom: .75pt; padding-top: .75pt; width: 276pt;" width="368"&gt;&lt;span style="mso-fareast-font-family: &amp;quot;Times New Roman&amp;quot;;"&gt;2.2 - 2.6 g/cm&lt;span class="font6"&gt;&lt;sup&gt;3&lt;/sup&gt;&lt;/span&gt;&lt;/span&gt;&lt;/td&gt;
 &lt;/tr&gt;
&lt;tr height="21" style="height: 15.75pt; mso-yfti-irow: 10;"&gt;
  &lt;td class="xl65" height="21" style="height: 15.75pt; padding-bottom: .75pt; padding-top: .75pt; width: 102pt;" width="136"&gt;&lt;span style="mso-fareast-font-family: &amp;quot;Times New Roman&amp;quot;;"&gt;Crystal System:&lt;/span&gt;&lt;/td&gt;
  &lt;td class="xl67" style="padding-bottom: .75pt; padding-top: .75pt; width: 276pt;" width="368"&gt;&lt;span style="mso-fareast-font-family: &amp;quot;Times New Roman&amp;quot;;"&gt;Hexagonal&lt;/span&gt;&lt;/td&gt;
 &lt;/tr&gt;
&lt;tr height="21" style="height: 15.75pt; mso-yfti-irow: 11;"&gt;
  &lt;td class="xl66" height="21" style="height: 15.75pt; padding-bottom: .75pt; padding-top: .75pt; width: 102pt;" width="136"&gt;&lt;span style="mso-fareast-font-family: &amp;quot;Times New Roman&amp;quot;;"&gt;&lt;a href="http://www.mindat.org/min-840.html" title="Click to Continue &amp;gt; by Text-Enhance"&gt;Class (H-M):&lt;/a&gt;&lt;/span&gt;&lt;/td&gt;
  &lt;td class="xl67" style="padding-bottom: .75pt; padding-top: .75pt; width: 276pt;" width="368"&gt;&lt;span style="mso-fareast-font-family: &amp;quot;Times New Roman&amp;quot;;"&gt;6/&lt;span class="font7"&gt;m&lt;/span&gt;&lt;span class="font5"&gt; - Di-pyramidal&lt;/span&gt;&lt;/span&gt;&lt;/td&gt;
 &lt;/tr&gt;
&lt;tr height="105" style="height: 78.75pt; mso-yfti-irow: 14; mso-yfti-lastrow: yes;"&gt;
  &lt;td class="xl65" height="105" style="height: 78.75pt; padding-bottom: .75pt; padding-top: .75pt; width: 102pt;" width="136"&gt;&lt;span style="mso-fareast-font-family: &amp;quot;Times New Roman&amp;quot;;"&gt;Morphology:&lt;/span&gt;&lt;/td&gt;
  &lt;td class="xl67" style="padding-bottom: .75pt; padding-top: .75pt; width: 276pt;" width="368"&gt;&lt;span style="mso-fareast-font-family: &amp;quot;Times New Roman&amp;quot;;"&gt;Crystals
  crudely hexagonal, acicular [0001], with a hexagonal cross section at times
  and indistinct pyramidal faces. Commonly in compact, concentric, spherical to
  radial aggregates. In bundles, randomly fibrous; as coatings or inter-granular
  cement.&lt;/span&gt;&lt;/td&gt;
 &lt;/tr&gt;
&lt;/tbody&gt;&lt;/table&gt;
&lt;/td&gt;&lt;td class="m2"&gt;&lt;br /&gt;&lt;/td&gt;&lt;td class="m2"&gt;&lt;br /&gt;&lt;/td&gt;&lt;td class="m2"&gt;&lt;!--[if gte mso 9]&gt;&lt;xml&gt;
 &lt;o:OfficeDocumentSettings&gt;
  &lt;o:AllowPNG/&gt;
 &lt;/o:OfficeDocumentSettings&gt;
&lt;/xml&gt;&lt;![endif]--&gt;

&lt;br /&gt;
&lt;table border="0" cellpadding="0" class="MsoNormalTable" style="mso-cellspacing: 1.5pt; mso-yfti-tbllook: 1184;"&gt;
 &lt;tbody&gt;
&lt;tr style="mso-yfti-firstrow: yes; mso-yfti-irow: 0;"&gt;
  &lt;td style="padding: 0.75pt; text-align: justify;"&gt;&lt;br /&gt;&lt;/td&gt;
  &lt;td style="padding: 0.75pt; text-align: justify;"&gt;&lt;br /&gt;&lt;/td&gt;
 &lt;/tr&gt;
&lt;tr style="mso-yfti-irow: 1;"&gt;
  &lt;td style="padding: 0.75pt; text-align: justify;"&gt;&lt;br /&gt;&lt;/td&gt;
  &lt;td style="padding: 0.75pt; text-align: justify;"&gt;&lt;br /&gt;&lt;/td&gt;
 &lt;/tr&gt;
&lt;tr align="justify"&gt;
  &lt;td colspan="2" style="padding: 0.75pt;"&gt;&lt;br /&gt;&lt;/td&gt;
 &lt;/tr&gt;
&lt;tr style="mso-yfti-irow: 3;"&gt;
  &lt;td style="padding: 0.75pt; text-align: justify;"&gt;&lt;br /&gt;&lt;/td&gt;
  &lt;td style="padding: 0.75pt; text-align: justify;"&gt;&lt;br /&gt;&lt;/td&gt;
 &lt;/tr&gt;
&lt;tr align="justify"&gt;
  &lt;td colspan="2" style="padding: 0.75pt;"&gt;&lt;br /&gt;&lt;/td&gt;
 &lt;/tr&gt;
&lt;tr style="mso-yfti-irow: 5;"&gt;
  &lt;td style="padding: 0.75pt; text-align: justify;"&gt;&lt;br /&gt;&lt;/td&gt;
  &lt;td style="padding: 0.75pt; text-align: justify;"&gt;&lt;br /&gt;&lt;/td&gt;
 &lt;/tr&gt;
&lt;tr style="mso-yfti-irow: 6;"&gt;
  &lt;td style="padding: 0.75pt; text-align: justify;"&gt;&lt;br /&gt;&lt;/td&gt;
  &lt;td style="padding: 0.75pt; text-align: justify;"&gt;&lt;br /&gt;&lt;/td&gt;
 &lt;/tr&gt;
&lt;tr style="mso-yfti-irow: 7;"&gt;
  &lt;td style="padding: 0.75pt; text-align: justify;"&gt;&lt;br /&gt;&lt;/td&gt;
  &lt;td style="padding: 0.75pt; text-align: justify;"&gt;&lt;br /&gt;&lt;/td&gt;
 &lt;/tr&gt;
&lt;tr style="mso-yfti-irow: 8;"&gt;
  &lt;td style="padding: 0.75pt; text-align: justify;"&gt;&lt;br /&gt;&lt;/td&gt;
  &lt;td style="padding: 0.75pt; text-align: justify;"&gt;&lt;br /&gt;&lt;/td&gt;
 &lt;/tr&gt;
&lt;tr style="mso-yfti-irow: 9;"&gt;
  &lt;td style="padding: 0.75pt; text-align: justify;"&gt;&lt;br /&gt;&lt;/td&gt;
  &lt;td style="padding: 0.75pt; text-align: justify;"&gt;&lt;br /&gt;&lt;/td&gt;
 &lt;/tr&gt;
&lt;tr style="mso-yfti-irow: 10;"&gt;
  &lt;td style="padding: 0.75pt; text-align: justify;"&gt;&lt;br /&gt;&lt;/td&gt;
  &lt;td style="padding: 0.75pt; text-align: justify;"&gt;&lt;br /&gt;&lt;/td&gt;
 &lt;/tr&gt;
&lt;tr style="mso-yfti-irow: 11;"&gt;
  &lt;td style="padding: 0.75pt; text-align: justify;"&gt;&lt;br /&gt;&lt;/td&gt;
  &lt;td style="padding: 0.75pt; text-align: justify;"&gt;&lt;br /&gt;&lt;/td&gt;
 &lt;/tr&gt;
&lt;tr style="mso-yfti-irow: 12;"&gt;
  &lt;td style="padding: 0.75pt; text-align: justify;"&gt;&lt;br /&gt;&lt;/td&gt;
  &lt;td style="padding: 0.75pt; text-align: justify;"&gt;&lt;br /&gt;&lt;/td&gt;
 &lt;/tr&gt;
&lt;tr style="mso-yfti-irow: 13;"&gt;
  &lt;td style="padding: 0.75pt; text-align: justify;"&gt;&lt;br /&gt;&lt;/td&gt;
  &lt;td style="padding: 0.75pt; text-align: justify;"&gt;&lt;br /&gt;&lt;/td&gt;
 &lt;/tr&gt;
&lt;tr style="mso-yfti-irow: 14; mso-yfti-lastrow: yes;"&gt;
  &lt;td style="padding: 0.75pt; text-align: justify;"&gt;&lt;br /&gt;&lt;/td&gt;
  &lt;td style="padding: 0.75pt; text-align: justify;"&gt;&lt;br /&gt;&lt;/td&gt;
 &lt;/tr&gt;
&lt;/tbody&gt;&lt;/table&gt;
&lt;!--[if gte mso 9]&gt;&lt;xml&gt;
 &lt;w:WordDocument&gt;
  &lt;w:View&gt;Normal&lt;/w:View&gt;
  &lt;w:Zoom&gt;0&lt;/w:Zoom&gt;
  &lt;w:TrackMoves/&gt;
  &lt;w:TrackFormatting/&gt;
  &lt;w:PunctuationKerning/&gt;
  &lt;w:ValidateAgainstSchemas/&gt;
  &lt;w:SaveIfXMLInvalid&gt;false&lt;/w:SaveIfXMLInvalid&gt;
  &lt;w:IgnoreMixedContent&gt;false&lt;/w:IgnoreMixedContent&gt;
  &lt;w:AlwaysShowPlaceholderText&gt;false&lt;/w:AlwaysShowPlaceholderText&gt;
  &lt;w:DoNotPromoteQF/&gt;
  &lt;w:LidThemeOther&gt;EN-US&lt;/w:LidThemeOther&gt;
  &lt;w:LidThemeAsian&gt;X-NONE&lt;/w:LidThemeAsian&gt;
  &lt;w:LidThemeComplexScript&gt;X-NONE&lt;/w:LidThemeComplexScript&gt;
  &lt;w:Compatibility&gt;
   &lt;w:BreakWrappedTables/&gt;
   &lt;w:SnapToGridInCell/&gt;
   &lt;w:WrapTextWithPunct/&gt;
   &lt;w:UseAsianBreakRules/&gt;
   &lt;w:DontGrowAutofit/&gt;
   &lt;w:SplitPgBreakAndParaMark/&gt;
   &lt;w:EnableOpenTypeKerning/&gt;
   &lt;w:DontFlipMirrorIndents/&gt;
   &lt;w:OverrideTableStyleHps/&gt;
  &lt;/w:Compatibility&gt;
  &lt;m:mathPr&gt;
   &lt;m:mathFont m:val="Cambria Math"/&gt;
   &lt;m:brkBin m:val="before"/&gt;
   &lt;m:brkBinSub m:val="&amp;#45;-"/&gt;
   &lt;m:smallFrac m:val="off"/&gt;
   &lt;m:dispDef/&gt;
   &lt;m:lMargin m:val="0"/&gt;
   &lt;m:rMargin m:val="0"/&gt;
   &lt;m:defJc m:val="centerGroup"/&gt;
   &lt;m:wrapIndent m:val="1440"/&gt;
   &lt;m:intLim m:val="subSup"/&gt;
   &lt;m:naryLim m:val="undOvr"/&gt;
  &lt;/m:mathPr&gt;&lt;/w:WordDocument&gt;
&lt;/xml&gt;&lt;![endif]--&gt;&lt;!--[if gte mso 9]&gt;&lt;xml&gt;
 &lt;w:LatentStyles DefLockedState="false" DefUnhideWhenUsed="true"
  DefSemiHidden="true" DefQFormat="false" DefPriority="99"
  LatentStyleCount="267"&gt;
  &lt;w:LsdException Locked="false" Priority="0" SemiHidden="false"
   UnhideWhenUsed="false" QFormat="true" Name="Normal"/&gt;
  &lt;w:LsdException Locked="false" Priority="9" SemiHidden="false"
   UnhideWhenUsed="false" QFormat="true" Name="heading 1"/&gt;
  &lt;w:LsdException Locked="false" Priority="9" QFormat="true" Name="heading 2"/&gt;
  &lt;w:LsdException Locked="false" Priority="9" QFormat="true" Name="heading 3"/&gt;
  &lt;w:LsdException Locked="false" Priority="9" QFormat="true" Name="heading 4"/&gt;
  &lt;w:LsdException Locked="false" Priority="9" QFormat="true" Name="heading 5"/&gt;
  &lt;w:LsdException Locked="false" Priority="9" QFormat="true" Name="heading 6"/&gt;
  &lt;w:LsdException Locked="false" Priority="9" QFormat="true" Name="heading 7"/&gt;
  &lt;w:LsdException Locked="false" Priority="9" QFormat="true" Name="heading 8"/&gt;
  &lt;w:LsdException Locked="false" Priority="9" QFormat="true" Name="heading 9"/&gt;
  &lt;w:LsdException Locked="false" Priority="39" Name="toc 1"/&gt;
  &lt;w:LsdException Locked="false" Priority="39" Name="toc 2"/&gt;
  &lt;w:LsdException Locked="false" Priority="39" Name="toc 3"/&gt;
  &lt;w:LsdException Locked="false" Priority="39" Name="toc 4"/&gt;
  &lt;w:LsdException Locked="false" Priority="39" Name="toc 5"/&gt;
  &lt;w:LsdException Locked="false" Priority="39" Name="toc 6"/&gt;
  &lt;w:LsdException Locked="false" Priority="39" Name="toc 7"/&gt;
  &lt;w:LsdException Locked="false" Priority="39" Name="toc 8"/&gt;
  &lt;w:LsdException Locked="false" Priority="39" Name="toc 9"/&gt;
  &lt;w:LsdException Locked="false" Priority="35" QFormat="true" Name="caption"/&gt;
  &lt;w:LsdException Locked="false" Priority="10" SemiHidden="false"
   UnhideWhenUsed="false" QFormat="true" Name="Title"/&gt;
  &lt;w:LsdException Locked="false" Priority="1" Name="Default Paragraph Font"/&gt;
  &lt;w:LsdException Locked="false" Priority="11" SemiHidden="false"
   UnhideWhenUsed="false" QFormat="true" Name="Subtitle"/&gt;
  &lt;w:LsdException Locked="false" Priority="22" SemiHidden="false"
   UnhideWhenUsed="false" QFormat="true" Name="Strong"/&gt;
  &lt;w:LsdException Locked="false" Priority="20" SemiHidden="false"
   UnhideWhenUsed="false" QFormat="true" Name="Emphasis"/&gt;
  &lt;w:LsdException Locked="false" Priority="59" SemiHidden="false"
   UnhideWhenUsed="false" Name="Table Grid"/&gt;
  &lt;w:LsdException Locked="false" UnhideWhenUsed="false" Name="Placeholder Text"/&gt;
  &lt;w:LsdException Locked="false" Priority="1" SemiHidden="false"
   UnhideWhenUsed="false" QFormat="true" Name="No Spacing"/&gt;
  &lt;w:LsdException Locked="false" Priority="60" SemiHidden="false"
   UnhideWhenUsed="false" Name="Light Shading"/&gt;
  &lt;w:LsdException Locked="false" Priority="61" SemiHidden="false"
   UnhideWhenUsed="false" Name="Light List"/&gt;
  &lt;w:LsdException Locked="false" Priority="62" SemiHidden="false"
   UnhideWhenUsed="false" Name="Light Grid"/&gt;
  &lt;w:LsdException Locked="false" Priority="63" SemiHidden="false"
   UnhideWhenUsed="false" Name="Medium Shading 1"/&gt;
  &lt;w:LsdException Locked="false" Priority="64" SemiHidden="false"
   UnhideWhenUsed="false" Name="Medium Shading 2"/&gt;
  &lt;w:LsdException Locked="false" Priority="65" SemiHidden="false"
   UnhideWhenUsed="false" Name="Medium List 1"/&gt;
  &lt;w:LsdException Locked="false" Priority="66" SemiHidden="false"
   UnhideWhenUsed="false" Name="Medium List 2"/&gt;
  &lt;w:LsdException Locked="false" Priority="67" SemiHidden="false"
   UnhideWhenUsed="false" Name="Medium Grid 1"/&gt;
  &lt;w:LsdException Locked="false" Priority="68" SemiHidden="false"
   UnhideWhenUsed="false" Name="Medium Grid 2"/&gt;
  &lt;w:LsdException Locked="false" Priority="69" SemiHidden="false"
   UnhideWhenUsed="false" Name="Medium Grid 3"/&gt;
  &lt;w:LsdException Locked="false" Priority="70" SemiHidden="false"
   UnhideWhenUsed="false" Name="Dark List"/&gt;
  &lt;w:LsdException Locked="false" Priority="71" SemiHidden="false"
   UnhideWhenUsed="false" Name="Colorful Shading"/&gt;
  &lt;w:LsdException Locked="false" Priority="72" SemiHidden="false"
   UnhideWhenUsed="false" Name="Colorful List"/&gt;
  &lt;w:LsdException Locked="false" Priority="73" SemiHidden="false"
   UnhideWhenUsed="false" Name="Colorful Grid"/&gt;
  &lt;w:LsdException Locked="false" Priority="60" SemiHidden="false"
   UnhideWhenUsed="false" Name="Light Shading Accent 1"/&gt;
  &lt;w:LsdException Locked="false" Priority="61" SemiHidden="false"
   UnhideWhenUsed="false" Name="Light List Accent 1"/&gt;
  &lt;w:LsdException Locked="false" Priority="62" SemiHidden="false"
   UnhideWhenUsed="false" Name="Light Grid Accent 1"/&gt;
  &lt;w:LsdException Locked="false" Priority="63" SemiHidden="false"
   UnhideWhenUsed="false" Name="Medium Shading 1 Accent 1"/&gt;
  &lt;w:LsdException Locked="false" Priority="64" SemiHidden="false"
   UnhideWhenUsed="false" Name="Medium Shading 2 Accent 1"/&gt;
  &lt;w:LsdException Locked="false" Priority="65" SemiHidden="false"
   UnhideWhenUsed="false" Name="Medium List 1 Accent 1"/&gt;
  &lt;w:LsdException Locked="false" UnhideWhenUsed="false" Name="Revision"/&gt;
  &lt;w:LsdException Locked="false" Priority="34" SemiHidden="false"
   UnhideWhenUsed="false" QFormat="true" Name="List Paragraph"/&gt;
  &lt;w:LsdException Locked="false" Priority="29" SemiHidden="false"
   UnhideWhenUsed="false" QFormat="true" Name="Quote"/&gt;
  &lt;w:LsdException Locked="false" Priority="30" SemiHidden="false"
   UnhideWhenUsed="false" QFormat="true" Name="Intense Quote"/&gt;
  &lt;w:LsdException Locked="false" Priority="66" SemiHidden="false"
   UnhideWhenUsed="false" Name="Medium List 2 Accent 1"/&gt;
  &lt;w:LsdException Locked="false" Priority="67" SemiHidden="false"
   UnhideWhenUsed="false" Name="Medium Grid 1 Accent 1"/&gt;
  &lt;w:LsdException Locked="false" Priority="68" SemiHidden="false"
   UnhideWhenUsed="false" Name="Medium Grid 2 Accent 1"/&gt;
  &lt;w:LsdException Locked="false" Priority="69" SemiHidden="false"
   UnhideWhenUsed="false" Name="Medium Grid 3 Accent 1"/&gt;
  &lt;w:LsdException Locked="false" Priority="70" SemiHidden="false"
   UnhideWhenUsed="false" Name="Dark List Accent 1"/&gt;
  &lt;w:LsdException Locked="false" Priority="71" SemiHidden="false"
   UnhideWhenUsed="false" Name="Colorful Shading Accent 1"/&gt;
  &lt;w:LsdException Locked="false" Priority="72" SemiHidden="false"
   UnhideWhenUsed="false" Name="Colorful List Accent 1"/&gt;
  &lt;w:LsdException Locked="false" Priority="73" SemiHidden="false"
   UnhideWhenUsed="false" Name="Colorful Grid Accent 1"/&gt;
  &lt;w:LsdException Locked="false" Priority="60" SemiHidden="false"
   UnhideWhenUsed="false" Name="Light Shading Accent 2"/&gt;
  &lt;w:LsdException Locked="false" Priority="61" SemiHidden="false"
   UnhideWhenUsed="false" Name="Light List Accent 2"/&gt;
  &lt;w:LsdException Locked="false" Priority="62" SemiHidden="false"
   UnhideWhenUsed="false" Name="Light Grid Accent 2"/&gt;
  &lt;w:LsdException Locked="false" Priority="63" SemiHidden="false"
   UnhideWhenUsed="false" Name="Medium Shading 1 Accent 2"/&gt;
  &lt;w:LsdException Locked="false" Priority="64" SemiHidden="false"
   UnhideWhenUsed="false" Name="Medium Shading 2 Accent 2"/&gt;
  &lt;w:LsdException Locked="false" Priority="65" SemiHidden="false"
   UnhideWhenUsed="false" Name="Medium List 1 Accent 2"/&gt;
  &lt;w:LsdException Locked="false" Priority="66" SemiHidden="false"
   UnhideWhenUsed="false" Name="Medium List 2 Accent 2"/&gt;
  &lt;w:LsdException Locked="false" Priority="67" SemiHidden="false"
   UnhideWhenUsed="false" Name="Medium Grid 1 Accent 2"/&gt;
  &lt;w:LsdException Locked="false" Priority="68" SemiHidden="false"
   UnhideWhenUsed="false" Name="Medium Grid 2 Accent 2"/&gt;
  &lt;w:LsdException Locked="false" Priority="69" SemiHidden="false"
   UnhideWhenUsed="false" Name="Medium Grid 3 Accent 2"/&gt;
  &lt;w:LsdException Locked="false" Priority="70" SemiHidden="false"
   UnhideWhenUsed="false" Name="Dark List Accent 2"/&gt;
  &lt;w:LsdException Locked="false" Priority="71" SemiHidden="false"
   UnhideWhenUsed="false" Name="Colorful Shading Accent 2"/&gt;
  &lt;w:LsdException Locked="false" Priority="72" SemiHidden="false"
   UnhideWhenUsed="false" Name="Colorful List Accent 2"/&gt;
  &lt;w:LsdException Locked="false" Priority="73" SemiHidden="false"
   UnhideWhenUsed="false" Name="Colorful Grid Accent 2"/&gt;
  &lt;w:LsdException Locked="false" Priority="60" SemiHidden="false"
   UnhideWhenUsed="false" Name="Light Shading Accent 3"/&gt;
  &lt;w:LsdException Locked="false" Priority="61" SemiHidden="false"
   UnhideWhenUsed="false" Name="Light List Accent 3"/&gt;
  &lt;w:LsdException Locked="false" Priority="62" SemiHidden="false"
   UnhideWhenUsed="false" Name="Light Grid Accent 3"/&gt;
  &lt;w:LsdException Locked="false" Priority="63" SemiHidden="false"
   UnhideWhenUsed="false" Name="Medium Shading 1 Accent 3"/&gt;
  &lt;w:LsdException Locked="false" Priority="64" SemiHidden="false"
   UnhideWhenUsed="false" Name="Medium Shading 2 Accent 3"/&gt;
  &lt;w:LsdException Locked="false" Priority="65" SemiHidden="false"
   UnhideWhenUsed="false" Name="Medium List 1 Accent 3"/&gt;
  &lt;w:LsdException Locked="false" Priority="66" SemiHidden="false"
   UnhideWhenUsed="false" Name="Medium List 2 Accent 3"/&gt;
  &lt;w:LsdException Locked="false" Priority="67" SemiHidden="false"
   UnhideWhenUsed="false" Name="Medium Grid 1 Accent 3"/&gt;
  &lt;w:LsdException Locked="false" Priority="68" SemiHidden="false"
   UnhideWhenUsed="false" Name="Medium Grid 2 Accent 3"/&gt;
  &lt;w:LsdException Locked="false" Priority="69" SemiHidden="false"
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&lt;img src="http://feeds.feedburner.com/~r/Mineralogy/~4/8c9P3Ty8nzI" height="1" width="1"/&gt;</content><link rel="replies" type="application/atom+xml" href="http://ogshelly.blogspot.com/feeds/4929097978276555387/comments/default" title="Post Comments" /><link rel="replies" type="text/html" href="http://www.blogger.com/comment.g?blogID=609124123307797670&amp;postID=4929097978276555387" title="0 Comments" /><link rel="edit" type="application/atom+xml" href="http://www.blogger.com/feeds/609124123307797670/posts/default/4929097978276555387?v=2" /><link rel="self" type="application/atom+xml" href="http://www.blogger.com/feeds/609124123307797670/posts/default/4929097978276555387?v=2" /><link rel="alternate" type="text/html" href="http://feedproxy.google.com/~r/Mineralogy/~3/8c9P3Ty8nzI/blog-post.html" title="Oranges? no, Cacoxenite, as seen through a microscope 18x" /><author><name>Oscar Garcia</name><uri>https://plus.google.com/100300946102962552972</uri><email>noreply@blogger.com</email><gd:image rel="http://schemas.google.com/g/2005#thumbnail" width="32" height="32" src="//lh4.googleusercontent.com/-bTyqdIBIO4E/AAAAAAAAAAI/AAAAAAAAAAA/flc2ZUO4-D0/s512-c/photo.jpg" /></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="http://2.bp.blogspot.com/-MxJqBJvuTH8/UIvrUzD3CEI/AAAAAAAAJNc/N8sEFnZovV8/s72-c/50F864DF-8574-4E8A-B63E-A48565AABADC.JPG" height="72" width="72" /><thr:total>0</thr:total><feedburner:origLink>http://ogshelly.blogspot.com/2012/10/blog-post.html</feedburner:origLink></entry><entry gd:etag="W/&quot;DEAGQ3w4eCp7ImA9WhVXGUk.&quot;"><id>tag:blogger.com,1999:blog-609124123307797670.post-1809497647390265723</id><published>2012-04-20T13:32:00.001-05:00</published><updated>2012-04-20T13:32:02.230-05:00</updated><app:edited xmlns:app="http://www.w3.org/2007/app">2012-04-20T13:32:02.230-05:00</app:edited><title /><content type="html">&lt;div dir="ltr" style="text-align: left;" trbidi="on"&gt;
&lt;br /&gt;
&lt;h2 class="entry-title" style="background-attachment: initial; background-clip: initial; background-color: #fdfdfd; background-image: initial; background-origin: initial; border-bottom-width: 0px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: #545658; font-family: 'Helvetica Neue', Helvetica, Arial, sans-serif; font-size: 20px; line-height: 28px; margin-bottom: 16px; margin-left: 0px; margin-right: 0px; margin-top: 0px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; text-align: -webkit-auto; vertical-align: baseline;"&gt;
&lt;a href="http://www.onlinecollegeclasses.com/volcanic-and-geological-resources.html"&gt;Volcanic and Geological Resources&lt;/a&gt;&lt;/h2&gt;
&lt;div class="entry-content" style="background-attachment: initial; background-clip: initial; background-color: #fdfdfd; background-image: initial; background-origin: initial; border-bottom-width: 0px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; margin-bottom: 15px; margin-left: 0px; margin-right: 0px; margin-top: 0px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; text-align: -webkit-auto; vertical-align: baseline;"&gt;
&lt;div style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-width: 0px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: #545658; font-family: 'Helvetica Neue', Helvetica, Arial, sans-serif; font-size: 12px; line-height: 20px; margin-bottom: 20px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; vertical-align: baseline;"&gt;
&lt;img alt="" class="size-medium wp-image-883 alignleft" height="300" src="http://www.onlinecollegeclasses.com/wp-content/uploads/2012/02/volcano-201x300.jpg" style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-width: 0px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; float: left; margin-bottom: 20px; margin-left: 0px; margin-right: 25px; margin-top: 10px; max-width: 600px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; vertical-align: baseline;" title="volcano" width="201" /&gt;&lt;/div&gt;
&lt;div style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-width: 0px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: #545658; font-family: 'Helvetica Neue', Helvetica, Arial, sans-serif; font-size: 12px; line-height: 20px; margin-bottom: 20px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; vertical-align: baseline;"&gt;
&lt;br /&gt;&lt;/div&gt;
&lt;div style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-width: 0px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: #545658; font-family: 'Helvetica Neue', Helvetica, Arial, sans-serif; font-size: 12px; line-height: 20px; margin-bottom: 20px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; vertical-align: baseline;"&gt;
There are over 500 documented volcanos on Earth. Just about every culture has some reference to these fantastic natural events; in fact, the word “volcano” comes from Vulcan, the Roman God of Fire and Metalworking (&lt;a href="http://jersey.uoregon.edu/~mstrick/geology/Geo_Lectures/Volcanoes.html" style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-color: rgb(221, 223, 226); border-bottom-style: solid; border-bottom-width: 1px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: #a1a3a6; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; text-decoration: none; vertical-align: baseline;"&gt;Volcanoes&lt;/a&gt;). As society progressed, people began to understand volcanoes as more than just gateways to hell and internal suffering, and instead recognize them as the result of tectonic plate boundaries and shifting.&lt;/div&gt;
&lt;div style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-width: 0px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: #545658; font-family: 'Helvetica Neue', Helvetica, Arial, sans-serif; font-size: 12px; line-height: 20px; margin-bottom: 20px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; vertical-align: baseline;"&gt;
Below you’ll find a collection of resources centered around volcanoes and geology from around our world and the planets closest to us. Many of these resources are products of geology departments at various different universities, and feature a wide range of information in addition to the resources listed. Image courtesy of Wikimedia Commons.&lt;/div&gt;
&lt;div style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-width: 0px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: #545658; font-family: 'Helvetica Neue', Helvetica, Arial, sans-serif; font-size: 12px; line-height: 20px; margin-bottom: 20px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; vertical-align: baseline;"&gt;
&lt;br /&gt;&lt;/div&gt;
&lt;div style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-width: 0px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: #545658; font-family: 'Helvetica Neue', Helvetica, Arial, sans-serif; font-size: 12px; line-height: 20px; margin-bottom: 20px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; vertical-align: baseline;"&gt;
&lt;a href="http://volcano.oregonstate.edu/education/glossary.html" style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-color: rgb(221, 223, 226); border-bottom-style: solid; border-bottom-width: 1px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: #a1a3a6; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; text-decoration: none; vertical-align: baseline;"&gt;Glossary of Volcanic and Geologic Terms&lt;/a&gt;&amp;nbsp;– The most extensive glossary on the web. Presented by Oregon State University, this list covers all the basic terms and all the un-basic terms as well.&lt;/div&gt;
&lt;div style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-width: 0px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: #545658; font-family: 'Helvetica Neue', Helvetica, Arial, sans-serif; font-size: 12px; line-height: 20px; margin-bottom: 20px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; vertical-align: baseline;"&gt;
&lt;a href="http://www.geology.sdsu.edu/how_volcanoes_work/" style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-color: rgb(221, 223, 226); border-bottom-style: solid; border-bottom-width: 1px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: #a1a3a6; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; text-decoration: none; vertical-align: baseline;"&gt;How Volcanos Work&lt;/a&gt;&amp;nbsp;– If you need a refresher course, this website is a comprehensive educational resource that describes the science behind both&amp;nbsp;&lt;em style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-width: 0px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; vertical-align: baseline;"&gt;volcanoes&lt;/em&gt;&lt;em style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-width: 0px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; vertical-align: baseline;"&gt;&amp;nbsp;&lt;/em&gt;and the&amp;nbsp;&lt;em style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-width: 0px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; vertical-align: baseline;"&gt;volcanic&lt;/em&gt;&amp;nbsp;processes.&lt;/div&gt;
&lt;div style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-width: 0px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: #545658; font-family: 'Helvetica Neue', Helvetica, Arial, sans-serif; font-size: 12px; line-height: 20px; margin-bottom: 20px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; vertical-align: baseline;"&gt;
&lt;a href="http://hvo.wr.usgs.gov/" style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-color: rgb(221, 223, 226); border-bottom-style: solid; border-bottom-width: 1px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: #a1a3a6; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; text-decoration: none; vertical-align: baseline;"&gt;Hawaiian Volcano Observatory&lt;/a&gt;&amp;nbsp;– From the United States Geological Survey, this site takes an in-depth look at the many volcanos and earthquakes on the Hawaiian islands, including fantastic images and extensive fact sheets.&lt;/div&gt;
&lt;div style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-width: 0px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: #545658; font-family: 'Helvetica Neue', Helvetica, Arial, sans-serif; font-size: 12px; line-height: 20px; margin-bottom: 20px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; vertical-align: baseline;"&gt;
&lt;a href="http://www.discover-the-world.co.uk/en/special-interest/volcano-geology-guide.html" style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-color: rgb(221, 223, 226); border-bottom-style: solid; border-bottom-width: 1px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: #a1a3a6; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; text-decoration: none; vertical-align: baseline;"&gt;Volcanic Activity in Iceland&lt;/a&gt;&amp;nbsp;– A comprehensive overview of the volcanos in Iceland, including a gallery of images and a video of the Fimmvörđuháls volcano erupting in Southern Iceland.&lt;/div&gt;
&lt;div style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-width: 0px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: #545658; font-family: 'Helvetica Neue', Helvetica, Arial, sans-serif; font-size: 12px; line-height: 20px; margin-bottom: 20px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; vertical-align: baseline;"&gt;
&lt;a href="http://www.uwgb.edu/dutchs/EarthSC202Slides/volcslid.htm" style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-color: rgb(221, 223, 226); border-bottom-style: solid; border-bottom-width: 1px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: #a1a3a6; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; text-decoration: none; vertical-align: baseline;"&gt;Physical Geology Slides-Volcanoes&lt;/a&gt;&amp;nbsp;– A great collection of images, categorized by type with descriptions. Includes cinder cones, stratovolcanoes, calderas, and images of Vesuvius and Pompeii.&lt;/div&gt;
&lt;div style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-width: 0px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: #545658; font-family: 'Helvetica Neue', Helvetica, Arial, sans-serif; font-size: 12px; line-height: 20px; margin-bottom: 20px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; vertical-align: baseline;"&gt;
&lt;a href="http://www.colby.edu/geology/V&amp;amp;e.html" style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-color: rgb(221, 223, 226); border-bottom-style: solid; border-bottom-width: 1px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: #a1a3a6; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; text-decoration: none; vertical-align: baseline;"&gt;Volcano and Earthquake Resources on the World Wide Web&lt;/a&gt;&amp;nbsp;– Though an older site, this page from Colby College contains live links to some fantastic volcano and geographic links from around the net, including observatory homepages and earthquake information in the U.S. by region.&lt;/div&gt;
&lt;div style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-width: 0px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: #545658; font-family: 'Helvetica Neue', Helvetica, Arial, sans-serif; font-size: 12px; line-height: 20px; margin-bottom: 20px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; vertical-align: baseline;"&gt;
&lt;a href="http://www.virtual-geology.info/" style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-color: rgb(221, 223, 226); border-bottom-style: solid; border-bottom-width: 1px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: #a1a3a6; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; text-decoration: none; vertical-align: baseline;"&gt;Virtual Geology&lt;/a&gt;&amp;nbsp;– This site features virtual field trips, regional geology, as well as some truly incredible images of geology and scenery from around the world.&lt;/div&gt;
&lt;div style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-width: 0px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: #545658; font-family: 'Helvetica Neue', Helvetica, Arial, sans-serif; font-size: 12px; line-height: 20px; margin-bottom: 20px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; vertical-align: baseline;"&gt;
&lt;a href="http://www.geol.umd.edu/facilities/lmdr/dante/dante.htm" style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-color: rgb(221, 223, 226); border-bottom-style: solid; border-bottom-width: 1px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: #a1a3a6; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; text-decoration: none; vertical-align: baseline;"&gt;A Geological Guidebook to Dante’s Peak&lt;/a&gt;&amp;nbsp;– A humorous rendition of the movie Dante’s Peak as told by a geologist horrified by the inaccuracies of the film who feels the need to set the record straight about volcanos.&lt;/div&gt;
&lt;div style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-width: 0px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: #545658; font-family: 'Helvetica Neue', Helvetica, Arial, sans-serif; font-size: 12px; line-height: 20px; margin-bottom: 20px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; vertical-align: baseline;"&gt;
&lt;a href="http://volcano.oregonstate.edu/oldroot/volcanoes/planet_volcano/venus/intro.html" style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-color: rgb(221, 223, 226); border-bottom-style: solid; border-bottom-width: 1px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: #a1a3a6; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; text-decoration: none; vertical-align: baseline;"&gt;Volcanoes on Venus&lt;/a&gt;&amp;nbsp;– From Oregon State University, this webpage features an overview of volcanoes on Venus, as well as images of Venus’ large shield volcanoes, lava flow features, and some remarkably unusual volcanoes as well.&lt;/div&gt;
&lt;div style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-width: 0px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: #545658; font-family: 'Helvetica Neue', Helvetica, Arial, sans-serif; font-size: 12px; line-height: 20px; margin-bottom: 20px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; vertical-align: baseline;"&gt;
&lt;a href="http://marine.rutgers.edu/main/Exciting-Science/Exciting-Science-Life-at-the-Extremes-Microbiology-of-deep-sea-volcanoes.html" style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-color: rgb(221, 223, 226); border-bottom-style: solid; border-bottom-width: 1px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: #a1a3a6; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; text-decoration: none; vertical-align: baseline;"&gt;Exciting Science: Life at the Extremes – Microbiology of deep-sea volcanoes&lt;/a&gt;&amp;nbsp;– Rutgers University presents a fascinating look at the life that consists in water as hot as 400°C, extremely high pressures, and surrounded by high concentrations of hydrogen sulfide.&lt;/div&gt;
&lt;div style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-width: 0px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: #545658; font-family: 'Helvetica Neue', Helvetica, Arial, sans-serif; font-size: 12px; line-height: 20px; margin-bottom: 20px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; vertical-align: baseline;"&gt;
&lt;a href="http://volcano.oregonstate.edu/book/export/html/138" style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-color: rgb(221, 223, 226); border-bottom-style: solid; border-bottom-width: 1px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: #a1a3a6; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; text-decoration: none; vertical-align: baseline;"&gt;Submarine Volcanoes&lt;/a&gt;&amp;nbsp;– This article contains a thorough explanation of submarine volcanoes’ plate tectonic settings, submarine eruptions, evidence of features and deposits, and is supplemented by several images.&lt;/div&gt;
&lt;div style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-width: 0px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: #545658; font-family: 'Helvetica Neue', Helvetica, Arial, sans-serif; font-size: 12px; line-height: 20px; margin-bottom: 20px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; vertical-align: baseline;"&gt;
&lt;a href="http://www.lukew.com/marsgeo/volcanic.html" style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-color: rgb(221, 223, 226); border-bottom-style: solid; border-bottom-width: 1px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: #a1a3a6; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; text-decoration: none; vertical-align: baseline;"&gt;Geology of Mars&lt;/a&gt;&amp;nbsp;– This site has information and images of many global features on the planet of Mars, including volcanoes, craters, landslides, tectonic plates, and wind mechanics.&lt;/div&gt;
&lt;div style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-width: 0px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: #545658; font-family: 'Helvetica Neue', Helvetica, Arial, sans-serif; font-size: 12px; line-height: 20px; margin-bottom: 20px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; vertical-align: baseline;"&gt;
&lt;a href="http://faculty.gg.uwyo.edu/heller/SedMovs/SandVolc.htm" style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-color: rgb(221, 223, 226); border-bottom-style: solid; border-bottom-width: 1px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: #a1a3a6; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; text-decoration: none; vertical-align: baseline;"&gt;Video of Sand Volcano (injectite) Erupting&lt;/a&gt;&amp;nbsp;– This video, taken in Saudi Arabia, shows an injectite volcano exploding right next to a busy street.&lt;/div&gt;
&lt;div style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-width: 0px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: #545658; font-family: 'Helvetica Neue', Helvetica, Arial, sans-serif; font-size: 12px; line-height: 20px; margin-bottom: 20px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; vertical-align: baseline;"&gt;
&lt;a href="http://www.geo.mtu.edu/volcanoes/" style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-color: rgb(221, 223, 226); border-bottom-style: solid; border-bottom-width: 1px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: #a1a3a6; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; text-decoration: none; vertical-align: baseline;"&gt;Michigan Technological University Volcanoes Page&lt;/a&gt;&amp;nbsp;– This site, sponsored by the Keweenaw Volcano Observatory, includes an extensive variety of links to all things related to volcanos, including a section of volcano jokes and recipes for cooking with lava.&lt;/div&gt;
&lt;div style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-width: 0px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: #545658; font-family: 'Helvetica Neue', Helvetica, Arial, sans-serif; font-size: 12px; line-height: 20px; margin-bottom: 20px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; vertical-align: baseline;"&gt;
&lt;a href="http://volcanology.geol.ucsb.edu/" style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-color: rgb(221, 223, 226); border-bottom-style: solid; border-bottom-width: 1px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: #a1a3a6; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; text-decoration: none; vertical-align: baseline;"&gt;The Volcano Information Center&lt;/a&gt;&amp;nbsp;– From the University of California at Santa Barbara, this site “provides links to websites that are resources for data and to inform the user about general volcanology, including features of volcanoes, volcanic eruptions and volcanic hazards.”&lt;/div&gt;
&lt;div style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-width: 0px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: #545658; font-family: 'Helvetica Neue', Helvetica, Arial, sans-serif; font-size: 12px; line-height: 20px; margin-bottom: 20px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; vertical-align: baseline;"&gt;
&lt;a href="http://www.smate.wwu.edu/teched/geology/vo-HA-forms.html" style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-color: rgb(221, 223, 226); border-bottom-style: solid; border-bottom-width: 1px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: #a1a3a6; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; text-decoration: none; vertical-align: baseline;"&gt;Hawaii Volcanism: Lava Forms&lt;/a&gt;&amp;nbsp;– This page includes a brief but thorough explanation of different types and behaviors of lava and includes several pictures of lava from the Hawaii volcanoes.&lt;/div&gt;
&lt;div style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-width: 0px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: #545658; font-family: 'Helvetica Neue', Helvetica, Arial, sans-serif; font-size: 12px; line-height: 20px; margin-bottom: 20px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; vertical-align: baseline;"&gt;
&lt;a href="http://www.volcano.si.edu/world/region.cfm?rnum=12&amp;amp;rpage=list" style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-color: rgb(221, 223, 226); border-bottom-style: solid; border-bottom-width: 1px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: #a1a3a6; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; text-decoration: none; vertical-align: baseline;"&gt;Volcanoes of Canada and the western USA&lt;/a&gt;&amp;nbsp;– Each region of Canada and western United States features a map of where the volcanoes are, as well as a complete list of the documented volcanoes, their type, and activity status.&lt;/div&gt;
&lt;div style="background-attachment: initial; background-clip: initial; background-color: transparent; background-image: initial; background-origin: initial; border-bottom-width: 0px; border-color: initial; border-image: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; margin-bottom: 20px; outline-color: initial; outline-style: initial; outline-width: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; vertical-align: baseline;"&gt;
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&lt;/div&gt;
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&lt;a href="http://4.bp.blogspot.com/-sz7jpI0uLxA/TmJTh9Q8_gI/AAAAAAAAFtc/5x60-TiH3ec/s1600/Tucson2011-101TopazKatlungPakistan62mm.jpg" imageanchor="1" style="margin-left:1em; margin-right:1em"&gt;&lt;img border="0" height="269" width="320" src="http://4.bp.blogspot.com/-sz7jpI0uLxA/TmJTh9Q8_gI/AAAAAAAAFtc/5x60-TiH3ec/s320/Tucson2011-101TopazKatlungPakistan62mm.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;

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From top to bottom:&lt;br&gt;

Topaz in Calcite matrix - From Katlang, Mardan District, Northwest Frontier Province, Pakistan.
Scheelite set with Quartz on matrix - From the Gharmung Area, Skardu District, Baltistan, Northern Areas of Pakistan.&lt;br&gt;
Fluorite with blades of white Barite - From Berbes, Berbes Mining Area, Ribadesella, Asturias, Spain.&lt;br&gt;
Acanthite and curling Native Silver wires - From the Reyes Mine in Guanajuato, Mexico.&lt;br&gt;
Pyrrhotites on Quartz crystals - From the Nikolaevskiy Mine, Dal'negorsk, Primorskiy Kray, Russia.&lt;br&gt;
Native Copper - From the Calumet &amp; Hecla Mine, Calumet, Houghton County, Michigan.&lt;br&gt;
Botryoidal Chalcedony and fine Millerite crystals - From Halls Gap, Lincoln County, Kentucky.&lt;br&gt;
Red Beryl crystals in and atop Rhyolite matrix - From the Wah Wah Mountains near Delta, Utah.&lt;br&gt;
Boleite with Calcite on hand matrix - From Boleo, Baja California, Mexico.&lt;br&gt;















&lt;img src="http://feeds.feedburner.com/~r/Mineralogy/~4/0c77TVQBAsM" height="1" width="1"/&gt;</content><link rel="replies" type="application/atom+xml" href="http://ogshelly.blogspot.com/feeds/4573845097291241106/comments/default" title="Post Comments" /><link rel="replies" type="text/html" href="http://www.blogger.com/comment.g?blogID=609124123307797670&amp;postID=4573845097291241106" title="0 Comments" /><link rel="edit" type="application/atom+xml" href="http://www.blogger.com/feeds/609124123307797670/posts/default/4573845097291241106?v=2" /><link rel="self" type="application/atom+xml" href="http://www.blogger.com/feeds/609124123307797670/posts/default/4573845097291241106?v=2" /><link rel="alternate" type="text/html" href="http://feedproxy.google.com/~r/Mineralogy/~3/0c77TVQBAsM/fluorite-pyrrhotite-native-silver.html" title="Topaz, Scheelite, Fluorite, Pyrrhotite, Copper, Silver, Millerite from Spain to Pakistan, Russia, Mexico and Michigan! to take your breath away!" /><author><name>Oscar Garcia</name><uri>https://plus.google.com/100300946102962552972</uri><email>noreply@blogger.com</email><gd:image rel="http://schemas.google.com/g/2005#thumbnail" width="32" height="32" src="//lh4.googleusercontent.com/-bTyqdIBIO4E/AAAAAAAAAAI/AAAAAAAAAAA/flc2ZUO4-D0/s512-c/photo.jpg" /></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="http://4.bp.blogspot.com/-sz7jpI0uLxA/TmJTh9Q8_gI/AAAAAAAAFtc/5x60-TiH3ec/s72-c/Tucson2011-101TopazKatlungPakistan62mm.jpg" height="72" width="72" /><thr:total>0</thr:total><feedburner:origLink>http://ogshelly.blogspot.com/2011/09/fluorite-pyrrhotite-native-silver.html</feedburner:origLink></entry><entry gd:etag="W/&quot;A04BQXg9fip7ImA9WhZaFEU.&quot;"><id>tag:blogger.com,1999:blog-609124123307797670.post-1309736986729935859</id><published>2011-06-30T22:01:00.008-05:00</published><updated>2011-06-30T22:12:30.666-05:00</updated><app:edited xmlns:app="http://www.w3.org/2007/app">2011-06-30T22:12:30.666-05:00</app:edited><title>Bloody minerals shouldn't be a bad word in UK, some as this red!</title><content type="html">&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://4.bp.blogspot.com/-0WcVhISAT8A/Tg07GsWKqtI/AAAAAAAAFF8/VIKjcIe8i8s/s1600/Denver2010-137GoldMalachiteMashambaWestZaire62mm.jpg"&gt;&lt;img style="display:block; 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margin:0px auto 10px; text-align:center;cursor:pointer; cursor:hand;width: 277px; height: 320px;" src="http://4.bp.blogspot.com/-_F9ZBkSVYsA/Tg05rmY6tpI/AAAAAAAAFFE/CXXAk2mincI/s320/Tucson2010-217GoldMockingbirdMineCalifornia.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5624214930857834130" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://2.bp.blogspot.com/-L1WZ6I4O_mY/Tg05AFZ6zvI/AAAAAAAAFE8/C5BMnNLH5yU/s1600/Tucson2010-151PyrargyriteStAndreasbergGermanyCLOSE.jpg"&gt;&lt;img style="display:block; margin:0px auto 10px; text-align:center;cursor:pointer; cursor:hand;width: 320px; height: 212px;" src="http://2.bp.blogspot.com/-L1WZ6I4O_mY/Tg05AFZ6zvI/AAAAAAAAFE8/C5BMnNLH5yU/s320/Tucson2010-151PyrargyriteStAndreasbergGermanyCLOSE.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5624214183269289714" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://3.bp.blogspot.com/-j8ghiAXs4Ec/Tg048PXjhGI/AAAAAAAAFE0/RaWqih6mkaw/s1600/Tucson2010-133WulfeniteLosLamentosMexico.jpg"&gt;&lt;img style="display:block; margin:0px auto 10px; text-align:center;cursor:pointer; cursor:hand;width: 320px; height: 233px;" src="http://3.bp.blogspot.com/-j8ghiAXs4Ec/Tg048PXjhGI/AAAAAAAAFE0/RaWqih6mkaw/s320/Tucson2010-133WulfeniteLosLamentosMexico.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5624214117224252514" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://3.bp.blogspot.com/-oQImu4XD6mA/Tg043z-8IkI/AAAAAAAAFEs/TwFgY_Mx8vw/s1600/Tucson2010-132FluoriteSchorl-NagarPakistan.jpg"&gt;&lt;img style="display:block; margin:0px auto 10px; text-align:center;cursor:pointer; cursor:hand;width: 309px; height: 320px;" src="http://3.bp.blogspot.com/-oQImu4XD6mA/Tg043z-8IkI/AAAAAAAAFEs/TwFgY_Mx8vw/s320/Tucson2010-132FluoriteSchorl-NagarPakistan.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5624214041153774146" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://3.bp.blogspot.com/-qSJl_qikw2E/Tg04zKDzxHI/AAAAAAAAFEk/tveouXiCnzU/s1600/Tucson2010-128BariteCalciteSouthDakota.jpg"&gt;&lt;img style="display:block; margin:0px auto 10px; text-align:center;cursor:pointer; cursor:hand;width: 294px; height: 320px;" src="http://3.bp.blogspot.com/-qSJl_qikw2E/Tg04zKDzxHI/AAAAAAAAFEk/tveouXiCnzU/s320/Tucson2010-128BariteCalciteSouthDakota.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5624213961180431474" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://2.bp.blogspot.com/-PRhkZ3l7YVc/Tg04t6-HadI/AAAAAAAAFEc/Eirck5KWCtM/s1600/Tucson2009-9erythrite.jpg"&gt;&lt;img style="display:block; margin:0px auto 10px; text-align:center;cursor:pointer; cursor:hand;width: 271px; height: 320px;" src="http://2.bp.blogspot.com/-PRhkZ3l7YVc/Tg04t6-HadI/AAAAAAAAFEc/Eirck5KWCtM/s320/Tucson2009-9erythrite.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5624213871230675410" /&gt;&lt;/a&gt;&lt;img src="http://feeds.feedburner.com/~r/Mineralogy/~4/9hZIUYE4Xr0" height="1" width="1"/&gt;</content><link rel="replies" type="application/atom+xml" href="http://ogshelly.blogspot.com/feeds/1309736986729935859/comments/default" title="Post Comments" /><link rel="replies" type="text/html" href="http://www.blogger.com/comment.g?blogID=609124123307797670&amp;postID=1309736986729935859" title="3 Comments" /><link rel="edit" type="application/atom+xml" href="http://www.blogger.com/feeds/609124123307797670/posts/default/1309736986729935859?v=2" /><link rel="self" type="application/atom+xml" href="http://www.blogger.com/feeds/609124123307797670/posts/default/1309736986729935859?v=2" /><link rel="alternate" type="text/html" href="http://feedproxy.google.com/~r/Mineralogy/~3/9hZIUYE4Xr0/bloody-minerals-shouldnt-be-bad-word-in.html" title="Bloody minerals shouldn't be a bad word in UK, some as this red!" /><author><name>Oscar Garcia</name><uri>https://plus.google.com/100300946102962552972</uri><email>noreply@blogger.com</email><gd:image rel="http://schemas.google.com/g/2005#thumbnail" width="32" height="32" src="//lh4.googleusercontent.com/-bTyqdIBIO4E/AAAAAAAAAAI/AAAAAAAAAAA/flc2ZUO4-D0/s512-c/photo.jpg" /></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="http://4.bp.blogspot.com/-0WcVhISAT8A/Tg07GsWKqtI/AAAAAAAAFF8/VIKjcIe8i8s/s72-c/Denver2010-137GoldMalachiteMashambaWestZaire62mm.jpg" height="72" width="72" /><thr:total>3</thr:total><feedburner:origLink>http://ogshelly.blogspot.com/2011/06/bloody-minerals-shouldnt-be-bad-word-in.html</feedburner:origLink></entry><entry gd:etag="W/&quot;DkMARXo6eyp7ImA9WhZUEkk.&quot;"><id>tag:blogger.com,1999:blog-609124123307797670.post-9055476352258830809</id><published>2011-06-04T21:15:00.018-05:00</published><updated>2011-06-04T22:27:24.413-05:00</updated><app:edited xmlns:app="http://www.w3.org/2007/app">2011-06-04T22:27:24.413-05:00</app:edited><title>Legrandite and Adamite from the famous Ojuela Mine in Mapimi, Durango Mexico, and of quartz... many more</title><content type="html">&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://2.bp.blogspot.com/-xTSzPsu5HUU/TernAvXrR1I/AAAAAAAAE2w/Va0qvHloqmY/s1600/Denver2010-77LegranditeOjuelaMineMexico29mm.jpg"&gt;&lt;img style="display:block; margin:0px auto 10px; text-align:center;cursor:pointer; cursor:hand;width: 258px; height: 320px;" src="http://2.bp.blogspot.com/-xTSzPsu5HUU/TernAvXrR1I/AAAAAAAAE2w/Va0qvHloqmY/s320/Denver2010-77LegranditeOjuelaMineMexico29mm.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5614553885372532562" /&gt;&lt;/a&gt;&lt;br&gt;&lt;br /&gt;Monoclinic prismatic Legrandite crystals with Limonite matrix From the Ojuela Mine in Mapimi, Durango, Mexico - Zn2(AsO4)(OH)•(H2O) - Named after the Belgian mining engineer, Legrande.&lt;br /&gt;&lt;br&gt;&lt;br /&gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://1.bp.blogspot.com/-uh5jemQdBG0/Ter2ouiOThI/AAAAAAAAE3A/2gR9FLDaGGc/s1600/Tucson2010-225RhodochrositeHedgehogSweetHomeMineColorado.jpg"&gt;&lt;img style="display:block; margin:0px auto 10px; text-align:center;cursor:pointer; cursor:hand;width: 302px; height: 320px;" src="http://1.bp.blogspot.com/-uh5jemQdBG0/Ter2ouiOThI/AAAAAAAAE3A/2gR9FLDaGGc/s320/Tucson2010-225RhodochrositeHedgehogSweetHomeMineColorado.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5614571065017519634" /&gt;&lt;/a&gt;&lt;br&gt;&lt;br /&gt;Trigonal hexagonal scalenohedral Rhodochrosite in cluster on Quartz crystals from the Hedgehog Pocket, Main Stope Drift, Sweet Home Mine, Alma, Colorado - MnCO3 - From the Greek rhodon -"rose" and chroma - "color."&lt;br&gt;&lt;br /&gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://3.bp.blogspot.com/-XZu3FGCo-TU/TernEK_qOII/AAAAAAAAE24/qWMkMuFHEJU/s1600/Denver2010-131AUCTIONBerylAquamarineSchorlErongoMtsNamibia65mm.jpg"&gt;&lt;img style="display:block; margin:0px auto 10px; text-align:center;cursor:pointer; cursor:hand;width: 320px; height: 298px;" src="http://3.bp.blogspot.com/-XZu3FGCo-TU/TernEK_qOII/AAAAAAAAE24/qWMkMuFHEJU/s320/Denver2010-131AUCTIONBerylAquamarineSchorlErongoMtsNamibia65mm.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5614553944327600258" /&gt;&lt;/a&gt;&lt;br&gt;&lt;br /&gt;Hexagonal dihexagonal dipyramidal Beryl var. Aquamarine crystal with tourmaline Schorl rom the Erongo Mine, Namibia, SW Africa - Be3Al2Si6O18 - From the ancient Greek, beryllos, signifying a "precious blue-green color of sea water" stone.&lt;br&gt;&lt;br /&gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://1.bp.blogspot.com/-8dQy7ppbaUw/Term9GbAiUI/AAAAAAAAE2o/se8pJC2QCQQ/s1600/Denver2009-540BariteEngland.jpg"&gt;&lt;img style="display:block; margin:0px auto 10px; text-align:center;cursor:pointer; cursor:hand;width: 225px; height: 320px;" src="http://1.bp.blogspot.com/-8dQy7ppbaUw/Term9GbAiUI/AAAAAAAAE2o/se8pJC2QCQQ/s320/Denver2009-540BariteEngland.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5614553822841047362" /&gt;&lt;/a&gt;&lt;br&gt;&lt;br /&gt;Orthorhombic dipyramidal Barite crystal on reddish Hematite &amp; Dolomite covered matrix from Frizington, West Cumberland Iron Field, North and Western Region (Cumberland), Cumbria, England - BaSO4 - From the Greek, baryos, "heavy."&lt;BR&gt;&lt;br /&gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://2.bp.blogspot.com/-9hhB07ss8ts/Term6Gm9gBI/AAAAAAAAE2g/yGuxonPnDAg/s1600/DEN2007-14acanthitecal.jpg"&gt;&lt;img style="display:block; margin:0px auto 10px; text-align:center;cursor:pointer; cursor:hand;width: 320px; height: 190px;" src="http://2.bp.blogspot.com/-9hhB07ss8ts/Term6Gm9gBI/AAAAAAAAE2g/yGuxonPnDAg/s320/DEN2007-14acanthitecal.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5614553771351572498" /&gt;&lt;/a&gt;&lt;br&gt;&lt;br /&gt;Trigonal ditrigonal pyramidal Pyrargyrite crystals on top of Calcite rhombs from the Samson Mine, St. Andreasberg, Harz, Germany - Ag3SbS3 - From the Samson Mine, St. Andreasberg, Harz, Germany. From the Greek, pyr and argyros, "fire-silver" in allusion to color and silver content.&lt;br&gt;&lt;br /&gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://3.bp.blogspot.com/-diHvoOv-9G4/Term2mnk9hI/AAAAAAAAE2Y/jmfP2jtJHaY/s1600/Tucson2010-70PeridotForsteriteMagnetitePakistan.jpg"&gt;&lt;img style="display:block; margin:0px auto 10px; text-align:center;cursor:pointer; cursor:hand;width: 250px; height: 320px;" src="http://3.bp.blogspot.com/-diHvoOv-9G4/Term2mnk9hI/AAAAAAAAE2Y/jmfP2jtJHaY/s320/Tucson2010-70PeridotForsteriteMagnetitePakistan.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5614553711224616466" /&gt;&lt;/a&gt;&lt;br&gt;&lt;br /&gt;Orthorhombic dipyramidal Forsterite var. Peridot on Magnetite from Sapat Gali, Naran-Kagan Valley, Kohistan District, North-West Frontier Province, Pakistan - Mg2(SiO4) - &lt;br /&gt;Named for Johann Forster, German naturalist. &lt;br&gt;&lt;br /&gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://4.bp.blogspot.com/-RKirmHsgPwU/TermzFtXB4I/AAAAAAAAE2Q/4bpkh-It0os/s1600/Tucson2010-18AdamiteOjuelaMineMexico.jpg"&gt;&lt;img style="display:block; margin:0px auto 10px; text-align:center;cursor:pointer; cursor:hand;width: 320px; height: 254px;" src="http://4.bp.blogspot.com/-RKirmHsgPwU/TermzFtXB4I/AAAAAAAAE2Q/4bpkh-It0os/s320/Tucson2010-18AdamiteOjuelaMineMexico.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5614553650850891650" /&gt;&lt;/a&gt;&lt;br&gt;&lt;br /&gt;&lt;br /&gt;Orthorhombic dipyramidal Adamite clusters on Limonite from the Ojuela Mine, Mapimí, Durango, Mexico - Zn2(AsO4)(OH) - Named after the French mineralogist Gilbert Joseph Adam (1795-1881).&lt;br&gt;&lt;br /&gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://3.bp.blogspot.com/-1-GibsZutYA/TermvmpAsDI/AAAAAAAAE2I/gBXFvmgmQ64/s1600/TUC2007-101erongo.jpg"&gt;&lt;img style="display:block; margin:0px auto 10px; text-align:center;cursor:pointer; cursor:hand;width: 248px; height: 320px;" src="http://3.bp.blogspot.com/-1-GibsZutYA/TermvmpAsDI/AAAAAAAAE2I/gBXFvmgmQ64/s320/TUC2007-101erongo.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5614553590971543602" /&gt;&lt;/a&gt;&lt;img src="http://feeds.feedburner.com/~r/Mineralogy/~4/RQhlxIo3Yno" height="1" width="1"/&gt;</content><link rel="replies" type="application/atom+xml" href="http://ogshelly.blogspot.com/feeds/9055476352258830809/comments/default" title="Post Comments" /><link rel="replies" type="text/html" href="http://www.blogger.com/comment.g?blogID=609124123307797670&amp;postID=9055476352258830809" title="0 Comments" /><link rel="edit" type="application/atom+xml" href="http://www.blogger.com/feeds/609124123307797670/posts/default/9055476352258830809?v=2" /><link rel="self" type="application/atom+xml" href="http://www.blogger.com/feeds/609124123307797670/posts/default/9055476352258830809?v=2" /><link rel="alternate" type="text/html" href="http://feedproxy.google.com/~r/Mineralogy/~3/RQhlxIo3Yno/legrandite-rom-famous-ojuela-mine-in.html" title="Legrandite and Adamite from the famous Ojuela Mine in Mapimi, Durango Mexico, and of quartz... many more" /><author><name>Oscar Garcia</name><uri>https://plus.google.com/100300946102962552972</uri><email>noreply@blogger.com</email><gd:image rel="http://schemas.google.com/g/2005#thumbnail" width="32" height="32" src="//lh4.googleusercontent.com/-bTyqdIBIO4E/AAAAAAAAAAI/AAAAAAAAAAA/flc2ZUO4-D0/s512-c/photo.jpg" /></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="http://2.bp.blogspot.com/-xTSzPsu5HUU/TernAvXrR1I/AAAAAAAAE2w/Va0qvHloqmY/s72-c/Denver2010-77LegranditeOjuelaMineMexico29mm.jpg" height="72" width="72" /><thr:total>0</thr:total><feedburner:origLink>http://ogshelly.blogspot.com/2011/06/legrandite-rom-famous-ojuela-mine-in.html</feedburner:origLink></entry><entry gd:etag="W/&quot;DUUMSXg_eSp7ImA9WhZWGEk.&quot;"><id>tag:blogger.com,1999:blog-609124123307797670.post-5556823626275324965</id><published>2011-05-19T18:06:00.008-05:00</published><updated>2011-05-19T18:21:28.641-05:00</updated><app:edited xmlns:app="http://www.w3.org/2007/app">2011-05-19T18:21:28.641-05:00</app:edited><title>Rhodochrosite, Calcite, Scheelite, Spessartine, Pyrrhotite, Millerite, and more all together in one post!</title><content type="html">&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://3.bp.blogspot.com/-CWGqBy5N-2M/TdWlvkZtL1I/AAAAAAAAEu8/anfIdSm2tG0/s1600/Tucson2011-182RhodochrositeSHMColorado33mm.jpg"&gt;&lt;img style="display:block; margin:0px auto 10px; text-align:center;cursor:pointer; cursor:hand;width: 280px; height: 320px;" src="http://3.bp.blogspot.com/-CWGqBy5N-2M/TdWlvkZtL1I/AAAAAAAAEu8/anfIdSm2tG0/s320/Tucson2011-182RhodochrositeSHMColorado33mm.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5608571147603750738" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://4.bp.blogspot.com/-av00nXFvCyc/TdWlMD-wbJI/AAAAAAAAEu0/1OfS5UW4Dfk/s1600/Denver2010-239CVCalciteSphaleriteDentonMineIllinois81mm.jpg"&gt;&lt;img style="display:block; margin:0px auto 10px; text-align:center;cursor:pointer; cursor:hand;width: 254px; height: 320px;" src="http://4.bp.blogspot.com/-av00nXFvCyc/TdWlMD-wbJI/AAAAAAAAEu0/1OfS5UW4Dfk/s320/Denver2010-239CVCalciteSphaleriteDentonMineIllinois81mm.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5608570537605360786" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://2.bp.blogspot.com/--Ex0MQvBtBU/TdWi3bUBmrI/AAAAAAAAEus/fJNI5v9ZNYE/s1600/Denver2010-224ScheeliteMtXuebaodingChina72mm.jpg"&gt;&lt;img style="display:block; margin:0px auto 10px; text-align:center;cursor:pointer; cursor:hand;width: 280px; height: 320px;" src="http://2.bp.blogspot.com/--Ex0MQvBtBU/TdWi3bUBmrI/AAAAAAAAEus/fJNI5v9ZNYE/s320/Denver2010-224ScheeliteMtXuebaodingChina72mm.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5608567984068074162" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://4.bp.blogspot.com/-BOosbGbAOAc/TdWi0QZXP1I/AAAAAAAAEuk/IyfSb0ovCMo/s1600/Denver2010-114GarnetHematiteChina125mm.jpg"&gt;&lt;img style="display:block; margin:0px auto 10px; text-align:center;cursor:pointer; cursor:hand;width: 320px; height: 310px;" src="http://4.bp.blogspot.com/-BOosbGbAOAc/TdWi0QZXP1I/AAAAAAAAEuk/IyfSb0ovCMo/s320/Denver2010-114GarnetHematiteChina125mm.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5608567929598066514" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://2.bp.blogspot.com/-RoBbaZzL4x8/TdWiwwr7rcI/AAAAAAAAEuc/o9yxIt1nfNM/s1600/Denver2010-51PyrrhotiteNikolaiMineRussia127mm.jpg"&gt;&lt;img style="display:block; margin:0px auto 10px; text-align:center;cursor:pointer; cursor:hand;width: 320px; height: 232px;" src="http://2.bp.blogspot.com/-RoBbaZzL4x8/TdWiwwr7rcI/AAAAAAAAEuc/o9yxIt1nfNM/s320/Denver2010-51PyrrhotiteNikolaiMineRussia127mm.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5608567869546409410" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://2.bp.blogspot.com/-fLbAAew7uTw/TdWitQWtW3I/AAAAAAAAEuU/vLSpGus4KN8/s1600/Tucson2010-312MilleriteGeode.jpg"&gt;&lt;img style="display:block; margin:0px auto 10px; text-align:center;cursor:pointer; cursor:hand;width: 320px; height: 221px;" src="http://2.bp.blogspot.com/-fLbAAew7uTw/TdWitQWtW3I/AAAAAAAAEuU/vLSpGus4KN8/s320/Tucson2010-312MilleriteGeode.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5608567809327848306" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://2.bp.blogspot.com/-RL8XDwMFlCE/TdWiqaZd4wI/AAAAAAAAEuM/qR_vwMfEfn4/s1600/Tucson2010-300PyrargyriteCalciteZacatecasMexico.jpg"&gt;&lt;img style="display:block; margin:0px auto 10px; text-align:center;cursor:pointer; cursor:hand;width: 320px; height: 271px;" src="http://2.bp.blogspot.com/-RL8XDwMFlCE/TdWiqaZd4wI/AAAAAAAAEuM/qR_vwMfEfn4/s320/Tucson2010-300PyrargyriteCalciteZacatecasMexico.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5608567760484164354" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://2.bp.blogspot.com/-tftxiK8Nq6g/TdWimg18YQI/AAAAAAAAEuE/y6qbQII3-7E/s1600/Denver2009-538BariteSeleniteCalciteElkCreekSouthDakota2.jpg"&gt;&lt;img style="display:block; margin:0px auto 10px; text-align:center;cursor:pointer; cursor:hand;width: 320px; height: 200px;" src="http://2.bp.blogspot.com/-tftxiK8Nq6g/TdWimg18YQI/AAAAAAAAEuE/y6qbQII3-7E/s320/Denver2009-538BariteSeleniteCalciteElkCreekSouthDakota2.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5608567693494739202" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;In order of appearance from the top down: &lt;br /&gt;&lt;br /&gt;Rhombs of Rhodochrosite atop Tetrahedrite and Quartz matrix! From the Sweet Home Mine, Alma, Park County, Colorado.&lt;br /&gt;Measures 3.1 cm by 3 cm by 3.5 cm in total size.&lt;br /&gt;&lt;br /&gt;Twinned Golden Calcite with Sphalerite on matrix! From the Denton Mine, Harris Creek District, Hardin County, Illinois.&lt;br /&gt;Measures 7 cm by 7.2 cm by 5.2 cm in total size.&lt;br /&gt;&lt;br /&gt;Scheelite crystal with glassy Adularia! From Mt Xuebaoding, Pingwu Co., Mianyang Prefecture, Sichuan Province of China. Measures 7.3 cm by 5.5 cm by 4.4 cm in total size.&lt;br /&gt;&lt;br /&gt;Spessartine Garnet with dark botryoidal Goethite! From Tongbei, Yunxiao Co., Zhangzhou Prefecture, Fujian Province, China.&lt;br /&gt;Measures 12.5 cm by 10.2 cm in size.&lt;br /&gt;&lt;br /&gt;Large pyramidal Pyrrhotites on Quartz crystals! From the Nikolaevskiy Mine, Dal'negorsk, Primorskiy Kray, Russia.&lt;br /&gt;Measures 7 cm by 12.6 cm by 10 cm in total size.&lt;br /&gt;&lt;br /&gt;Cavern of botryoidal Chalcedony and fine Millerite crystals! From Halls Gap, Lincoln County, Kentucky.&lt;br /&gt;Measures 7.2 cm by 11 cm by 6.8 cm in size.&lt;br /&gt;&lt;br /&gt;Lustrous crystals of Pyrargyrite nestled between brown Calcite crystals and casts!From Level 630 of the San Guillermo Vein, San Luis Shaft, Fresnillo, Zacatecas, Mexico.&lt;br /&gt;Measures 3 cm by 4.5 cm in size.&lt;br /&gt;&lt;br /&gt;Combination of Barite and Gypsum crystals on Yellow Calcite! From the Elk Creek locality, Dalzell, Meade County, South Dakota.&lt;br /&gt;Measures 7.5 cm by 15.3 cm by 12.5 cm in size.&lt;br /&gt;&lt;br /&gt;Simply Amazing!&lt;img src="http://feeds.feedburner.com/~r/Mineralogy/~4/2r9II4kV8Rs" height="1" width="1"/&gt;</content><link rel="replies" type="application/atom+xml" href="http://ogshelly.blogspot.com/feeds/5556823626275324965/comments/default" title="Post Comments" /><link rel="replies" type="text/html" href="http://www.blogger.com/comment.g?blogID=609124123307797670&amp;postID=5556823626275324965" title="0 Comments" /><link rel="edit" type="application/atom+xml" href="http://www.blogger.com/feeds/609124123307797670/posts/default/5556823626275324965?v=2" /><link rel="self" type="application/atom+xml" href="http://www.blogger.com/feeds/609124123307797670/posts/default/5556823626275324965?v=2" /><link rel="alternate" type="text/html" href="http://feedproxy.google.com/~r/Mineralogy/~3/2r9II4kV8Rs/blog-post.html" title="Rhodochrosite, Calcite, Scheelite, Spessartine, Pyrrhotite, Millerite, and more all together in one post!" /><author><name>Oscar Garcia</name><uri>https://plus.google.com/100300946102962552972</uri><email>noreply@blogger.com</email><gd:image rel="http://schemas.google.com/g/2005#thumbnail" width="32" height="32" src="//lh4.googleusercontent.com/-bTyqdIBIO4E/AAAAAAAAAAI/AAAAAAAAAAA/flc2ZUO4-D0/s512-c/photo.jpg" /></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="http://3.bp.blogspot.com/-CWGqBy5N-2M/TdWlvkZtL1I/AAAAAAAAEu8/anfIdSm2tG0/s72-c/Tucson2011-182RhodochrositeSHMColorado33mm.jpg" height="72" width="72" /><thr:total>0</thr:total><feedburner:origLink>http://ogshelly.blogspot.com/2011/05/blog-post.html</feedburner:origLink></entry><entry gd:etag="W/&quot;DEABSX06eSp7ImA9WhZWE0Q.&quot;"><id>tag:blogger.com,1999:blog-609124123307797670.post-2809983440797372717</id><published>2011-05-14T12:36:00.012-05:00</published><updated>2011-05-14T13:12:38.311-05:00</updated><app:edited xmlns:app="http://www.w3.org/2007/app">2011-05-14T13:12:38.311-05:00</app:edited><title>If you want to buy beautiful minerals, bring lots of money!</title><content type="html">&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://1.bp.blogspot.com/-65NlkNqklDk/Tc7DuOCY7HI/AAAAAAAAEo8/KOImVA0rqyg/s1600/Tucson2010-28RhodochrositeAmericanTunnelMineColorado.jpg"&gt;&lt;img style="display:block; margin:0px auto 10px; text-align:center;cursor:pointer; cursor:hand;width: 310px; height: 320px;" src="http://1.bp.blogspot.com/-65NlkNqklDk/Tc7DuOCY7HI/AAAAAAAAEo8/KOImVA0rqyg/s320/Tucson2010-28RhodochrositeAmericanTunnelMineColorado.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5606633784932363378" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://4.bp.blogspot.com/-9NnqWJRHxHw/Tc7DpFHrG1I/AAAAAAAAEo0/bUm9-ZX1KtI/s1600/Tucson2010-29TripleBerylEmeraldLaPitaMineColombia2.jpg"&gt;&lt;img style="display:block; margin:0px auto 10px; text-align:center;cursor:pointer; cursor:hand;width: 320px; height: 190px;" src="http://4.bp.blogspot.com/-9NnqWJRHxHw/Tc7DpFHrG1I/AAAAAAAAEo0/bUm9-ZX1KtI/s320/Tucson2010-29TripleBerylEmeraldLaPitaMineColombia2.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5606633696639261522" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://1.bp.blogspot.com/-7wegulA8jv4/Tc6_hZFDBNI/AAAAAAAAEok/yVQb3U7Gbpg/s1600/Denver2010-144closeup%2Bsilver.jpg"&gt;&lt;img style="display:block; margin:0px auto 10px; text-align:center;cursor:pointer; cursor:hand;width: 320px; height: 282px;" src="http://1.bp.blogspot.com/-7wegulA8jv4/Tc6_hZFDBNI/AAAAAAAAEok/yVQb3U7Gbpg/s320/Denver2010-144closeup%2Bsilver.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5606629166511490258" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://3.bp.blogspot.com/-4iXeUMzJF6I/Tc6--oDYD7I/AAAAAAAAEoc/izUsRpuotGE/s1600/Tucson2011-55SpodumemeKunziteAfghanistan95mm.jpg"&gt;&lt;img style="display:block; margin:0px auto 10px; text-align:center;cursor:pointer; cursor:hand;width: 263px; height: 320px;" src="http://3.bp.blogspot.com/-4iXeUMzJF6I/Tc6--oDYD7I/AAAAAAAAEoc/izUsRpuotGE/s320/Tucson2011-55SpodumemeKunziteAfghanistan95mm.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5606628569235591090" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://1.bp.blogspot.com/-vIAROJjISvc/Tc6-7p7aI_I/AAAAAAAAEoU/yHrI2u3YJck/s1600/Tucson2011-39SpanishFluoriteBarite15cm.jpg"&gt;&lt;img style="display:block; margin:0px auto 10px; text-align:center;cursor:pointer; cursor:hand;width: 320px; height: 305px;" src="http://1.bp.blogspot.com/-vIAROJjISvc/Tc6-7p7aI_I/AAAAAAAAEoU/yHrI2u3YJck/s320/Tucson2011-39SpanishFluoriteBarite15cm.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5606628518199436274" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://2.bp.blogspot.com/-E6bfgssJURQ/Tc6-4F_d45I/AAAAAAAAEoM/HkV8HFfncpU/s1600/Tucson2010-310SilverAcanthiteReyesMineMexico.jpg"&gt;&lt;img style="display:block; margin:0px auto 10px; text-align:center;cursor:pointer; cursor:hand;width: 320px; height: 282px;" src="http://2.bp.blogspot.com/-E6bfgssJURQ/Tc6-4F_d45I/AAAAAAAAEoM/HkV8HFfncpU/s320/Tucson2010-310SilverAcanthiteReyesMineMexico.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5606628457013175186" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://2.bp.blogspot.com/--X8skRsXzw4/Tc6-0g0L8LI/AAAAAAAAEoE/PDCHrvUxM4s/s1600/Tucson2010-278CopperKeweenawMichigan.jpg"&gt;&lt;img style="display:block; margin:0px auto 10px; text-align:center;cursor:pointer; cursor:hand;width: 200px; height: 320px;" src="http://2.bp.blogspot.com/--X8skRsXzw4/Tc6-0g0L8LI/AAAAAAAAEoE/PDCHrvUxM4s/s320/Tucson2010-278CopperKeweenawMichigan.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5606628395494142130" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://3.bp.blogspot.com/-pWrv7sovBf0/Tc69ufdBYZI/AAAAAAAAEn8/1zWhd5Ig70w/s1600/Denver2009-469RedBerylWahWahUtah.jpg"&gt;&lt;img style="display:block; margin:0px auto 10px; text-align:center;cursor:pointer; cursor:hand;width: 279px; height: 320px;" src="http://3.bp.blogspot.com/-pWrv7sovBf0/Tc69ufdBYZI/AAAAAAAAEn8/1zWhd5Ig70w/s320/Denver2009-469RedBerylWahWahUtah.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5606627192537702802" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;A good challenge: Walk the aisles of the Tucson Gem and Mineral show, and mentally buy the ones you like! I confess, I spent millions in less than 100 yards wow! Here, in order of appearance: rhodochrosite, emerald, again rhodochrosite, native silver, kunzite, fluorite/barite acanthite, native copper and ruby red beryl. Impressive specimens that adorn the museums and private collections, like that of Rep. Romero de Tehuacan Puebla, a beautiful museum with amazing specimens such as legrandita, adamite, pyrites from Naica, etc. I used to take my students to this museum on an unforgettable journey of two days, after visiting the museum, Dr. Romero used to take us to a tour around his state of the art chicken farm. I lost track of my students, and obviously of the Mineral Museum of Tehuacan, unique in Mexico at least in the 80's, of course, the Deputy Romero died a few years ago. &lt;br /&gt;&lt;br /&gt;In a recent visit I did to a gem &amp; mineral show in Houston, I saw specimens worth almost $100,000 USD, I could not believe it. That inspired my title of this post. May 2011&lt;img src="http://feeds.feedburner.com/~r/Mineralogy/~4/b3M3ChMJuSY" height="1" width="1"/&gt;</content><link rel="replies" type="application/atom+xml" href="http://ogshelly.blogspot.com/feeds/2809983440797372717/comments/default" title="Post Comments" /><link rel="replies" type="text/html" href="http://www.blogger.com/comment.g?blogID=609124123307797670&amp;postID=2809983440797372717" title="0 Comments" /><link rel="edit" type="application/atom+xml" href="http://www.blogger.com/feeds/609124123307797670/posts/default/2809983440797372717?v=2" /><link rel="self" type="application/atom+xml" href="http://www.blogger.com/feeds/609124123307797670/posts/default/2809983440797372717?v=2" /><link rel="alternate" type="text/html" href="http://feedproxy.google.com/~r/Mineralogy/~3/b3M3ChMJuSY/if-you-want-to-but-beautiful-minerals.html" title="If you want to buy beautiful minerals, bring lots of money!" /><author><name>Oscar Garcia</name><uri>https://plus.google.com/100300946102962552972</uri><email>noreply@blogger.com</email><gd:image rel="http://schemas.google.com/g/2005#thumbnail" width="32" height="32" src="//lh4.googleusercontent.com/-bTyqdIBIO4E/AAAAAAAAAAI/AAAAAAAAAAA/flc2ZUO4-D0/s512-c/photo.jpg" /></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="http://1.bp.blogspot.com/-65NlkNqklDk/Tc7DuOCY7HI/AAAAAAAAEo8/KOImVA0rqyg/s72-c/Tucson2010-28RhodochrositeAmericanTunnelMineColorado.jpg" height="72" width="72" /><thr:total>0</thr:total><feedburner:origLink>http://ogshelly.blogspot.com/2011/05/if-you-want-to-but-beautiful-minerals.html</feedburner:origLink></entry><entry gd:etag="W/&quot;DEUHR3o-eip7ImA9WhZSEko.&quot;"><id>tag:blogger.com,1999:blog-609124123307797670.post-8128781970549837194</id><published>2011-03-27T13:35:00.008-05:00</published><updated>2011-03-27T20:37:16.452-05:00</updated><app:edited xmlns:app="http://www.w3.org/2007/app">2011-03-27T20:37:16.452-05:00</app:edited><title>Fluorite lego? No, actual crystals directly from Mother Nature</title><content type="html">&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://3.bp.blogspot.com/-zQ-vVJ3bdQs/TY_hlyHq5EI/AAAAAAAAET0/rQBq_HQkT2c/s1600/aquaapatitefluor%2B%25281%2529.jpg"&gt;&lt;img style="display:block; margin:0px auto 10px; text-align:center;cursor:pointer; cursor:hand;width: 320px; height: 273px;" src="http://3.bp.blogspot.com/-zQ-vVJ3bdQs/TY_hlyHq5EI/AAAAAAAAET0/rQBq_HQkT2c/s320/aquaapatitefluor%2B%25281%2529.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5588933701815428162" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://3.bp.blogspot.com/-ihtxZUOHNd4/TY_hOI95WNI/AAAAAAAAETs/77Z-sXhvibg/s1600/Tucson2009-19russianfluorqtz.jpg"&gt;&lt;img style="display:block; margin:0px auto 10px; text-align:center;cursor:pointer; cursor:hand;width: 275px; height: 320px;" src="http://3.bp.blogspot.com/-ihtxZUOHNd4/TY_hOI95WNI/AAAAAAAAETs/77Z-sXhvibg/s320/Tucson2009-19russianfluorqtz.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5588933295631587538" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://2.bp.blogspot.com/-hFb2o_uiDr8/TY_hE4TtMzI/AAAAAAAAETk/3YFFmcsHzw4/s1600/Tucson2009-247RLbignagarfluorite2.jpg"&gt;&lt;img style="display:block; margin:0px auto 10px; text-align:center;cursor:pointer; cursor:hand;width: 289px; height: 320px;" src="http://2.bp.blogspot.com/-hFb2o_uiDr8/TY_hE4TtMzI/AAAAAAAAETk/3YFFmcsHzw4/s320/Tucson2009-247RLbignagarfluorite2.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5588933136540840754" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://3.bp.blogspot.com/-y5jtDCkdbKc/TY_g0ZfYacI/AAAAAAAAETc/AU-Hv8JGxDc/s1600/Tucson2010-132FluoriteSchorl-NagarPakistan.jpg"&gt;&lt;img style="display:block; margin:0px auto 10px; text-align:center;cursor:pointer; cursor:hand;width: 309px; height: 320px;" src="http://3.bp.blogspot.com/-y5jtDCkdbKc/TY_g0ZfYacI/AAAAAAAAETc/AU-Hv8JGxDc/s320/Tucson2010-132FluoriteSchorl-NagarPakistan.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5588932853390404034" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://1.bp.blogspot.com/-KXBhUkrNz0c/TY_eT4zIwnI/AAAAAAAAETU/qtGX5gh1_0I/s1600/Fluorite1.jpg"&gt;&lt;img style="display:block; margin:0px auto 10px; text-align:center;cursor:pointer; cursor:hand;width: 320px; height: 241px;" src="http://1.bp.blogspot.com/-KXBhUkrNz0c/TY_eT4zIwnI/AAAAAAAAETU/qtGX5gh1_0I/s320/Fluorite1.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5588930095835824754" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://2.bp.blogspot.com/-rQXV11kymHo/TY_dg6qV-wI/AAAAAAAAETM/iW9T4pht1F4/s1600/RA12I2.jpg"&gt;&lt;img style="display:block; margin:0px auto 10px; text-align:center;cursor:pointer; cursor:hand;width: 320px; height: 274px;" src="http://2.bp.blogspot.com/-rQXV11kymHo/TY_dg6qV-wI/AAAAAAAAETM/iW9T4pht1F4/s320/RA12I2.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5588929220162484994" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://3.bp.blogspot.com/-I7ACxgUs90E/TY_ddmkXkPI/AAAAAAAAETE/_ZfcIV-9_GU/s1600/NY14K7t.jpg"&gt;&lt;img style="display:block; margin:0px auto 10px; text-align:center;cursor:pointer; cursor:hand;width: 320px; height: 243px;" src="http://3.bp.blogspot.com/-I7ACxgUs90E/TY_ddmkXkPI/AAAAAAAAETE/_ZfcIV-9_GU/s320/NY14K7t.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5588929163229106418" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://1.bp.blogspot.com/-o5I15637g1A/TY_cyqcJM9I/AAAAAAAAES8/QNaxM8e46Is/s1600/Fluorite-TP86R9f.jpg"&gt;&lt;img style="display:block; margin:0px auto 10px; text-align:center;cursor:pointer; cursor:hand;width: 218px; height: 320px;" src="http://1.bp.blogspot.com/-o5I15637g1A/TY_cyqcJM9I/AAAAAAAAES8/QNaxM8e46Is/s320/Fluorite-TP86R9f.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5588928425533977554" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://3.bp.blogspot.com/-73VAkf85lyA/TY_cvGOhS3I/AAAAAAAAES0/_eH5dJ5YD0I/s1600/Fluorite-MK50R9f-upd.jpg"&gt;&lt;img style="display:block; margin:0px auto 10px; text-align:center;cursor:pointer; cursor:hand;width: 320px; height: 299px;" src="http://3.bp.blogspot.com/-73VAkf85lyA/TY_cvGOhS3I/AAAAAAAAES0/_eH5dJ5YD0I/s320/Fluorite-MK50R9f-upd.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5588928364273552242" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;From various locations, in its amazing variety of colors and habits, Fluorite is a fantastic mineral. Let me start from a location I visited for several months, such as Naica, Chihuahua in Northern Mexico whose location is off the "Panamerican Freeway" between Camargo and Delicias. From this mine, fluorite and other beautiful crystals have been collected, and it became world famous for its recently discovered giant gypsum crystals cave. Naica produced unique crystals of fluorite that vary from a very pale pink to almost transparent specimens with pyrite crystals inside, some of these in my private collection. I worked in this mine while I was still in College back in the late 70's, and to tell you the truth, I really enjoyed it, as I was assistant of the most prominent Mineralogist in Mexico Dr Raul Ortiz Asiain, and my passion for minerals was already there.&lt;br /&gt;&lt;br /&gt;Also, pictures of fluorite from Pointe Kurz (3600 m altitude), Mont Blanc Massif, Haute-Savoie, France, and finally from Caldera 3, Mina Moscona, Solís, Corvera, Asturias Spain &lt;br /&gt;&lt;br /&gt;Fluorite:&lt;br /&gt;&lt;br /&gt;Chemical Formula: CaF2&lt;br /&gt;Composition: Molecular Weight = 78.07 gm&lt;br /&gt;Calcium   51.33 %  Ca   71.83 % CaO&lt;br /&gt;Fluorine  48.67 %  F    48.67 % F&lt;br /&gt;Environment: Low temperature vein deposits&lt;br /&gt;Crystal System: Isometric - HexoctahedralH-M Symbol&lt;br /&gt;Cleavage: {111} Perfect, {111} Perfect, {111} Perfect&lt;br /&gt;Color: White, Yellow, Green, Red, Blue.&lt;br /&gt;Density: 3.01 - 3.25, Average = 3.13&lt;br /&gt;Diaphaneity: Transparent to subtranslucent&lt;br /&gt;Fracture: Uneven - Flat surfaces (not cleavage) fractured in an uneven pattern.&lt;br /&gt;Habit: Crystalline - Coarse - Occurs as well-formed coarse sized crystals.&lt;br /&gt;Habit: Disseminated - Occurs in small, distinct particles dispersed in matrix.&lt;br /&gt;Habit: Massive - Granular - Common texture observed in granite and other igneous rock.&lt;br /&gt;Hardness: 4 - Fluorite&lt;br /&gt;Luminescence: Fluorescent, Short UV=blue, Long UV=blue.&lt;br /&gt;Luster: Vitreous (Glassy)&lt;br /&gt;Streak: White&lt;img src="http://feeds.feedburner.com/~r/Mineralogy/~4/4ElMQXsJ4VM" height="1" width="1"/&gt;</content><link rel="replies" type="application/atom+xml" href="http://ogshelly.blogspot.com/feeds/8128781970549837194/comments/default" title="Post Comments" /><link rel="replies" type="text/html" href="http://www.blogger.com/comment.g?blogID=609124123307797670&amp;postID=8128781970549837194" title="2 Comments" /><link rel="edit" type="application/atom+xml" href="http://www.blogger.com/feeds/609124123307797670/posts/default/8128781970549837194?v=2" /><link rel="self" type="application/atom+xml" href="http://www.blogger.com/feeds/609124123307797670/posts/default/8128781970549837194?v=2" /><link rel="alternate" type="text/html" href="http://feedproxy.google.com/~r/Mineralogy/~3/4ElMQXsJ4VM/fluorite-lego-no-actual-crystals.html" title="Fluorite lego? No, actual crystals directly from Mother Nature" /><author><name>Oscar Garcia</name><uri>https://plus.google.com/100300946102962552972</uri><email>noreply@blogger.com</email><gd:image rel="http://schemas.google.com/g/2005#thumbnail" width="32" height="32" src="//lh4.googleusercontent.com/-bTyqdIBIO4E/AAAAAAAAAAI/AAAAAAAAAAA/flc2ZUO4-D0/s512-c/photo.jpg" /></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="http://3.bp.blogspot.com/-zQ-vVJ3bdQs/TY_hlyHq5EI/AAAAAAAAET0/rQBq_HQkT2c/s72-c/aquaapatitefluor%2B%25281%2529.jpg" height="72" width="72" /><thr:total>2</thr:total><feedburner:origLink>http://ogshelly.blogspot.com/2011/03/fluorite-lego-no-actual-crystals.html</feedburner:origLink></entry><entry gd:etag="W/&quot;D0cMQng-eyp7ImA9Wx5QE0Q.&quot;"><id>tag:blogger.com,1999:blog-609124123307797670.post-3739265727323899066</id><published>2010-09-01T21:33:00.002-05:00</published><updated>2010-09-01T21:38:03.653-05:00</updated><app:edited xmlns:app="http://www.w3.org/2007/app">2010-09-01T21:38:03.653-05:00</app:edited><title>Lead vanadate forms Vanadinite, discovered in Mexico</title><content type="html">&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://3.bp.blogspot.com/_JwBNq1qsBN0/TH8NCZ78Y_I/AAAAAAAADFg/JFGjcESQQuM/s1600/Vanadinite-TX97Q8f.jpg"&gt;&lt;img style="display:block; margin:0px auto 10px; text-align:center;cursor:pointer; cursor:hand;width: 232px; height: 320px;" src="http://3.bp.blogspot.com/_JwBNq1qsBN0/TH8NCZ78Y_I/AAAAAAAADFg/JFGjcESQQuM/s320/Vanadinite-TX97Q8f.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5512138803897983986" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;Mine: San Carlos (Mina Apex), San Carlos, Manuel Benavides, Chihuahua  Mexico &lt;br /&gt;Pb5(VO4)3Cl &lt;br /&gt;&lt;br /&gt;Vanadinite is an uncommon mineral, only occurring as the result of chemical alterations to a pre-existing material. It is therefore known as a secondary mineral. It is found in arid climates and forms by oxidation of primary lead minerals. Vanadinite is especially found in association with the lead sulfide, galena. Other associated minerals include wulfenite, limonite, and barite.[2][4][5]&lt;br /&gt;&lt;br /&gt;It was originally discovered in Mexico by the Spanish mineralogist Andrés Manuel del Río in 1801. He called the mineral "brown lead" and asserted that it contained a new element, which he first named pancromium and later, erythronium. However, he was later led to believe that this was not a new element but merely an impure form of chromium. In 1830, Nils Gabriel Sefström discovered a new element, which he named vanadium. It was later revealed that this was identical to the metal discovered earlier by Andrés Manuel del Río. Del Río's "brown lead" was also rediscovered, in 1838 in Zimapan, Hidalgo, Mexico, and was named vanadinite due its high vanadium content. Other names that have since been given to vanadinite are johnstonite and lead vanadate.&lt;br /&gt;&lt;br /&gt;Along with carnotite and roscoelite, vanadinite is one of the main industrial ores of the element vanadium, which can be extracted by roasting and smelting. It is occasionally used as a source of lead. A common process for extracting the vanadium begins with the heating of vanadinite with salt (NaCl) or sodium carbonate (Na2CO3) at about 850°C to produce sodium vanadate (NaVO3). This is dissolved in water and then treated with ammonium chloride to give an orange coloured precipitate of ammonium metavanadate. This is then melted to form a crude form of vanadium pentoxide (V2O5). Reduction of vanadium pentoxide with calcium gives pure vanadium.&lt;br /&gt;&lt;br /&gt;Sources: WEikipedia and the University of life!&lt;img src="http://feeds.feedburner.com/~r/Mineralogy/~4/Lcwzd71q8pA" height="1" width="1"/&gt;</content><link rel="replies" type="application/atom+xml" href="http://ogshelly.blogspot.com/feeds/3739265727323899066/comments/default" title="Post Comments" /><link rel="replies" type="text/html" href="http://www.blogger.com/comment.g?blogID=609124123307797670&amp;postID=3739265727323899066" title="1 Comments" /><link rel="edit" type="application/atom+xml" href="http://www.blogger.com/feeds/609124123307797670/posts/default/3739265727323899066?v=2" /><link rel="self" type="application/atom+xml" href="http://www.blogger.com/feeds/609124123307797670/posts/default/3739265727323899066?v=2" /><link rel="alternate" type="text/html" href="http://feedproxy.google.com/~r/Mineralogy/~3/Lcwzd71q8pA/lead-vanadate-forms-vanadinite.html" title="Lead vanadate forms Vanadinite, discovered in Mexico" /><author><name>Oscar Garcia</name><uri>https://plus.google.com/100300946102962552972</uri><email>noreply@blogger.com</email><gd:image rel="http://schemas.google.com/g/2005#thumbnail" width="32" height="32" src="//lh4.googleusercontent.com/-bTyqdIBIO4E/AAAAAAAAAAI/AAAAAAAAAAA/flc2ZUO4-D0/s512-c/photo.jpg" /></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="http://3.bp.blogspot.com/_JwBNq1qsBN0/TH8NCZ78Y_I/AAAAAAAADFg/JFGjcESQQuM/s72-c/Vanadinite-TX97Q8f.jpg" height="72" width="72" /><thr:total>1</thr:total><feedburner:origLink>http://ogshelly.blogspot.com/2010/09/lead-vanadate-forms-vanadinite.html</feedburner:origLink></entry><entry gd:etag="W/&quot;DkEBRHkycSp7ImA9WxFRGEQ.&quot;"><id>tag:blogger.com,1999:blog-609124123307797670.post-4616747798705783349</id><published>2010-05-03T08:50:00.001-05:00</published><updated>2010-05-03T08:50:55.799-05:00</updated><app:edited xmlns:app="http://www.w3.org/2007/app">2010-05-03T08:50:55.799-05:00</app:edited><title>Featured blog</title><content type="html">&lt;a href="http://makingjewelrysupplies.com/blog_awards/index.php?id=12911"&gt;Blog award&lt;/a&gt;&lt;img src="http://feeds.feedburner.com/~r/Mineralogy/~4/du7vQTfvric" height="1" width="1"/&gt;</content><link rel="replies" type="application/atom+xml" href="http://ogshelly.blogspot.com/feeds/4616747798705783349/comments/default" title="Post Comments" /><link rel="replies" type="text/html" href="http://www.blogger.com/comment.g?blogID=609124123307797670&amp;postID=4616747798705783349" title="0 Comments" /><link rel="edit" type="application/atom+xml" href="http://www.blogger.com/feeds/609124123307797670/posts/default/4616747798705783349?v=2" /><link rel="self" type="application/atom+xml" href="http://www.blogger.com/feeds/609124123307797670/posts/default/4616747798705783349?v=2" /><link rel="alternate" type="text/html" href="http://feedproxy.google.com/~r/Mineralogy/~3/du7vQTfvric/featured-blog.html" title="Featured blog" /><author><name>Oscar Garcia</name><uri>https://plus.google.com/100300946102962552972</uri><email>noreply@blogger.com</email><gd:image rel="http://schemas.google.com/g/2005#thumbnail" width="32" height="32" src="//lh4.googleusercontent.com/-bTyqdIBIO4E/AAAAAAAAAAI/AAAAAAAAAAA/flc2ZUO4-D0/s512-c/photo.jpg" /></author><thr:total>0</thr:total><feedburner:origLink>http://ogshelly.blogspot.com/2010/05/featured-blog.html</feedburner:origLink></entry><entry gd:etag="W/&quot;CEYESX46eCp7ImA9WxFREUs.&quot;"><id>tag:blogger.com,1999:blog-609124123307797670.post-17371918066957592</id><published>2010-04-17T11:06:00.011-05:00</published><updated>2010-04-24T21:21:48.010-05:00</updated><app:edited xmlns:app="http://www.w3.org/2007/app">2010-04-24T21:21:48.010-05:00</app:edited><title>I am sad seeing these beauties in women's rings / collars!</title><content type="html">&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://3.bp.blogspot.com/_JwBNq1qsBN0/S8nfStwlgLI/AAAAAAAACO8/KBxf_i-Wh2w/s1600/tourmaline2.jpg"&gt;&lt;img style="float:left; margin:0 10px 10px 0;cursor:pointer; cursor:hand;width: 320px; height: 319px;" src="http://3.bp.blogspot.com/_JwBNq1qsBN0/S8nfStwlgLI/AAAAAAAACO8/KBxf_i-Wh2w/s320/tourmaline2.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5461141535777456306" /&gt;&lt;/a&gt;In order of appearance:&lt;br /&gt;&lt;br /&gt;Tourmalines on Cleavelandite blades from the Himalaya Mine, Mesa Grande District, San Diego County, California&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://1.bp.blogspot.com/_JwBNq1qsBN0/S8nelsqDgaI/AAAAAAAACO0/NBHhKS-AN2M/s1600/linarite.jpg"&gt;&lt;img style="float:left; margin:0 10px 10px 0;cursor:pointer; cursor:hand;width: 252px; height: 320px;" src="http://1.bp.blogspot.com/_JwBNq1qsBN0/S8nelsqDgaI/AAAAAAAACO0/NBHhKS-AN2M/s320/linarite.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5461140762387513762" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;Linarite from the Grand Reef Mine in Graham County, Arizona&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://3.bp.blogspot.com/_JwBNq1qsBN0/S8ndwGyb-yI/AAAAAAAACOs/v6rSD7oZtdg/s1600/proustite.jpg"&gt;&lt;img style="float:left; margin:0 10px 10px 0;cursor:pointer; cursor:hand;width: 318px; height: 320px;" src="http://3.bp.blogspot.com/_JwBNq1qsBN0/S8ndwGyb-yI/AAAAAAAACOs/v6rSD7oZtdg/s320/proustite.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5461139841689058082" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;Prousite sitting atop a Polybasite cluster from the Uchucchacua Mine, Oyon Province, Lima Department, Peru.&lt;br /&gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://3.bp.blogspot.com/_JwBNq1qsBN0/S8ndOpndeUI/AAAAAAAACOk/vcI9zFq_B80/s1600/tourmaline.jpg"&gt;&lt;img style="float:left; margin:0 10px 10px 0;cursor:pointer; cursor:hand;width: 258px; height: 320px;" src="http://3.bp.blogspot.com/_JwBNq1qsBN0/S8ndOpndeUI/AAAAAAAACOk/vcI9zFq_B80/s320/tourmaline.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5461139266922707266" /&gt;&lt;/a&gt;Tourmaline from the 1974 Pocket, Tourmaline Queen Mine, San Diego County, California&lt;br /&gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://1.bp.blogspot.com/_JwBNq1qsBN0/S8ncvbYQaNI/AAAAAAAACOU/hOvAU_0eUYQ/s1600/galena.jpg"&gt;&lt;img style="float:left; margin:0 10px 10px 0;cursor:pointer; cursor:hand;width: 276px; height: 320px;" src="http://1.bp.blogspot.com/_JwBNq1qsBN0/S8ncvbYQaNI/AAAAAAAACOU/hOvAU_0eUYQ/s320/galena.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5461138730524895442" /&gt;&lt;/a&gt;Galena from the Tsumeb Mine in Tsumeb, Namibia, SW Africa.&lt;br /&gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://2.bp.blogspot.com/_JwBNq1qsBN0/S8nckrdEaKI/AAAAAAAACOM/0dSHu0EN5sA/s1600/adamite.jpg"&gt;&lt;img style="float:left; margin:0 10px 10px 0;cursor:pointer; cursor:hand;width: 320px; height: 254px;" src="http://2.bp.blogspot.com/_JwBNq1qsBN0/S8nckrdEaKI/AAAAAAAACOM/0dSHu0EN5sA/s320/adamite.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5461138545861486754" /&gt;&lt;/a&gt;Adamite from the Ojuela mine in Mapimi, Durango Mexico&lt;img src="http://feeds.feedburner.com/~r/Mineralogy/~4/GzLThXXj43c" height="1" width="1"/&gt;</content><link rel="replies" type="application/atom+xml" href="http://ogshelly.blogspot.com/feeds/17371918066957592/comments/default" title="Post Comments" /><link rel="replies" type="text/html" href="http://www.blogger.com/comment.g?blogID=609124123307797670&amp;postID=17371918066957592" title="2 Comments" /><link rel="edit" type="application/atom+xml" href="http://www.blogger.com/feeds/609124123307797670/posts/default/17371918066957592?v=2" /><link rel="self" type="application/atom+xml" href="http://www.blogger.com/feeds/609124123307797670/posts/default/17371918066957592?v=2" /><link rel="alternate" type="text/html" href="http://feedproxy.google.com/~r/Mineralogy/~3/GzLThXXj43c/tourmaline-gold-with-calcite-and-pyrite.html" title="I am sad seeing these beauties in women's rings / collars!" /><author><name>Oscar Garcia</name><uri>https://plus.google.com/100300946102962552972</uri><email>noreply@blogger.com</email><gd:image rel="http://schemas.google.com/g/2005#thumbnail" width="32" height="32" src="//lh4.googleusercontent.com/-bTyqdIBIO4E/AAAAAAAAAAI/AAAAAAAAAAA/flc2ZUO4-D0/s512-c/photo.jpg" /></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="http://3.bp.blogspot.com/_JwBNq1qsBN0/S8nfStwlgLI/AAAAAAAACO8/KBxf_i-Wh2w/s72-c/tourmaline2.jpg" height="72" width="72" /><thr:total>2</thr:total><feedburner:origLink>http://ogshelly.blogspot.com/2010/04/tourmaline-gold-with-calcite-and-pyrite.html</feedburner:origLink></entry><entry gd:etag="W/&quot;A0ENRH4zeyp7ImA9WxFSFUw.&quot;"><id>tag:blogger.com,1999:blog-609124123307797670.post-5253348439604722711</id><published>2010-04-17T10:30:00.007-05:00</published><updated>2010-04-17T10:54:55.083-05:00</updated><app:edited xmlns:app="http://www.w3.org/2007/app">2010-04-17T10:54:55.083-05:00</app:edited><title>For sure, these crystals ore from another galaxy!</title><content type="html">&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://1.bp.blogspot.com/_JwBNq1qsBN0/S8nYW0TePFI/AAAAAAAACOE/HiZYitmDWzw/s1600/emeraldrussian.jpg"&gt;&lt;img style="float:left; margin:0 10px 10px 0;cursor:pointer; cursor:hand;width: 293px; height: 320px;" src="http://1.bp.blogspot.com/_JwBNq1qsBN0/S8nYW0TePFI/AAAAAAAACOE/HiZYitmDWzw/s320/emeraldrussian.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5461133909672475730" /&gt;&lt;/a&gt;By order of appearance: &lt;br /&gt;&lt;br /&gt;Beryl var. Emerald from a locality near Alabashka, Ural Mountains, Russia&lt;br /&gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://3.bp.blogspot.com/_JwBNq1qsBN0/S8nYJPUDYkI/AAAAAAAACN8/PtpkGyVQVQ0/s1600/amazonite.jpg"&gt;&lt;img style="float:left; margin:0 10px 10px 0;cursor:pointer; cursor:hand;width: 320px; height: 237px;" src="http://3.bp.blogspot.com/_JwBNq1qsBN0/S8nYJPUDYkI/AAAAAAAACN8/PtpkGyVQVQ0/s320/amazonite.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5461133676404499010" /&gt;&lt;/a&gt;Amazonite crystals with Smoky Quartz and Albite from Sentinel Rock, El Paso County, Colorado&lt;br /&gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://3.bp.blogspot.com/_JwBNq1qsBN0/S8nXdXcCwbI/AAAAAAAACN0/3NqVFyyPS6k/s1600/silver.jpg"&gt;&lt;img style="float:left; margin:0 10px 10px 0;cursor:pointer; cursor:hand;width: 280px; height: 320px;" src="http://3.bp.blogspot.com/_JwBNq1qsBN0/S8nXdXcCwbI/AAAAAAAACN0/3NqVFyyPS6k/s320/silver.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5461132922671251890" /&gt;&lt;/a&gt;Silver from Imiter Mine in Morocco&lt;br /&gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://2.bp.blogspot.com/_JwBNq1qsBN0/S8nWwzH7aSI/AAAAAAAACNk/T7B2pviMUQ0/s1600/scheelite.jpg"&gt;&lt;img style="float:left; margin:0 10px 10px 0;cursor:pointer; cursor:hand;width: 320px; height: 218px;" src="http://2.bp.blogspot.com/_JwBNq1qsBN0/S8nWwzH7aSI/AAAAAAAACNk/T7B2pviMUQ0/s320/scheelite.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5461132157008963874" /&gt;&lt;/a&gt;Scheelite with fluorite and muscovite from the Mt. Xuebaoding Mine, Pingwu, Sichuan Province of China&lt;br /&gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://3.bp.blogspot.com/_JwBNq1qsBN0/S8nWgCmTm2I/AAAAAAAACNc/GpoUC5SXLDw/s1600/redberyl.jpg"&gt;&lt;img style="float:left; margin:0 10px 10px 0;cursor:pointer; cursor:hand;width: 279px; height: 320px;" src="http://3.bp.blogspot.com/_JwBNq1qsBN0/S8nWgCmTm2I/AAAAAAAACNc/GpoUC5SXLDw/s320/redberyl.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5461131869105134434" /&gt;&lt;/a&gt;Red beryl from the Wah Wah Mountains near Delta, Utah&lt;br /&gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://2.bp.blogspot.com/_JwBNq1qsBN0/S8nWXsR8czI/AAAAAAAACNU/XuIH2raFxpU/s1600/mimetite.jpg"&gt;&lt;img style="float:left; margin:0 10px 10px 0;cursor:pointer; cursor:hand;width: 320px; height: 228px;" src="http://2.bp.blogspot.com/_JwBNq1qsBN0/S8nWXsR8czI/AAAAAAAACNU/XuIH2raFxpU/s320/mimetite.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5461131725675197234" /&gt;&lt;/a&gt;Mimetite from San Pedro Corralitos, Chihuahua Mexico&lt;br /&gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://2.bp.blogspot.com/_JwBNq1qsBN0/S8nXCCoGvMI/AAAAAAAACNs/dIQN0HuSHW4/s1600/spessartine+garnets.jpg"&gt;&lt;img style="float:left; margin:0 10px 10px 0;cursor:pointer; cursor:hand;width: 320px; height: 234px;" src="http://2.bp.blogspot.com/_JwBNq1qsBN0/S8nXCCoGvMI/AAAAAAAACNs/dIQN0HuSHW4/s320/spessartine+garnets.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5461132453228231874" /&gt;&lt;/a&gt;Spessartine garnets from Nani, Loliondo, Arusha Region, Tanzania&lt;img src="http://feeds.feedburner.com/~r/Mineralogy/~4/VjdqY0ZGYts" height="1" width="1"/&gt;</content><link rel="replies" type="application/atom+xml" href="http://ogshelly.blogspot.com/feeds/5253348439604722711/comments/default" title="Post Comments" /><link rel="replies" type="text/html" href="http://www.blogger.com/comment.g?blogID=609124123307797670&amp;postID=5253348439604722711" title="3 Comments" /><link rel="edit" type="application/atom+xml" href="http://www.blogger.com/feeds/609124123307797670/posts/default/5253348439604722711?v=2" /><link rel="self" type="application/atom+xml" href="http://www.blogger.com/feeds/609124123307797670/posts/default/5253348439604722711?v=2" /><link rel="alternate" type="text/html" href="http://feedproxy.google.com/~r/Mineralogy/~3/VjdqY0ZGYts/spessartine-garnets-from-nani-loliondo.html" title="For sure, these crystals ore from another galaxy!" /><author><name>Oscar Garcia</name><uri>https://plus.google.com/100300946102962552972</uri><email>noreply@blogger.com</email><gd:image rel="http://schemas.google.com/g/2005#thumbnail" width="32" height="32" src="//lh4.googleusercontent.com/-bTyqdIBIO4E/AAAAAAAAAAI/AAAAAAAAAAA/flc2ZUO4-D0/s512-c/photo.jpg" /></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="http://1.bp.blogspot.com/_JwBNq1qsBN0/S8nYW0TePFI/AAAAAAAACOE/HiZYitmDWzw/s72-c/emeraldrussian.jpg" height="72" width="72" /><thr:total>3</thr:total><feedburner:origLink>http://ogshelly.blogspot.com/2010/04/spessartine-garnets-from-nani-loliondo.html</feedburner:origLink></entry><entry gd:etag="W/&quot;A0AEQnY4fSp7ImA9WxBXE0g.&quot;"><id>tag:blogger.com,1999:blog-609124123307797670.post-8969678058962255692</id><published>2010-01-24T12:43:00.009-06:00</published><updated>2010-01-24T13:01:43.835-06:00</updated><app:edited xmlns:app="http://www.w3.org/2007/app">2010-01-24T13:01:43.835-06:00</app:edited><title>More jaw dropping specimens!</title><content type="html">&lt;a href="http://1.bp.blogspot.com/_JwBNq1qsBN0/S1yXmYiVmGI/AAAAAAAAByM/ASuLqYns4dY/s1600-h/MAR20-image2.jpg"&gt;&lt;img style="float:left; margin:0 10px 10px 0;cursor:pointer; cursor:hand;width: 320px; height: 270px;" src="http://1.bp.blogspot.com/_JwBNq1qsBN0/S1yXmYiVmGI/AAAAAAAAByM/ASuLqYns4dY/s320/MAR20-image2.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5430381936379271266" /&gt;&lt;/a&gt;Kunzite, Elbaite, Quartz and Albite &lt;br /&gt;Cabinet &lt;br /&gt;Nuristan &lt;br /&gt;Laghman Prov., Afghanistan, Asia &lt;br /&gt;&lt;br /&gt;&lt;a href="http://2.bp.blogspot.com/_JwBNq1qsBN0/S1yWbXgGaHI/AAAAAAAAByE/vyaWo9uoHco/s1600-h/1TCG03-image.jpg"&gt;&lt;img style="float:left; margin:0 10px 10px 0;cursor:pointer; cursor:hand;width: 287px; height: 320px;" src="http://2.bp.blogspot.com/_JwBNq1qsBN0/S1yWbXgGaHI/AAAAAAAAByE/vyaWo9uoHco/s320/1TCG03-image.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5430380647611263090" /&gt;&lt;/a&gt;Fluorite &lt;br /&gt;Miniature &lt;br /&gt;Dow Scar Vein, Hilton Mine &lt;br /&gt;Scordale, Cumbria, England, Europe &lt;br /&gt;&lt;br /&gt;&lt;a href="http://4.bp.blogspot.com/_JwBNq1qsBN0/S1yWU3b-N8I/AAAAAAAABx8/qOEaWWJ9zrE/s1600-h/1TCG08-image2.jpg"&gt;&lt;img style="float:left; margin:0 10px 10px 0;cursor:pointer; cursor:hand;width: 320px; height: 314px;" src="http://4.bp.blogspot.com/_JwBNq1qsBN0/S1yWU3b-N8I/AAAAAAAABx8/qOEaWWJ9zrE/s320/1TCG08-image2.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5430380535924799426" /&gt;&lt;/a&gt;Rhodochrosite &lt;br /&gt;Small Miniature &lt;br /&gt;Santa Eulalia &lt;br /&gt;Chihuahua, Mexico &lt;br /&gt;&lt;br /&gt;&lt;a href="http://4.bp.blogspot.com/_JwBNq1qsBN0/S1yWP0tmsHI/AAAAAAAABx0/pyATsYtMA_A/s1600-h/image_1.jpg"&gt;&lt;img style="float:left; margin:0 10px 10px 0;cursor:pointer; cursor:hand;width: 320px; height: 300px;" src="http://4.bp.blogspot.com/_JwBNq1qsBN0/S1yWP0tmsHI/AAAAAAAABx0/pyATsYtMA_A/s320/image_1.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5430380449294102642" /&gt;&lt;/a&gt;Neptunite &lt;br /&gt;Small Cabinet &lt;br /&gt;Benitoite Gem Mine &lt;br /&gt;San Benito County, California &lt;br /&gt;&lt;br /&gt;&lt;a href="http://3.bp.blogspot.com/_JwBNq1qsBN0/S1yWJ3kpZNI/AAAAAAAABxs/CmcRBNv2gN4/s1600-h/1TCG07-image.jpg"&gt;&lt;img style="float:left; margin:0 10px 10px 0;cursor:pointer; cursor:hand;width: 309px; height: 320px;" src="http://3.bp.blogspot.com/_JwBNq1qsBN0/S1yWJ3kpZNI/AAAAAAAABxs/CmcRBNv2gN4/s320/1TCG07-image.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5430380346982622418" /&gt;&lt;/a&gt;Wulfenite &lt;br /&gt;Thumbnail &lt;br /&gt;Los Lamentos &lt;br /&gt;Chihuahua, Mexico&lt;img src="http://feeds.feedburner.com/~r/Mineralogy/~4/3g1nGUaASHY" height="1" width="1"/&gt;</content><link rel="replies" type="application/atom+xml" href="http://ogshelly.blogspot.com/feeds/8969678058962255692/comments/default" title="Post Comments" /><link rel="replies" type="text/html" href="http://www.blogger.com/comment.g?blogID=609124123307797670&amp;postID=8969678058962255692" title="5 Comments" /><link rel="edit" type="application/atom+xml" href="http://www.blogger.com/feeds/609124123307797670/posts/default/8969678058962255692?v=2" /><link rel="self" type="application/atom+xml" href="http://www.blogger.com/feeds/609124123307797670/posts/default/8969678058962255692?v=2" /><link rel="alternate" type="text/html" href="http://feedproxy.google.com/~r/Mineralogy/~3/3g1nGUaASHY/more-jaw-dropping-specimens.html" title="More jaw dropping specimens!" /><author><name>Oscar Garcia</name><uri>https://plus.google.com/100300946102962552972</uri><email>noreply@blogger.com</email><gd:image rel="http://schemas.google.com/g/2005#thumbnail" width="32" height="32" src="//lh4.googleusercontent.com/-bTyqdIBIO4E/AAAAAAAAAAI/AAAAAAAAAAA/flc2ZUO4-D0/s512-c/photo.jpg" /></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="http://1.bp.blogspot.com/_JwBNq1qsBN0/S1yXmYiVmGI/AAAAAAAAByM/ASuLqYns4dY/s72-c/MAR20-image2.jpg" height="72" width="72" /><thr:total>5</thr:total><feedburner:origLink>http://ogshelly.blogspot.com/2010/01/more-jaw-dropping-specimens.html</feedburner:origLink></entry><entry gd:etag="W/&quot;DkQCRX8_fCp7ImA9WxNaEks.&quot;"><id>tag:blogger.com,1999:blog-609124123307797670.post-2768897983920703189</id><published>2009-11-26T09:36:00.015-06:00</published><updated>2009-11-26T13:39:24.144-06:00</updated><app:edited xmlns:app="http://www.w3.org/2007/app">2009-11-26T13:39:24.144-06:00</app:edited><title>Specimens with a beauty beyond this planet!</title><content type="html">Magnificent specimens I am glad to welcome to my blog. These are jaw-dropping, breath-taking minerals, with a beauty beyond this world! Some of those are on sale by &lt;a href="http://www.exceptionalminerals.com/" target="http://www.exceptionalminerals.com/"&gt;Exceptional minerals&lt;/a&gt;. The description of each mineral follows the order of the pictures: &lt;br /&gt;&lt;br /&gt;Golden Calcite (CaCO3)crystal on Barite (BaSO4)from the Elmwood Mine, Smith County, Tennessee.&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://3.bp.blogspot.com/_JwBNq1qsBN0/Sw6iXry0jRI/AAAAAAAABhc/0Qa4YnchAV0/s1600/calcite%26baryte.jpg"&gt;&lt;img style="float:right; margin:0 0 10px 10px;cursor:pointer; cursor:hand;width: 320px; height: 189px;" src="http://3.bp.blogspot.com/_JwBNq1qsBN0/Sw6iXry0jRI/AAAAAAAABhc/0Qa4YnchAV0/s320/calcite%26baryte.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5408438730295119122" /&gt;&lt;/a&gt;&lt;br /&gt;Gorgeous deep cherry-red Rhodochrosite (MnCO3) rhombs Trigonal - Hexagonal Scalenohedral with Quartz on Tetrahedrite matrix from the Millennium Pocket of the Fluorite raise, Sweet Home Mine in Alma, Colorado now closed.&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://4.bp.blogspot.com/_JwBNq1qsBN0/Sw6h-UL2UCI/AAAAAAAABhU/QXfp9XjYiSc/s1600/rhodochrosite.jpg"&gt;&lt;img style="float:right; margin:0 0 10px 10px;cursor:pointer; cursor:hand;width: 267px; height: 320px;" src="http://4.bp.blogspot.com/_JwBNq1qsBN0/Sw6h-UL2UCI/AAAAAAAABhU/QXfp9XjYiSc/s320/rhodochrosite.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5408438294460911650" /&gt;&lt;/a&gt;&lt;br /&gt;The gold on quartz collected from the San Pedro Mine in Santa Fe county New Mexico is on sale for $45,000 USD, I am sure that the gold price of $1,160 US/oz fueled this price tag among its rarity and beauty, just affordable by affluent collectors, or by well funded museums. &lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://1.bp.blogspot.com/_JwBNq1qsBN0/Sw6hlCxUs8I/AAAAAAAABhM/qWGnrEdKDYE/s1600/goldcalpyrite.jpg"&gt;&lt;img style="float:right; margin:0 0 10px 10px;cursor:pointer; cursor:hand;width: 320px; height: 257px;" src="http://1.bp.blogspot.com/_JwBNq1qsBN0/Sw6hlCxUs8I/AAAAAAAABhM/qWGnrEdKDYE/s320/goldcalpyrite.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5408437860289524674" /&gt;&lt;/a&gt;&lt;br /&gt;Beryl var. Aquamarine (Be3Al2Si6O18)crystal sitting atop bronze Muscovite (KAl2(Si3Al)O10(OH,F)2)blades from Nagar, Aliabad, Hunza Valley, Northern Areas of Pakistan.&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://2.bp.blogspot.com/_JwBNq1qsBN0/Sw6ggywyyoI/AAAAAAAABhE/Vt6y1TgjUmI/s1600/aquamarine.jpg"&gt;&lt;img style="float:right; margin:0 0 10px 10px;cursor:pointer; cursor:hand;width: 265px; height: 320px;" src="http://2.bp.blogspot.com/_JwBNq1qsBN0/Sw6ggywyyoI/AAAAAAAABhE/Vt6y1TgjUmI/s320/aquamarine.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5408436687761230466" /&gt;&lt;/a&gt; &lt;br /&gt;Grossular (garnet Ca3Al2(SiO4)3)), and Diopside (CaMg(Si2O6) from Val d'Aosta, Italy. &lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://3.bp.blogspot.com/_JwBNq1qsBN0/Sv9L8D2ZRzI/AAAAAAAABdM/bp3WuXLQyfU/s1600-h/grossular2.JPG"&gt;&lt;img style="float:right; margin:0 0 10px 10px;cursor:pointer; cursor:hand;width: 320px; height: 277px;" src="http://3.bp.blogspot.com/_JwBNq1qsBN0/Sv9L8D2ZRzI/AAAAAAAABdM/bp3WuXLQyfU/s320/grossular2.JPG" border="0" alt=""id="BLOGGER_PHOTO_ID_5404121573065574194" /&gt;&lt;/a&gt; &lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://1.bp.blogspot.com/_JwBNq1qsBN0/Sv9NaLkvzXI/AAAAAAAABdc/tKAIklz_874/s1600-h/Diopside.jpg"&gt;&lt;img style="float:right; margin:0 0 10px 10px;cursor:pointer; cursor:hand;width: 320px; height: 213px;" src="http://1.bp.blogspot.com/_JwBNq1qsBN0/Sv9NaLkvzXI/AAAAAAAABdc/tKAIklz_874/s320/Diopside.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5404123190046739826" /&gt;&lt;/a&gt;&lt;img src="http://feeds.feedburner.com/~r/Mineralogy/~4/3EikOQNv5sg" height="1" width="1"/&gt;</content><link rel="replies" type="application/atom+xml" href="http://ogshelly.blogspot.com/feeds/2768897983920703189/comments/default" title="Post Comments" /><link rel="replies" type="text/html" href="http://www.blogger.com/comment.g?blogID=609124123307797670&amp;postID=2768897983920703189" title="3 Comments" /><link rel="edit" type="application/atom+xml" href="http://www.blogger.com/feeds/609124123307797670/posts/default/2768897983920703189?v=2" /><link rel="self" type="application/atom+xml" href="http://www.blogger.com/feeds/609124123307797670/posts/default/2768897983920703189?v=2" /><link rel="alternate" type="text/html" href="http://feedproxy.google.com/~r/Mineralogy/~3/3EikOQNv5sg/blog-post_26.html" title="Specimens with a beauty beyond this planet!" /><author><name>Oscar Garcia</name><uri>https://plus.google.com/100300946102962552972</uri><email>noreply@blogger.com</email><gd:image rel="http://schemas.google.com/g/2005#thumbnail" width="32" height="32" src="//lh4.googleusercontent.com/-bTyqdIBIO4E/AAAAAAAAAAI/AAAAAAAAAAA/flc2ZUO4-D0/s512-c/photo.jpg" /></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="http://3.bp.blogspot.com/_JwBNq1qsBN0/Sw6iXry0jRI/AAAAAAAABhc/0Qa4YnchAV0/s72-c/calcite%26baryte.jpg" height="72" width="72" /><thr:total>3</thr:total><feedburner:origLink>http://ogshelly.blogspot.com/2009/11/blog-post_26.html</feedburner:origLink></entry><entry gd:etag="W/&quot;DUMGQXw9cSp7ImA9WxNRFk8.&quot;"><id>tag:blogger.com,1999:blog-609124123307797670.post-7641770747608987481</id><published>2009-09-10T18:45:00.004-05:00</published><updated>2009-09-10T19:03:40.269-05:00</updated><app:edited xmlns:app="http://www.w3.org/2007/app">2009-09-10T19:03:40.269-05:00</app:edited><title>Apatite / Apatita var. Esparriguina, what a name uh?</title><content type="html">&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://3.bp.blogspot.com/_JwBNq1qsBN0/SqmPneruM6I/AAAAAAAABGU/OjUu1MUg1gE/s1600-h/apatite.jpg"&gt;&lt;img style="float:right; margin:0 0 10px 10px;cursor:pointer; cursor:hand;width: 320px; height: 224px;" src="http://3.bp.blogspot.com/_JwBNq1qsBN0/SqmPneruM6I/AAAAAAAABGU/OjUu1MUg1gE/s320/apatite.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5379989138284884898" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;This is a beautiful mineral rarely found in good crystals, this particular one from the Market Hill (Cerro del Mercado) in Durango, state of Durango, Mexico. Variety of this pale yellow specimen is named "Esparriguina." &lt;br /&gt;&lt;br /&gt;Apatite is actually three different minerals depending on the predominance of either fluorine, chlorine or the hydroxyl group. These ions can freely substitute in the crystal lattice and all three are usually present in every specimen although some specimens have been close to 100% in one or the other. The rather non-inventive names of these minerals are Fluorapatite, Chlorapatite and Hydroxylapatite. The three are usually considered together due to the difficulty in distinguishing them in hand samples using ordinary methods.&lt;br /&gt;&lt;br /&gt;An irony of the name apatite is that apatite is the mineral that makes up the teeth in all vertebrate animals as well as their bones. Get it? Apatite - teeth! Anyway, the name apatite comes from a Greek word meaning to decieve in allusion to its similarity to other more valuable minerals such as olivine, peridot and beryl.&lt;br /&gt;&lt;br /&gt;Apatite is widely distributed in all rock types; igneous, sedimentary and metamorphic, but is usually just small disseminated grains or cryptocrystalline fragments. Large well formed crystals though can be found in certain contact metamorphic rocks. Very gemmy crystals of apatite can be cut as gems but the softness of apatite prevents wide distribution or acceptance of apatite as a gemstone.&lt;br /&gt;&lt;br /&gt;Let's go technical:&lt;br /&gt;Chemical Formula: Ca5(PO4)3(OH,F,Cl)&lt;br /&gt;Name Origin: Named in 1788 from the Greek apatao - "I am misleading." Reason is that it mislead to confuse for some valuable minerals, such as olivinite, etc.&lt;br /&gt;Crystal System: Hexagonal - Dipyramidal &lt;br /&gt;Cleavage: {0001} Indistinct, {1010} Indistinct&lt;br /&gt;Color: White, Yellow, Green, Red, Blue.&lt;br /&gt;Density: 3.16 - 3.22, Average = 3.19&lt;br /&gt;Diaphaneity: Transparent to translucent&lt;br /&gt;Fracture: Conchoidal - Fractures developed in brittle materials characterized by smoothly curving surfaces, (e.g. quartz).&lt;br /&gt;Habit: Colloform - Forming from a gel or colloidal mass.&lt;br /&gt;Habit: Earthy - Dull, clay-like texture with no visible crystalline affinities, (e.g. howlite).&lt;br /&gt;Habit: Massive - Granular - Common texture observed in granite and other igneous rock. Crystal Habits include the typical hexagonal prism with the hexagonal pyramid or a pinacoid or both as a termination. Also accicular, granular, reniform and massive. A cryptocrystalline variety is called collophane and can make up a rock type called phosphorite and also can replace fossil fragments.&lt;br /&gt;Hardness: 5 &lt;br /&gt;Luminescence: Non-fluorescent.&lt;br /&gt;Luster: Vitreous (Glassy)&lt;br /&gt;Streak: White&lt;br /&gt;&lt;br /&gt;Associated Minerals are hornblende, micas, nepheline and calcite.&lt;br /&gt;Other Characteristics: An unusual "partially dissolved" look similar to the look of previously sucked on hard candy.&lt;br /&gt;&lt;br /&gt;Notable Occurrences include Durango, Mexico; Bancroft, Ontario; Germany and Russia.&lt;br /&gt;Best Field Indicators are crystal habit, color, hardness and look.&lt;br /&gt;Radioactivity: Apatite is Not Radioactive&lt;br /&gt;&lt;br /&gt;I apologize, took a little while to post another one, been busy. I hope you are doing good.&lt;br /&gt;&lt;br /&gt;Best regards,&lt;br /&gt;Oscar G. Shelly&lt;img src="http://feeds.feedburner.com/~r/Mineralogy/~4/Tk0-WO_yYEE" height="1" width="1"/&gt;</content><link rel="replies" type="application/atom+xml" href="http://ogshelly.blogspot.com/feeds/7641770747608987481/comments/default" title="Post Comments" /><link rel="replies" type="text/html" href="http://www.blogger.com/comment.g?blogID=609124123307797670&amp;postID=7641770747608987481" title="0 Comments" /><link rel="edit" type="application/atom+xml" href="http://www.blogger.com/feeds/609124123307797670/posts/default/7641770747608987481?v=2" /><link rel="self" type="application/atom+xml" href="http://www.blogger.com/feeds/609124123307797670/posts/default/7641770747608987481?v=2" /><link rel="alternate" type="text/html" href="http://feedproxy.google.com/~r/Mineralogy/~3/Tk0-WO_yYEE/apatite-apatita-var-esparriguina-what.html" title="Apatite / Apatita var. Esparriguina, what a name uh?" /><author><name>Oscar Garcia</name><uri>https://plus.google.com/100300946102962552972</uri><email>noreply@blogger.com</email><gd:image rel="http://schemas.google.com/g/2005#thumbnail" width="32" height="32" src="//lh4.googleusercontent.com/-bTyqdIBIO4E/AAAAAAAAAAI/AAAAAAAAAAA/flc2ZUO4-D0/s512-c/photo.jpg" /></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="http://3.bp.blogspot.com/_JwBNq1qsBN0/SqmPneruM6I/AAAAAAAABGU/OjUu1MUg1gE/s72-c/apatite.jpg" height="72" width="72" /><thr:total>0</thr:total><feedburner:origLink>http://ogshelly.blogspot.com/2009/09/apatite-apatita-var-esparriguina-what.html</feedburner:origLink></entry><entry gd:etag="W/&quot;C0AARH85eCp7ImA9WxVWGEo.&quot;"><id>tag:blogger.com,1999:blog-609124123307797670.post-3920036514858814986</id><published>2009-02-28T14:51:00.008-06:00</published><updated>2009-02-28T19:42:25.120-06:00</updated><app:edited xmlns:app="http://www.w3.org/2007/app">2009-02-28T19:42:25.120-06:00</app:edited><title>Caramel? no, not at all, fire agate, one of many quartz' forms</title><content type="html">&lt;a href="http://3.bp.blogspot.com/_JwBNq1qsBN0/SammAzR0_LI/AAAAAAAAAHE/4xUZhI3CvTQ/s1600-h/fireagate.jpg"&gt;&lt;img style="float:right; margin:0 0 10px 10px;cursor:pointer; cursor:hand;width: 320px; height: 250px;" src="http://3.bp.blogspot.com/_JwBNq1qsBN0/SammAzR0_LI/AAAAAAAAAHE/4xUZhI3CvTQ/s320/fireagate.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5307956168528034994" /&gt;&lt;/a&gt;&lt;br /&gt;Fire agate&lt;br /&gt;&lt;br /&gt;Probably one the most fascinating mineral combinations there is (according to me), hematite and amorphus silica (quartz). I'd say this is the equivalent to an opal, only the iridiscense is not because of water molecules, but because of the iron oxide embedded in the silica. First time I saw one of these specimens - common in Aguascalientes, Mexico - was in college in my Mineralogy class back in 1975 (Faculty of Engineering of the National Autonomous University of Mexico), and I fell off my chair, I was in shock with the beauty of this baby.&lt;br /&gt;&lt;br /&gt;Anyhow, I am not sure why this mineral has never made it to precious stone status, but if I ever become president of the Mexico, I'll declare it the stone of the country. If you don't like it as much as I do, don't vote for me.&lt;br /&gt;&lt;br /&gt;Ok, let us see what are the fire agate (another form of quartz) life technical specifications:&lt;br /&gt;&lt;br /&gt;Chemical Formula:  SiO2  &lt;br /&gt;Environment:  Sedimentary, metamorphic, and igneous rocks.  &lt;br /&gt;Locality:  Very common mineral found world wide.  &lt;br /&gt;Name Origin: From the German "quarz", of uncertain origin according to many, however I heard once that it comes from the old saxonic that means ice very frozen.&lt;br /&gt;  &lt;br /&gt;Synonyms of quartz:  &lt;br /&gt;&lt;br /&gt;   Agate - banded variety of chaledony  &lt;br /&gt;   Amethyst - purple  &lt;br /&gt;   Avanturine - feebly translucent chalcedony  &lt;br /&gt;   Carnelian - flesh red chalcedony  &lt;br /&gt;   Cat's Eye - chatoyant  &lt;br /&gt;   Chalcedony - microcrystalline quartz  &lt;br /&gt;   Chert - cryptocrystalline quartz  &lt;br /&gt;   Chrysoprase - apple green chalcedony  &lt;br /&gt;   Citrine - yellow  &lt;br /&gt;   Flint - microcrystalline quartz  &lt;br /&gt;   Hornstone - flint  &lt;br /&gt;   Jasper - red or brown chalcedony  &lt;br /&gt;   Moss Agate - variety of chaledony  &lt;br /&gt;   Plasma - green chalcedony  &lt;br /&gt;   Prase - leek green chalcedony  &lt;br /&gt;   Rock Crystal  &lt;br /&gt;   Rose Quartz - rose colored  &lt;br /&gt;   Sapphire Quartz - blue colored  &lt;br /&gt;   Smoky Quartz - brown to black  &lt;br /&gt;   Tiger Eye - pseudomorph of asbestos &lt;br /&gt;&lt;br /&gt;Cleavage:  [0110] Indistinct  &lt;br /&gt;Color:  Brown, Colorless, Violet, Gray, Yellow.  &lt;br /&gt;Density: 2.6 - 2.65, Average = 2.62  &lt;br /&gt;Diaphaniety: Transparent  &lt;br /&gt;Fracture: Conchoidal - Fractures developed in brittle materials characterized by smoothly curving surfaces, (e.g. quartz).  &lt;br /&gt;Habits: Crystalline - Coarse - Occurs as well-formed coarse sized crystals.  &lt;br /&gt;        Crystalline - Fine - Occurs as well-formed fine sized crystals.  &lt;br /&gt;        Druse - Crystal growth in a cavity which results in numerous crystal tipped surfaces.  &lt;br /&gt;Hardness: 7 - Quartz  &lt;br /&gt;Luminescence: Triboluminescent.  &lt;br /&gt;Luster: Vitreous (Glassy)  &lt;br /&gt;Streak: White&lt;br /&gt;&lt;br /&gt;I hope you enjoy a terrific weekend, today is 2/28/09, visit my website if you have some chance: &lt;a href="http://www.freewebs.com/ogshelly"&gt;Oscar el Mexicano&lt;/a&gt;&lt;img src="http://feeds.feedburner.com/~r/Mineralogy/~4/86XZS9J5Dcw" height="1" width="1"/&gt;</content><link rel="replies" type="application/atom+xml" href="http://ogshelly.blogspot.com/feeds/3920036514858814986/comments/default" title="Post Comments" /><link rel="replies" type="text/html" href="http://www.blogger.com/comment.g?blogID=609124123307797670&amp;postID=3920036514858814986" title="0 Comments" /><link rel="edit" type="application/atom+xml" href="http://www.blogger.com/feeds/609124123307797670/posts/default/3920036514858814986?v=2" /><link rel="self" type="application/atom+xml" href="http://www.blogger.com/feeds/609124123307797670/posts/default/3920036514858814986?v=2" /><link rel="alternate" type="text/html" href="http://feedproxy.google.com/~r/Mineralogy/~3/86XZS9J5Dcw/fire-agate.html" title="Caramel? no, not at all, fire agate, one of many quartz' forms" /><author><name>Oscar Garcia</name><uri>https://plus.google.com/100300946102962552972</uri><email>noreply@blogger.com</email><gd:image rel="http://schemas.google.com/g/2005#thumbnail" width="32" height="32" src="//lh4.googleusercontent.com/-bTyqdIBIO4E/AAAAAAAAAAI/AAAAAAAAAAA/flc2ZUO4-D0/s512-c/photo.jpg" /></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="http://3.bp.blogspot.com/_JwBNq1qsBN0/SammAzR0_LI/AAAAAAAAAHE/4xUZhI3CvTQ/s72-c/fireagate.jpg" height="72" width="72" /><thr:total>0</thr:total><feedburner:origLink>http://ogshelly.blogspot.com/2009/02/fire-agate.html</feedburner:origLink></entry><entry gd:etag="W/&quot;C04EQ3g4fSp7ImA9WxVTGE4.&quot;"><id>tag:blogger.com,1999:blog-609124123307797670.post-1224044956671132660</id><published>2009-01-01T11:43:00.000-06:00</published><updated>2009-01-01T11:45:02.635-06:00</updated><app:edited xmlns:app="http://www.w3.org/2007/app">2009-01-01T11:45:02.635-06:00</app:edited><title>Nominated one of the 100 Best Blogs for Earth Science Scholars</title><content type="html">By: &lt;a href="http://www.bachelorsdegreeonline.com/blog/2008/100-best-blogs-for-earth-science-scholars/" target="100 Best Blogs for Earth Science Scholars"&gt;by Bachelors Degree Online&lt;/a&gt;&lt;br&gt;&lt;br /&gt;Thanks &amp; Happy New Year!&lt;br /&gt;&lt;br /&gt;&lt;a href="http://www.freewebs.com/ogshelly/" target="http://www.freewebs.com/ogshelly/"&gt;Oscar G. Shelly&lt;/a&gt;&lt;img src="http://feeds.feedburner.com/~r/Mineralogy/~4/OnzXO-9w8mE" height="1" width="1"/&gt;</content><link rel="replies" type="application/atom+xml" href="http://ogshelly.blogspot.com/feeds/1224044956671132660/comments/default" title="Post Comments" /><link rel="replies" type="text/html" href="http://www.blogger.com/comment.g?blogID=609124123307797670&amp;postID=1224044956671132660" title="1 Comments" /><link rel="edit" type="application/atom+xml" href="http://www.blogger.com/feeds/609124123307797670/posts/default/1224044956671132660?v=2" /><link rel="self" type="application/atom+xml" href="http://www.blogger.com/feeds/609124123307797670/posts/default/1224044956671132660?v=2" /><link rel="alternate" type="text/html" href="http://feedproxy.google.com/~r/Mineralogy/~3/OnzXO-9w8mE/nominated-one-of-100-best-blogs-for_01.html" title="Nominated one of the 100 Best Blogs for Earth Science Scholars" /><author><name>Oscar Garcia</name><uri>https://plus.google.com/100300946102962552972</uri><email>noreply@blogger.com</email><gd:image rel="http://schemas.google.com/g/2005#thumbnail" width="32" height="32" src="//lh4.googleusercontent.com/-bTyqdIBIO4E/AAAAAAAAAAI/AAAAAAAAAAA/flc2ZUO4-D0/s512-c/photo.jpg" /></author><thr:total>1</thr:total><feedburner:origLink>http://ogshelly.blogspot.com/2009/01/nominated-one-of-100-best-blogs-for_01.html</feedburner:origLink></entry><entry gd:etag="W/&quot;CEcERXwyfCp7ImA9WxVWGEo.&quot;"><id>tag:blogger.com,1999:blog-609124123307797670.post-3009415276416726036</id><published>2009-01-01T11:29:00.009-06:00</published><updated>2009-02-28T19:46:44.294-06:00</updated><app:edited xmlns:app="http://www.w3.org/2007/app">2009-02-28T19:46:44.294-06:00</app:edited><title>Extinct minerals: Brazilianite...due to mineralogists? or Ice....due to global warming?</title><content type="html">Brazilianite &lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://4.bp.blogspot.com/_JwBNq1qsBN0/SV0BmUhD3ZI/AAAAAAAAAGw/hmtIqPNQoA4/s1600-h/0664160001154828723jpg"&gt;&lt;img style="float:right; margin:0 0 10px 10px;cursor:pointer; cursor:hand;width: 320px; height: 263px;" src="http://4.bp.blogspot.com/_JwBNq1qsBN0/SV0BmUhD3ZI/AAAAAAAAAGw/hmtIqPNQoA4/s320/0664160001154828723jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5286383295456861586" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;I read something today (1/1/2009), - Happy New Year by the way - that caught my eye, and it was related to minerals extinction. The article / blog made me wonder if in fact minerals are subject to extinction due to Geological causes, according to &lt;a href="http://geology.about.com/b/" target="http://geology.about.com/b/"&gt;  Andrew's Geology blog&lt;/a&gt;. After serious, and some not so serious thinking, I came up to the following conclusions / examples that I put into consideration for comments / critics. &lt;br /&gt;&lt;br /&gt;I believe that is true that some minerals are subject to extinction, due to a variety of causes / phenomena. The first one that comes to mind is the mineral &lt;strong&gt;ice&lt;/strong&gt;. If after all, Al Gore is right with his Global Warming theory, this will be the cause for melting icebergs, glaciers, and the poles in general, which will make ice disappear from the Earth, or better yet: follow one of Newton's laws; thus, ice will be transformed into water and/or vapor. What about snow?&lt;br /&gt;&lt;br /&gt;Now, another one that comes to mind is the &lt;strong&gt;Brazilianite&lt;/strong&gt;. A beautiful mineral with a beautiful name too in honor of its country in which it was discovered Brazil.  Why does this mineral being so much harder, and stable than ice would disappear from the Earth? well, the disappearance will not be from the Earth, but from the pegmatites of Brazil (at least the ones so far discovered and exploited); Brazilianite specimens have been placed into many Museus and mineralogical collections around the globe, including mine. This is a mineral you don't see anymore in trade shows, so as far as I am concerned, there is another cause for mineral extinction: Avid mineralogists.&lt;br /&gt;&lt;br /&gt;Let me take advantage of discussing about this amazing mineral sadly extinct to talk about its mineralogical features as follows:&lt;br /&gt;&lt;br /&gt;Chemical Formula: NaAl3(PO4)2(OH)4&lt;br /&gt;Composition: Molecular Weight = 361.91 gm&lt;br /&gt;   Sodium       6.35 %  Na    8.56 % Na2O&lt;br /&gt;   Aluminum    22.37 %  Al   42.26 % Al2O3&lt;br /&gt;   Phosphorus  17.12 %  P    39.22 % P2O5&lt;br /&gt;   Hydrogen     1.11 %  H     9.96 % H2O&lt;br /&gt;   Oxygen      53.05 %  O&lt;br /&gt;  &lt;br /&gt;Name Origin: Named after its first discovery in Brazil.&lt;br /&gt;Crystal System: Monoclinic - PrismaticH-M Symbol (2/m) Space Group: P 21/n&lt;br /&gt;Cleavage: [010] Good&lt;br /&gt;Color: Colorless, Greenish yellow, Yellow green, Light yellow.&lt;br /&gt;Density: 2.98&lt;br /&gt;Diaphaniety: Transparent&lt;br /&gt;Fracture: Conchoidal - Fractures developed in brittle materials characterized by smoothly curving surfaces, (e.g. quartz).&lt;br /&gt;Habit: Euhedral Crystals - Occurs as well-formed crystals showing good external form.&lt;br /&gt;Habit: Spherical - Spherical, rounded aggregates.&lt;br /&gt;Hardness: 5.5 - Knife Blade&lt;br /&gt;Luster: Vitreous (Glassy)&lt;br /&gt;Streak: White&lt;br /&gt;Radioactivity: Brazilianite is not Radioactive&lt;img src="http://feeds.feedburner.com/~r/Mineralogy/~4/8_0wKiQWtPg" height="1" width="1"/&gt;</content><link rel="replies" type="application/atom+xml" href="http://ogshelly.blogspot.com/feeds/3009415276416726036/comments/default" title="Post Comments" /><link rel="replies" type="text/html" href="http://www.blogger.com/comment.g?blogID=609124123307797670&amp;postID=3009415276416726036" title="0 Comments" /><link rel="edit" type="application/atom+xml" href="http://www.blogger.com/feeds/609124123307797670/posts/default/3009415276416726036?v=2" /><link rel="self" type="application/atom+xml" href="http://www.blogger.com/feeds/609124123307797670/posts/default/3009415276416726036?v=2" /><link rel="alternate" type="text/html" href="http://feedproxy.google.com/~r/Mineralogy/~3/8_0wKiQWtPg/extinct-minerals-brazilianitethanks-to.html" title="Extinct minerals: Brazilianite...due to mineralogists? or Ice....due to global warming?" /><author><name>Oscar Garcia</name><uri>https://plus.google.com/100300946102962552972</uri><email>noreply@blogger.com</email><gd:image rel="http://schemas.google.com/g/2005#thumbnail" width="32" height="32" src="//lh4.googleusercontent.com/-bTyqdIBIO4E/AAAAAAAAAAI/AAAAAAAAAAA/flc2ZUO4-D0/s512-c/photo.jpg" /></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="http://4.bp.blogspot.com/_JwBNq1qsBN0/SV0BmUhD3ZI/AAAAAAAAAGw/hmtIqPNQoA4/s72-c/0664160001154828723jpg" height="72" width="72" /><thr:total>0</thr:total><feedburner:origLink>http://ogshelly.blogspot.com/2009/01/extinct-minerals-brazilianitethanks-to.html</feedburner:origLink></entry><entry gd:etag="W/&quot;DkYDQnY_eSp7ImA9WxRaEk0.&quot;"><id>tag:blogger.com,1999:blog-609124123307797670.post-4198717727123391685</id><published>2008-12-13T12:03:00.007-06:00</published><updated>2008-12-13T15:36:13.841-06:00</updated><app:edited xmlns:app="http://www.w3.org/2007/app">2008-12-13T15:36:13.841-06:00</app:edited><title>Is snow a mineral? Of quartz! just kidding, it's made out of one mineral: ICE</title><content type="html">&lt;a href="http://1.bp.blogspot.com/_JwBNq1qsBN0/SUP7bj6hN9I/AAAAAAAAAD8/1BycOeGGbQU/s1600-h/x050118b070.jpg"&gt;&lt;img style="float:right; margin:0 0 10px 10px;cursor:pointer; cursor:hand;width: 219px; height: 200px;" src="http://1.bp.blogspot.com/_JwBNq1qsBN0/SUP7bj6hN9I/AAAAAAAAAD8/1BycOeGGbQU/s320/x050118b070.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5279339639124080594" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;I haven't have the opportunity of collecting a snow flake to analyze it under the microscope, or simply with a magnifying glass just to make sure I too believe that snow is made out of ice crystals, and that these are considered just like any other specimen, a true mineral! unbelievable uh? Anyhow, this is the hyperlink to a website in which I saw the latest and most astonishing pictures of snow crytals I've ever seen: &lt;a href="http://www.its.caltech.edu/~atomic/snowcrystals/photos/photos.htm" target="http://www.its.caltech.edu/~atomic/snowcrystals/photos/photos.htm"&gt;Snowflakes&lt;/a&gt;&lt;br&gt;. &lt;br /&gt;&lt;br /&gt;If someone asked me what is that I learned in the subject of mineralogy about ice as a mineral I can still remember that it has basal cleveage, and therfore, that permits the flow of ice in a glaciar. Is it true? does it make sense? I leave this open for discussion.&lt;br /&gt;&lt;br /&gt;Following is the technical data of ice crystals:&lt;br /&gt;&lt;br /&gt;Chemical Formula: H2O  &lt;br /&gt;&lt;br /&gt;Composition:  Molecular Weight = 18.02 gm  &lt;br /&gt;    Hydrogen  11.19 %  H   100.00 % H2O  &lt;br /&gt;    Oxygen    88.81 %  O  &lt;br /&gt;&lt;br /&gt;Environment: Cold weather as snow crystals, coating ponds, glaciers, and icebergs.  &lt;br /&gt;Locality: World wide (I don't think someone has ever seen snow in the Sahara Desert though).  &lt;br /&gt;Name Origin: From the Middle English "is" or "iis", related to the Dutch "ijs" and German "eis".&lt;br /&gt;&lt;br /&gt;Cleavage: None according to many, but it does have basal cleavage &lt;br /&gt;Color: Colorless, Pale blue, Greenish blue, White.  &lt;br /&gt;Density: 0.9167  &lt;br /&gt;Diaphaniety: Transparent  &lt;br /&gt;Fracture: Brittle - Conchoidal - Very brittle fracture producing small, conchoidal fragments.  &lt;br /&gt;Habit: Crystalline - Coarse - Occurs as well-formed coarse sized crystals.  &lt;br /&gt;Habit: Dendritic - Branching "tree-like" growths of great complexity (e.g. pyrolusite).  &lt;br /&gt;Habit: Massive - Granular - Common texture observed in granite and other igneous rock.  &lt;br /&gt;Hardness: 2.5 - Finger Nail  &lt;br /&gt;Streak: White  &lt;br /&gt;Luminescence: Non-fluorescent.  &lt;br /&gt;Luster: Vitreous - Dull&lt;img src="http://feeds.feedburner.com/~r/Mineralogy/~4/nwfoGmcZVKM" height="1" width="1"/&gt;</content><link rel="replies" type="application/atom+xml" href="http://ogshelly.blogspot.com/feeds/4198717727123391685/comments/default" title="Post Comments" /><link rel="replies" type="text/html" href="http://www.blogger.com/comment.g?blogID=609124123307797670&amp;postID=4198717727123391685" title="0 Comments" /><link rel="edit" type="application/atom+xml" href="http://www.blogger.com/feeds/609124123307797670/posts/default/4198717727123391685?v=2" /><link rel="self" type="application/atom+xml" href="http://www.blogger.com/feeds/609124123307797670/posts/default/4198717727123391685?v=2" /><link rel="alternate" type="text/html" href="http://feedproxy.google.com/~r/Mineralogy/~3/nwfoGmcZVKM/is-snow-mineral-of-quartz-just-kidding.html" title="Is snow a mineral? Of quartz! just kidding, it's made out of one mineral: ICE" /><author><name>Oscar Garcia</name><uri>https://plus.google.com/100300946102962552972</uri><email>noreply@blogger.com</email><gd:image rel="http://schemas.google.com/g/2005#thumbnail" width="32" height="32" src="//lh4.googleusercontent.com/-bTyqdIBIO4E/AAAAAAAAAAI/AAAAAAAAAAA/flc2ZUO4-D0/s512-c/photo.jpg" /></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="http://1.bp.blogspot.com/_JwBNq1qsBN0/SUP7bj6hN9I/AAAAAAAAAD8/1BycOeGGbQU/s72-c/x050118b070.jpg" height="72" width="72" /><thr:total>0</thr:total><feedburner:origLink>http://ogshelly.blogspot.com/2008/12/is-snow-mineral-of-quartz-just-kidding.html</feedburner:origLink></entry><entry gd:etag="W/&quot;A0QGSX05fSp7ImA9WxdQEk4.&quot;"><id>tag:blogger.com,1999:blog-609124123307797670.post-5202846984954028899</id><published>2008-06-07T18:34:00.005-05:00</published><updated>2008-06-11T21:55:28.325-05:00</updated><app:edited xmlns:app="http://www.w3.org/2007/app">2008-06-11T21:55:28.325-05:00</app:edited><title>Boleite from El Boleo, Baja California</title><content type="html">&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://bp3.blogger.com/_JwBNq1qsBN0/SEsf1HRG80I/AAAAAAAAADE/hZj2Xu0R-hg/s1600-h/boleite.jpg"&gt;&lt;img style="float:right; margin:0 0 10px 10px;cursor:pointer; cursor:hand;" src="http://bp3.blogger.com/_JwBNq1qsBN0/SEsf1HRG80I/AAAAAAAAADE/hZj2Xu0R-hg/s320/boleite.jpg" border="0" alt=""id="BLOGGER_PHOTO_ID_5209292391328445250" /&gt;&lt;/a&gt;&lt;br /&gt;This mineral takes me back to 1975, when I took Mineralogy with Professor Raul Ortiz Asiain in the faculty of Engineering of the National Autonomous University of Mexico; he used to bring specimens to class fostering our love for minerals, and boosting the learning process of us, the students. Of course not everyone enjoyed the minerals as much as I did for instance.&lt;br /&gt;&lt;br /&gt;I feel lucky I learned so much, and moreover when I was selected professor of the same subject, and I taught it from 1987 until 1989, the year I moved to the USA. Anyhow, I feel it was like a month ago when I saw the first crystal of boleite, its bluish color, its crystallography made a mineral simply unforgettable.&lt;br /&gt;&lt;br /&gt;Below is boleite's technical details:&lt;br /&gt;&lt;br /&gt;Chemical Formula: KPb26Ag9Cu24Cl62(OH)48&lt;br /&gt;Composition: &lt;br /&gt;&lt;br /&gt;Potassium   0.36 %  K      &lt;br /&gt;Copper     13.94 %  Cu    &lt;br /&gt;Silver      8.88 %  Ag     &lt;br /&gt;Hydrogen    0.44 %  H      &lt;br /&gt;Lead       49.26 %  Pb    &lt;br /&gt;Chlorine   20.10 %  Cl    &lt;br /&gt;Oxygen      7.02 %  O&lt;br /&gt;&lt;br /&gt;Environment: Sedimentary copper deposits. The fugitive presence of K in the formula was determined by microprobe.&lt;br /&gt;Locality: Boleo, Baja California, Mexico.  &lt;br /&gt;Name Origin: Named after is locality.&lt;br /&gt;Synonym: Percylite&lt;br /&gt;&lt;br /&gt;Cleavage: [001] Perfect, [101] Good&lt;br /&gt;Color: Indigo blue, Light blue.&lt;br /&gt;Density: 4.8 - 5.1, Average = 4.94&lt;br /&gt;Diaphaniety: Transparent to sub translucent&lt;br /&gt;Fracture: Uneven - Flat surfaces (not cleavage) fractured in an uneven pattern.&lt;br /&gt;Habit: Pseudo Cubic - Crystals show a cubic outline.&lt;br /&gt;Hardness: 3-3.5 - Calcite-Copper Penny&lt;br /&gt;Luster: Vitreous - Pearly&lt;br /&gt;Streak: Light green&lt;br /&gt;Estimated Radioactivity from Boleite: Barely detectable&lt;br /&gt;&lt;br /&gt;I apologize I took a long break, just changed jobs from Dresser-Rand to T3 Energy, in the meantime I was busy, and traveling like a pilot. I am getting a little bit more relaxed, so thank you for your patience.&lt;br /&gt;&lt;br /&gt;I hope you enjoy a terrific weekend, today is 6/7/08, visit my website if you have some chance: &lt;a href="http://www.freewebs.com/ogshelly"&gt;Oscar el Mexicano&lt;/a&gt;&lt;img src="http://feeds.feedburner.com/~r/Mineralogy/~4/I2tnjftvywY" height="1" width="1"/&gt;</content><link rel="replies" type="application/atom+xml" href="http://ogshelly.blogspot.com/feeds/5202846984954028899/comments/default" title="Post Comments" /><link rel="replies" type="text/html" href="http://www.blogger.com/comment.g?blogID=609124123307797670&amp;postID=5202846984954028899" title="0 Comments" /><link rel="edit" type="application/atom+xml" href="http://www.blogger.com/feeds/609124123307797670/posts/default/5202846984954028899?v=2" /><link rel="self" type="application/atom+xml" href="http://www.blogger.com/feeds/609124123307797670/posts/default/5202846984954028899?v=2" /><link rel="alternate" type="text/html" href="http://feedproxy.google.com/~r/Mineralogy/~3/I2tnjftvywY/boleite-from-el-boleo-baja-california.html" title="Boleite from El Boleo, Baja California" /><author><name>Oscar Garcia</name><uri>https://plus.google.com/100300946102962552972</uri><email>noreply@blogger.com</email><gd:image rel="http://schemas.google.com/g/2005#thumbnail" width="32" height="32" src="//lh4.googleusercontent.com/-bTyqdIBIO4E/AAAAAAAAAAI/AAAAAAAAAAA/flc2ZUO4-D0/s512-c/photo.jpg" /></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="http://bp3.blogger.com/_JwBNq1qsBN0/SEsf1HRG80I/AAAAAAAAADE/hZj2Xu0R-hg/s72-c/boleite.jpg" height="72" width="72" /><thr:total>0</thr:total><feedburner:origLink>http://ogshelly.blogspot.com/2008/06/boleite-from-el-boleo-baja-california.html</feedburner:origLink></entry></feed>
