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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: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;DkcEQXY9fip7ImA9WhRaEkk.&quot;"><id>tag:blogger.com,1999:blog-8683684774032524979</id><updated>2012-02-14T16:26:40.866-02:00</updated><category term="http://bp2.blogger.com/_YWldrkTV_x8/SHM4yayoOaI/AAAAAAAAB4I/aafnRdStyNk/s1600-h/LCO_24hr.gif" /><category term="u" /><category term="tsunami" /><category term="terremotos" /><title>Terremotos</title><subtitle type="html" /><link rel="http://schemas.google.com/g/2005#feed" type="application/atom+xml" href="http://tremordeterra.blogspot.com/feeds/posts/default" /><link rel="alternate" type="text/html" href="http://tremordeterra.blogspot.com/" /><link rel="next" type="application/atom+xml" href="http://www.blogger.com/feeds/8683684774032524979/posts/default?start-index=26&amp;max-results=25&amp;redirect=false&amp;v=2" /><author><name>Prof.  George Sand França (Universidade de Brasília)</name><uri>http://www.blogger.com/profile/13658186359698780690</uri><email>noreply@blogger.com</email><gd:image rel="http://schemas.google.com/g/2005#thumbnail" width="32" height="24" src="http://bp0.blogger.com/_YWldrkTV_x8/R_ho6CYm-WI/AAAAAAAABas/e3S7LPid2TU/S220/mar%C3%A7o2008+015.jpg" /></author><generator version="7.00" uri="http://www.blogger.com">Blogger</generator><openSearch:totalResults>948</openSearch:totalResults><openSearch:startIndex>1</openSearch:startIndex><openSearch:itemsPerPage>25</openSearch:itemsPerPage><atom10:link xmlns:atom10="http://www.w3.org/2005/Atom" rel="self" type="application/atom+xml" href="http://feeds.feedburner.com/blogspot/surOo" /><feedburner:info uri="blogspot/suroo" /><atom10:link xmlns:atom10="http://www.w3.org/2005/Atom" rel="hub" href="http://pubsubhubbub.appspot.com/" /><entry gd:etag="W/&quot;DkcEQXY8cCp7ImA9WhRaEkk.&quot;"><id>tag:blogger.com,1999:blog-8683684774032524979.post-2951452512145848438</id><published>2012-02-14T16:26:00.000-02:00</published><updated>2012-02-14T16:26:40.878-02:00</updated><app:edited xmlns:app="http://www.w3.org/2007/app">2012-02-14T16:26:40.878-02:00</app:edited><title>MUST SEE !  2011 earthquakes WORLDWIDE plotted and animated...</title><content type="html">Animação muito boa do Japão!!&lt;br /&gt;&lt;br /&gt;&lt;iframe src="http://www.youtube.com/embed/2a--NC4Nong?fs=1" allowfullscreen="" frameborder="0" height="270" width="480"&gt;&lt;/iframe&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/8683684774032524979-2951452512145848438?l=tremordeterra.blogspot.com' alt='' /&gt;&lt;/div&gt;
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&lt;iframe allowfullscreen="" frameborder="0" height="270" src="http://www.youtube.com/embed/BpoE-mwpPT0?fs=1" width="480"&gt;&lt;/iframe&gt;&lt;br /&gt;
&lt;br /&gt;
Geologists have a new tool to study how earthquakes change the  landscape down to a few inches, and it’s giving them insight into how  earthquake faults behave. In the Feb. 10 issue of the journal Science, a  team of scientists from the U.S., Mexico and China reports the most  comprehensive before-and-after picture yet of an earthquake zone, using  data from the magnitude 7.2 event that struck near Mexicali, northern  Mexico in April 2010.&lt;br /&gt;
“We can learn so much about how earthquakes work by studying fresh  fault ruptures,” said Michael Oskin, geology professor at the University  of California, Davis, and lead author on the paper.&lt;br /&gt;
The team, working with the National Center for Airborne Laser Mapping  (NCALM), flew over the area with LiDAR (light detection and ranging),  which bounces a stream of laser pulses off the ground. New airborne  LiDAR equipment can measure surface features to within a few inches. The  researchers were able to make a detailed scan over about 140 square  miles in less than three days, Oskin said.&lt;br /&gt;
Oskin said that they knew the area had been mapped with LiDAR in 2006  by the Mexican government. When the earthquake occurred, Oskin and  Ramon Arrowsmith at Arizona State University applied for and got funding  from the National Science Foundation to carry out an immediate aerial  survey to compare the results.&lt;br /&gt;
Co-authors John Fletcher and graduate student Orlando Teran from the  Centro de Investigación Científica y de Educación Superior de Ensenada  (CICESE) carried out a traditional ground survey of the fault rupture,  which helped guide planning of the aerial LiDAR survey and the  interpretation of the results.&lt;br /&gt;
From the ground, features like the five-foot escarpment created when  part of a hillside abruptly moved up and sideways are readily visible.  But the LiDAR survey further reveals warping of the ground surface  adjacent to faults that previously could not easily be detected, Oskin  said. For example, it revealed the folding above the Indiviso fault  running beneath agricultural fields in the floodplain of the Colorado  River.&lt;br /&gt;
“This would be very hard to see in the field,” Oskin said.&lt;br /&gt;
Team members used the “virtual reality” facility at UC Davis’ W.M.  Keck Center for Active Visualization in Earth Sciences to handle and  view the data from the survey. By comparing pre- and post-earthquake  surveys, they could see exactly where the ground moved and by how much.&lt;br /&gt;
The survey revealed deformation around the system of small faults  that caused the earthquake, and allowed measurements that provide clues  to understanding how these multifault earthquakes occur.&lt;br /&gt;
The 2010 Mexicali earthquake did not occur on a major fault, like the  San Andreas, but ran through a series of smaller faults in the Earth’s  crust. These minor faults are common around major faults but are  “underappreciated,” Oskin said.&lt;br /&gt;
“This sort of earthquake happens out of the blue,” he said.&lt;br /&gt;
The new LiDAR survey shows how seven of these small faults came together to cause a major earthquake, Oskin said.&lt;br /&gt;
Ken Hudnut, a geophysicist with the U.S. Geological Survey and  co-author on the paper, made the first use of airborne LiDAR about 10  years ago to document surface faulting from the Hector Mine earthquake.  But “pre-earthquake” data were lacking. Since then, NCALM has carried  out LiDAR scans of the San Andreas system (the “B4 Project”) and other  active faults in the western U.S. (a component of the EarthScope  Project), thereby setting a trap for future earthquakes, he said.&lt;br /&gt;
“In this case, fortunately, our CICESE colleagues had set such a  trap, and this earthquake fell right into it and became the first ever  to be imaged by ‘before’ and ‘after’ LiDAR. It is a thrill for me to be  on the team that reached this important milestone," Hudnut said.&lt;br /&gt;
The post-event dataset collected by the team is publicly available through &lt;a href="http://opentopography.org/"&gt;http://opentopography.org/&lt;/a&gt;.&lt;br /&gt;
Other authors on the paper are, at UC Davis: graduate student Austin  Elliott and researcher Peter Gold; J. Ramon Arrowsmith, Arizona State  University; Alejandro Hinojosa Corona and J. Javier Gonzalez Garcia,  CICESE, Mexico; Eric Fielding, NASA Jet Propulsion Laboratory, Pasadena;  and Jing Liu-Zeng, Chinese Academy of Sciences, Beijing. The work was  supported by the National Science Foundation, the U.S. Geological  Survey, Consejo Nacional de Ciencia y Tecnología (Mexico) and NASA.&lt;/div&gt;&lt;h3&gt;About UC Davis&lt;/h3&gt;For more than 100 years, UC Davis has engaged in teaching, research  and public service that matter to California and transform the world.  Located close to the state capital, UC Davis has more than 32,000  students, more than 2,500 faculty and more than 21,000 staff, an annual  research budget that exceeds $684 million, a comprehensive health system  and 13 specialized research centers. The university offers  interdisciplinary graduate study and more than 100 undergraduate majors  in four colleges — Agricultural and Environmental Sciences, Biological  Sciences, Engineering, and Letters and Science. It also houses six  professional schools — Education, Law, Management, Medicine, Veterinary  Medicine and the Betty Irene Moore School of Nursing.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/8683684774032524979-8131403686761607075?l=tremordeterra.blogspot.com' alt='' /&gt;&lt;/div&gt;
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&lt;br /&gt;
A strong earthquake has jolted central Philippine islands, killing at  least 43 people and triggering landslides that left about 40 people  missing.&lt;br /&gt;
&lt;br /&gt;
The Philippine Institute of Volcanology and Seismology  said the quake had a magnitude of 6.9 and was felt at the strongest  intensity of 7.0 on the central island of Negros. The epicentre was located five kilometres northwest of Tayasan town in Negros Oriental province.&lt;br /&gt;
&lt;div class="ad adCentred" id="adspot-300x250-pos-3"&gt;&lt;br /&gt;
&lt;/div&gt;Governor Noel Degamo said at least 13 people were killed  in his province and 40 were missing in the village of Planas in  Guihulngan town, where a landslide occurred. An army commander later  confirmed at least 43 dead.&lt;br /&gt;
&lt;br /&gt;
"The military and police are leading search-and-rescue  operations in the affected areas," Degamo told a Manila radio station.  "At least three main bridges are not passable so we cannot reach some  areas."&lt;br /&gt;
&lt;br /&gt;
Another landslide in the village of Solongon in nearby La  Libertad town buried about 100 houses, said Colonel Francisco Zosimo  Patrimonio.&lt;br /&gt;
He said rescue operations were ongoing and no bodies or  survivors had been found. He warned the death toll would likely climb  because of the landslide. A nine-year-old girl was killed by a collapsed wall  inside her school in Tayasan town, and an 11-year-old girl who was  killed when the wall of a chapel collapsed in Jimalalud town.             &lt;br /&gt;
The quake struck at 11.49am (1449 AEDT) on Monday and was felt in at least seven central provinces, according to the institute.&lt;br /&gt;
&lt;br /&gt;
More than 200 aftershocks were recorded, the strongest of  magnitude of 6.2, the institute said. It had issued a tsunami alert  level 2 immediately after the quake but lifted the warning more than  three hours later.&lt;br /&gt;
&lt;br /&gt;
The Office of Civil Defence said a three-storey building  fell down in La Libertad town, while five cottages in a nearby beach  resort were destroyed by a sudden rise in seawater following the quake. Work in government offices and classes in schools were suspended in Iloilo and Negros Oriental.&lt;br /&gt;
&lt;br /&gt;
The Philippines, located in the so-called Pacific "Ring  of Fire", suffered its worst earthquake in 1990 when a 7.7-magnitude  tremor killed nearly 2000 people on the northern island of Luzon.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/8683684774032524979-6144034583178953151?l=tremordeterra.blogspot.com' alt='' /&gt;&lt;/div&gt;
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&lt;br /&gt;
------------------------------------------------------ &lt;br /&gt;
DA EFE&lt;br /&gt;
Folha on line &lt;br /&gt;
&lt;br /&gt;
Cerca de 10 mil pessoas, entre voluntários, bombeiros, policiais, Guarda  Costeira e até membros da Marinha americana, participaram nesta  sexta-feira de uma grande simulação de terremoto nas principais estações  de metrô de Tóquio.&lt;br /&gt;
&lt;br /&gt;
O treinamento, realizado a pouco mais de um mês do primeiro aniversário  do terremoto e o posterior tsunami que assolou o nordeste do país em  março de 2011, começou às 10h locais (23h de Brasília) e simulou um  terremoto de 7,3 graus na escala Richter. &lt;br /&gt;
No total, 138 empresas participaram da simulação, que teve como objetivo  prioritário a evacuação das pessoas que, diante da suspensão das  comunicações e dos transportes, ficaram presas nas estações de metrô e  em escritórios.&lt;br /&gt;
&lt;br /&gt;
Cada participante recebeu uma bolsa com o material que é utilizado em  casos deste tipo, além de folhetos com um questionário sobre seus dados  pessoais. &lt;br /&gt;
O teste juntou 5 mil voluntários na estação de metrô de Shinjuku, uma  das mais transitadas do mundo, e outras 2,5 mil na estação central de  Tóquio e na de Ikebukuro, segundo informou a organização.&lt;br /&gt;
&lt;br /&gt;
Além disso, se reuniram na baía de Tóquio centenas de pessoas  procedentes das estações de metrô para ser evacuadas pela Guarda  Costeira e a Marinha americana. &lt;br /&gt;
O Japão se encontra sobre o chamado Anel de Fogo do Pacífico, uma zona  de elevada atividade sísmica, e por isso registra terremotos frequentes. &lt;br /&gt;
Desde o grande terremoto de 11 de março, que deixou quase 20 mil mortos e  provocou a pior crise nuclear em 25 anos, o Japão sofreu mais de 660  réplicas de mais de 5 graus na escala Richter. &lt;br /&gt;
&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/8683684774032524979-8128277817935687222?l=tremordeterra.blogspot.com' alt='' /&gt;&lt;/div&gt;
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&lt;a href="http://feedads.g.doubleclick.net/~a/-0xGn4z_Psbh8IbEoTRwZBjyF4s/1/da"&gt;&lt;img src="http://feedads.g.doubleclick.net/~a/-0xGn4z_Psbh8IbEoTRwZBjyF4s/1/di" border="0" ismap="true"&gt;&lt;/img&gt;&lt;/a&gt;&lt;/p&gt;&lt;img src="http://feeds.feedburner.com/~r/blogspot/surOo/~4/QmBx3jhaGfQ" height="1" width="1"/&gt;</content><link rel="replies" type="application/atom+xml" href="http://tremordeterra.blogspot.com/feeds/8128277817935687222/comments/default" title="Postar comentários" /><link rel="replies" type="text/html" href="http://tremordeterra.blogspot.com/2012/02/simulacao-de-terremoto-em-toquio.html#comment-form" title="0 Comentários" /><link rel="edit" type="application/atom+xml" href="http://www.blogger.com/feeds/8683684774032524979/posts/default/8128277817935687222?v=2" /><link rel="self" type="application/atom+xml" href="http://www.blogger.com/feeds/8683684774032524979/posts/default/8128277817935687222?v=2" /><link rel="alternate" type="text/html" href="http://feedproxy.google.com/~r/blogspot/surOo/~3/QmBx3jhaGfQ/simulacao-de-terremoto-em-toquio.html" title="Simulação de terremoto em Tóquio envolve 10 mil pessoas." /><author><name>Prof.  George Sand França (Universidade de Brasília)</name><uri>http://www.blogger.com/profile/13658186359698780690</uri><email>noreply@blogger.com</email><gd:image rel="http://schemas.google.com/g/2005#thumbnail" width="32" height="24" src="http://bp0.blogger.com/_YWldrkTV_x8/R_ho6CYm-WI/AAAAAAAABas/e3S7LPid2TU/S220/mar%C3%A7o2008+015.jpg" /></author><thr:total>0</thr:total><feedburner:origLink>http://tremordeterra.blogspot.com/2012/02/simulacao-de-terremoto-em-toquio.html</feedburner:origLink></entry><entry gd:etag="W/&quot;DE4HR3w7eip7ImA9WhRVGUo.&quot;"><id>tag:blogger.com,1999:blog-8683684774032524979.post-3565235041373210062</id><published>2012-01-19T10:41:00.001-02:00</published><updated>2012-01-19T10:42:16.202-02:00</updated><app:edited xmlns:app="http://www.w3.org/2007/app">2012-01-19T10:42:16.202-02:00</app:edited><title>Oportunidade 2 - VLB Engenharia busca Projetista/Desenhista (Belo Horizonte)</title><content type="html">&lt;span style="font-family: &amp;quot;Tahoma&amp;quot;,&amp;quot;sans-serif&amp;quot;;"&gt;&amp;nbsp;&lt;/span&gt; &lt;span style="font-family: &amp;quot;Tahoma&amp;quot;,&amp;quot;sans-serif&amp;quot;;"&gt;A VLB Engenharia busca &lt;b&gt;Projetista/Desenhista&lt;/b&gt; para compor sua equipe de geotecnia em Belo Horizonte.&lt;/span&gt; &lt;br /&gt;
&lt;div class="MsoNormal"&gt;&lt;br /&gt;
&lt;/div&gt;&lt;div class="MsoNormal"&gt;&lt;span style="font-family: &amp;quot;Tahoma&amp;quot;,&amp;quot;sans-serif&amp;quot;;"&gt;O mesmo irá atuar com projetos civis geotécnicos voltados a hidrelétricas.&lt;/span&gt;&lt;/div&gt;&lt;div class="MsoNormal"&gt;&lt;span style="font-family: &amp;quot;Tahoma&amp;quot;,&amp;quot;sans-serif&amp;quot;;"&gt;Sendo as principais atividades: Elaboração de desenhos de perfis de escavação, topografia e taludes.&lt;/span&gt;&lt;/div&gt;&lt;div class="MsoNormal"&gt;&lt;br /&gt;
&lt;/div&gt;&lt;div class="MsoNormal"&gt;&lt;span style="font-family: &amp;quot;Tahoma&amp;quot;,&amp;quot;sans-serif&amp;quot;;"&gt;Necessário experiência na área ou em projetos geotécnicos aplicados a mineração ou estradas.&lt;/span&gt;&lt;/div&gt;&lt;div class="MsoNormal"&gt;&lt;br /&gt;
&lt;/div&gt;&lt;div class="MsoNormal"&gt;&lt;span style="font-family: &amp;quot;Tahoma&amp;quot;,&amp;quot;sans-serif&amp;quot;;"&gt;Salário a combinar.&lt;/span&gt;&lt;/div&gt;&lt;div class="MsoNormal"&gt;&lt;br /&gt;
&lt;/div&gt;&lt;div class="MsoNormal"&gt;&lt;span style="font-family: &amp;quot;Tahoma&amp;quot;,&amp;quot;sans-serif&amp;quot;;"&gt;Interessados deverão encaminhar currículo para: &lt;a href="http://www.blogger.com/post-edit.g?blogID=8683684774032524979&amp;amp;postID=3565235041373210062"&gt;glaucia.mesquita@vlb.com.br&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div class="MsoNormal"&gt;&lt;br /&gt;
&lt;/div&gt;&lt;br /&gt;
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&lt;a href="http://feedads.g.doubleclick.net/~a/IISuL_lGPgBhRodcf2d2F9lJL8M/1/da"&gt;&lt;img src="http://feedads.g.doubleclick.net/~a/IISuL_lGPgBhRodcf2d2F9lJL8M/1/di" border="0" ismap="true"&gt;&lt;/img&gt;&lt;/a&gt;&lt;/p&gt;&lt;img src="http://feeds.feedburner.com/~r/blogspot/surOo/~4/qdUm4IUOyVo" height="1" width="1"/&gt;</content><link rel="replies" type="application/atom+xml" href="http://tremordeterra.blogspot.com/feeds/3565235041373210062/comments/default" title="Postar comentários" /><link rel="replies" type="text/html" href="http://tremordeterra.blogspot.com/2012/01/oportunidade-2-vlb-engenharia-busca.html#comment-form" title="0 Comentários" /><link rel="edit" type="application/atom+xml" href="http://www.blogger.com/feeds/8683684774032524979/posts/default/3565235041373210062?v=2" /><link rel="self" type="application/atom+xml" href="http://www.blogger.com/feeds/8683684774032524979/posts/default/3565235041373210062?v=2" /><link rel="alternate" type="text/html" href="http://feedproxy.google.com/~r/blogspot/surOo/~3/qdUm4IUOyVo/oportunidade-2-vlb-engenharia-busca.html" title="Oportunidade 2 - VLB Engenharia busca Projetista/Desenhista (Belo Horizonte)" /><author><name>Prof.  George Sand França (Universidade de Brasília)</name><uri>http://www.blogger.com/profile/13658186359698780690</uri><email>noreply@blogger.com</email><gd:image rel="http://schemas.google.com/g/2005#thumbnail" width="32" height="24" src="http://bp0.blogger.com/_YWldrkTV_x8/R_ho6CYm-WI/AAAAAAAABas/e3S7LPid2TU/S220/mar%C3%A7o2008+015.jpg" /></author><thr:total>0</thr:total><feedburner:origLink>http://tremordeterra.blogspot.com/2012/01/oportunidade-2-vlb-engenharia-busca.html</feedburner:origLink></entry><entry gd:etag="W/&quot;DkYEQHc_fip7ImA9WhRVGUw.&quot;"><id>tag:blogger.com,1999:blog-8683684774032524979.post-3270406071120256402</id><published>2012-01-18T17:15:00.000-02:00</published><updated>2012-01-18T17:15:01.946-02:00</updated><app:edited xmlns:app="http://www.w3.org/2007/app">2012-01-18T17:15:01.946-02:00</app:edited><title>Oportunidade!!!</title><content type="html">&lt;table border="0" cellpadding="2" cellspacing="0"&gt;&lt;tbody&gt;
&lt;tr&gt;&lt;td colspan="2" height="10"&gt;&lt;span style="color: #993300; font-family: Verdana,Arial,Helvetica,sans-serif; font-size: x-small;"&gt;&lt;b&gt;UFBA abre concurso para professor&lt;/b&gt;&lt;/span&gt;                  &lt;/td&gt;               &lt;/tr&gt;
&lt;tr&gt;                  &lt;td height="13" width="64%"&gt;fonte:Jornal da Ciência&lt;/td&gt;&lt;td height="13" width="64%"&gt;&lt;br /&gt;
&lt;/td&gt;&lt;td height="13" width="64%"&gt;&lt;br /&gt;
&lt;/td&gt;&lt;td height="13" width="64%"&gt;&lt;br /&gt;
&lt;/td&gt;&lt;td height="13" width="64%"&gt;&lt;br /&gt;
&lt;/td&gt;&lt;td height="13" width="64%"&gt;&lt;br /&gt;
&lt;/td&gt;                 &lt;td height="13" width="36%"&gt;&lt;/td&gt;               &lt;/tr&gt;
&lt;tr&gt;                  &lt;td colspan="2"&gt;&lt;span style="font-family: Verdana,Arial,Helvetica,sans-serif; font-size: x-small;"&gt;&lt;br /&gt;
&lt;br /&gt;
Inscrições para professor auxiliar, assistente e adjunto estão abertas até o dia 27 de janeiro.&lt;br /&gt;
&lt;br /&gt;
O Instituto de Física da Universidade Federal da  Bahia (UFBA), em Salvador, realiza dois concursos para professores na  área de geofísica. As áreas de conhecimento são: Física da Terra Sólida e  Gravimetria. Estão disponíveis uma vaga para cada área e o candidato  deve ter graduação em Física, doutorado em Física, Geofísica ou áreas  afins.&lt;br /&gt;
&lt;br /&gt;
As inscrições estão abertas até o dia 27 de janeiro. A  seleção terá prova teórico-prática, prova didática, avaliação de títulos  e defesa de Memorial. As datas das provas serão divulgadas a partir de 9  de fevereiro.&lt;br /&gt;
&lt;br /&gt;
Mais detalhes no edital disponível no link &lt;a href="http://www.concursos.ufba.br/docentes/2011/editais/edital_docente_062011.pdf" target="_blank"&gt;http://www.concursos.ufba.br/docentes/2011/editais/edital_docente_062011.pdf&lt;/a&gt;.&lt;/span&gt;&lt;/td&gt;&lt;/tr&gt;
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&lt;a href="http://feedads.g.doubleclick.net/~a/9YQ6wvGRRYY7MinSrmuFYUjeGTU/1/da"&gt;&lt;img src="http://feedads.g.doubleclick.net/~a/9YQ6wvGRRYY7MinSrmuFYUjeGTU/1/di" border="0" ismap="true"&gt;&lt;/img&gt;&lt;/a&gt;&lt;/p&gt;&lt;img src="http://feeds.feedburner.com/~r/blogspot/surOo/~4/KpOmMEXVnzg" height="1" width="1"/&gt;</content><link rel="replies" type="application/atom+xml" href="http://tremordeterra.blogspot.com/feeds/3270406071120256402/comments/default" title="Postar comentários" /><link rel="replies" type="text/html" href="http://tremordeterra.blogspot.com/2012/01/oportunidade.html#comment-form" title="0 Comentários" /><link rel="edit" type="application/atom+xml" href="http://www.blogger.com/feeds/8683684774032524979/posts/default/3270406071120256402?v=2" /><link rel="self" type="application/atom+xml" href="http://www.blogger.com/feeds/8683684774032524979/posts/default/3270406071120256402?v=2" /><link rel="alternate" type="text/html" href="http://feedproxy.google.com/~r/blogspot/surOo/~3/KpOmMEXVnzg/oportunidade.html" title="Oportunidade!!!" /><author><name>Prof.  George Sand França (Universidade de Brasília)</name><uri>http://www.blogger.com/profile/13658186359698780690</uri><email>noreply@blogger.com</email><gd:image rel="http://schemas.google.com/g/2005#thumbnail" width="32" height="24" src="http://bp0.blogger.com/_YWldrkTV_x8/R_ho6CYm-WI/AAAAAAAABas/e3S7LPid2TU/S220/mar%C3%A7o2008+015.jpg" /></author><thr:total>0</thr:total><feedburner:origLink>http://tremordeterra.blogspot.com/2012/01/oportunidade.html</feedburner:origLink></entry><entry gd:etag="W/&quot;D0MGQ3szeCp7ImA9WhRWFEw.&quot;"><id>tag:blogger.com,1999:blog-8683684774032524979.post-1811063285966140943</id><published>2012-01-01T08:57:00.000-02:00</published><updated>2012-01-01T08:57:02.580-02:00</updated><app:edited xmlns:app="http://www.w3.org/2007/app">2012-01-01T08:57:02.580-02:00</app:edited><title>200th Anniversary of New Madrid Earthquakes</title><content type="html">Fonte:USGS&lt;br /&gt;
&lt;br /&gt;
Posted on December 16, 2011 at 5:24 pm&amp;nbsp;By Melanie Gade and Heidi Koontz                                                                                                           &lt;br /&gt;
&lt;div class="sf_page_shadowsInset" id="sf_single_media"&gt;                                                                                          &lt;div id="usgs_media_corecasts"&gt;                                 &lt;h3&gt;USGS CoreCast&lt;/h3&gt;&lt;div class="usgs_corecast"&gt;&lt;h4&gt;New Madrid Earthquakes Bicentennial&lt;/h4&gt;&lt;a href="http://gallery.usgs.gov/audios/398"&gt; Transcipt and Details &lt;/a&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;a href="http://www.usgs.gov/blogs/features/files/2011/12/NewMadrid620x350.jpg"&gt;&lt;img alt="Map showing distribution of earthquakes in the New Madrid sequence" class="size-full wp-image-173021 alignleft" height="224" src="http://www.usgs.gov/blogs/features/files/2011/12/NewMadrid620x350.jpg" width="397" /&gt;&lt;/a&gt;&lt;br /&gt;
Two  hundred years ago today, the central Mississippi River Valley was  violently shaken by the first of a series of three earthquakes of  magnitude 7 – 8 and hundreds of aftershocks greater than magnitude 3. By  March 15, 1812, an estimated 2,000 aftershocks had been felt, but it is  likely there were tens of thousands more that were not felt or  otherwise noted.&lt;br /&gt;
&lt;br /&gt;
The first of these quakes struck on December 16 around 2:15 a.m.,  near present-day Blytheville, Arkansas, waking residents located up to  900 miles away across what is now the eastern United States. According  to reports of boat captains and others on the Mississippi River, the  December 16 quake and its aftershocks caused the river to fill with  debris as tree-covered banks caved into the river. Other reports said  the river flooded large tracks of land, created temporary waterfalls,  and even ran backwards in some places.&lt;br /&gt;
&lt;br /&gt;
&lt;div class="wp-caption alignright" id="attachment_173018" style="width: 310px;"&gt;&lt;div style="text-align: center;"&gt;&lt;a href="http://www.youtube.com/user/NewMadrid2011#p/u/10/0fACj3206uQ" target="_blank"&gt;&lt;img alt="Video: Marion Haynes discusses the historic evidence of earthquakes" class="size-medium wp-image-173018   " height="165" src="http://www.usgs.gov/blogs/features/files/2011/12/Marion-Haynes-Video-300x165.jpg" width="300" /&gt;&amp;nbsp;&lt;/a&gt; &lt;/div&gt;&lt;div class="wp-caption-text"&gt;Video: Marion Haynes discusses the historic evidence of earthquakes&lt;/div&gt;&lt;div class="wp-caption-text"&gt;&lt;br /&gt;
&lt;/div&gt;&lt;/div&gt;&lt;strong&gt;&lt;/strong&gt;The second of the three major earthquakes, estimated  at magnitude 7.5, occurred on January 23, 1812, at about 9:15 a.m.  Similar to the December 1811 earthquake, this event was also widely  felt. Damage occurred in an area of about 232,000 square miles.&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
&lt;strong&gt;&lt;/strong&gt;&lt;br /&gt;
The third and probably the most widely felt of the three major earthquakes occurred on February &lt;strong&gt;7, &lt;/strong&gt;1812,  at about 3 a.m. There were several destructive shocks that day, the  last and largest estimated at magnitude 7.7. As a result, the town of  New Madrid, Missouri, was severely damaged.&lt;br /&gt;
&lt;br /&gt;
&lt;strong&gt;The New Madrid Quakes Not a One-Time Event&lt;/strong&gt;&lt;br /&gt;
We know the 1811 – 1812 earthquake sequence was not a one-time event.  The New Madrid earthquakes covered the region with sand blows,  thousands of which remain today and can be seen as large, light-colored  sandy patches in agricultural fields.&lt;br /&gt;
By digging into the sand blows, geologists found widespread evidence  of pre-historic sand blows telling of similar sequences of earthquakes  around 1450, 900, and 300 A.D. The USGS earthquake hazard map (&lt;a href="http://earthquake.usgs.gov/hazards/"&gt;http://earthquake.usgs.gov/hazards/&lt;/a&gt;),  which is a compilation of scientific studies over the past 40 years,  demonstrates the earthquake hazard revealed by this earthquake history.&lt;br /&gt;
&lt;div class="wp-caption alignright" id="attachment_173019" style="width: 310px;"&gt;&lt;a href="http://www.youtube.com/user/NewMadrid2011#p/u/16/sL1hs-MM4ec" target="_blank"&gt;&lt;img alt="Video: Tish Tuttle discusses the New Madrid Earthquakes" class="size-medium wp-image-173019  " height="163" src="http://www.usgs.gov/blogs/features/files/2011/12/Tish-Tuttle-video-300x163.jpg" width="300" /&gt;&lt;/a&gt;&lt;div class="wp-caption-text"&gt;Video: Tish Tuttle discusses the New Madrid Earthquakes&lt;/div&gt;&lt;div class="wp-caption-text"&gt;&lt;br /&gt;
&lt;/div&gt;&lt;/div&gt;&lt;strong&gt;Similar Risk Exists Today&lt;/strong&gt;&lt;br /&gt;
A risk of a similar sequence of earthquakes exists in the New Madrid  Seismic Zone today and threatens Alabama, Arkansas, Illinois, Indiana,  Kentucky, Mississippi, Missouri, and Tennessee. Recent USGS projections  place the likelihood of a magnitude-6 or higher earthquake at about 25 –  50 percent over the next few decades and place the likelihood of a  magnitude 7 or higher earthquake at 10 percent.&lt;br /&gt;
With large cities like Memphis, St. Louis, and Nashville well within  range of a large-scale New Madrid earthquake, understanding the science  of earthquakes and the area’s geologic history helps communities prepare  for earthquake hazards and prevent them from becoming catastrophes.&lt;br /&gt;
&lt;strong&gt;Are You Prepared?&lt;/strong&gt;&lt;br /&gt;
The USGS encourages citizens to join the thousands in eight States  who have signed up to participate in the February 7, 2012, Great Central  U.S. ShakeOut drill. The 200&lt;sup&gt;th&lt;/sup&gt; anniversary of the New Madrid  earthquakes is an opportune time to consider earthquake preparedness  and learn about the region’s earthquake history. Go to the &lt;a href="http://www.shakeout.org/centralus/"&gt;ShakeOut website&lt;/a&gt; to sign up for the drill, learn preparedness tips, and learn how to “Drop, Cover and Hold On” during an earthquake.&lt;br /&gt;
A newly released handbook from the USGS can help people in the central United States to prepare for earthquakess. “&lt;a href="http://pubs.usgs.gov/gip/119/"&gt;Putting Down Roots in Earthquake Country – Your Handbook for Earthquakes in the Central United States&lt;/a&gt;”  provides detailed information about the threat of earthquakes in this  part of the country, particularly along the New Madrid and Wabash Valley  seismic zones.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/8683684774032524979-1811063285966140943?l=tremordeterra.blogspot.com' alt='' /&gt;&lt;/div&gt;
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&lt;a href="http://feedads.g.doubleclick.net/~a/lRmROWfDWMt-AaDGgnzTRgVP5tc/1/da"&gt;&lt;img src="http://feedads.g.doubleclick.net/~a/lRmROWfDWMt-AaDGgnzTRgVP5tc/1/di" border="0" ismap="true"&gt;&lt;/img&gt;&lt;/a&gt;&lt;/p&gt;&lt;img src="http://feeds.feedburner.com/~r/blogspot/surOo/~4/isdCURdvOlw" height="1" width="1"/&gt;</content><link rel="replies" type="application/atom+xml" href="http://tremordeterra.blogspot.com/feeds/1811063285966140943/comments/default" title="Postar comentários" /><link rel="replies" type="text/html" href="http://tremordeterra.blogspot.com/2012/01/200th-anniversary-of-new-madrid.html#comment-form" title="0 Comentários" /><link rel="edit" type="application/atom+xml" href="http://www.blogger.com/feeds/8683684774032524979/posts/default/1811063285966140943?v=2" /><link rel="self" type="application/atom+xml" href="http://www.blogger.com/feeds/8683684774032524979/posts/default/1811063285966140943?v=2" /><link rel="alternate" type="text/html" href="http://feedproxy.google.com/~r/blogspot/surOo/~3/isdCURdvOlw/200th-anniversary-of-new-madrid.html" title="200th Anniversary of New Madrid Earthquakes" /><author><name>Prof.  George Sand França (Universidade de Brasília)</name><uri>http://www.blogger.com/profile/13658186359698780690</uri><email>noreply@blogger.com</email><gd:image rel="http://schemas.google.com/g/2005#thumbnail" width="32" height="24" src="http://bp0.blogger.com/_YWldrkTV_x8/R_ho6CYm-WI/AAAAAAAABas/e3S7LPid2TU/S220/mar%C3%A7o2008+015.jpg" /></author><thr:total>0</thr:total><feedburner:origLink>http://tremordeterra.blogspot.com/2012/01/200th-anniversary-of-new-madrid.html</feedburner:origLink></entry><entry gd:etag="W/&quot;A0AHSXg_eyp7ImA9WhRWE0k.&quot;"><id>tag:blogger.com,1999:blog-8683684774032524979.post-4558128904624111399</id><published>2011-12-31T14:39:00.003-02:00</published><updated>2011-12-31T14:42:18.643-02:00</updated><app:edited xmlns:app="http://www.w3.org/2007/app">2011-12-31T14:42:18.643-02:00</app:edited><title>Tremor na Argentina, com probabilidade de ser sentido em São Paulo.</title><content type="html">&lt;span style="font-size: large;"&gt;&lt;b&gt;5.3 Mb -  SALTA, ARGENTINA&lt;/b&gt;&lt;/span&gt;&lt;br /&gt;
&lt;br /&gt;
&lt;table cellpadding="2" cellspacing="1"&gt;&lt;thead&gt;   &lt;/thead&gt;&lt;caption&gt;fonte:USGS&lt;/caption&gt;    &lt;tbody&gt;
&lt;tr&gt;    &lt;td valign="top"&gt;&lt;a href="http://earthquake.usgs.gov/eqcenter/glossary.php#magnitude" target="_blank"&gt;Magnitude&lt;/a&gt;&lt;/td&gt;    &lt;td&gt;5.3 Mb&lt;/td&gt;   &lt;/tr&gt;
&lt;tr&gt;    &lt;td valign="top"&gt;&lt;a href="http://earthquake.usgs.gov/eqcenter/glossary.php#date" target="_blank"&gt;Date-Time&lt;/a&gt;&lt;/td&gt;    &lt;td&gt;&lt;ul&gt;&lt;li&gt;31 Dec 2011  16:15:10 UTC&lt;/li&gt;
&lt;li&gt;31 Dec 2011  13:15:10 near epicenter&lt;/li&gt;
&lt;li&gt;31 Dec 2011  16:15:10 standard time in your timezone&lt;/li&gt;
&lt;/ul&gt;&lt;/td&gt;   &lt;/tr&gt;
&lt;tr&gt;    &lt;td valign="top"&gt;&lt;a href="http://earthquake.usgs.gov/eqcenter/glossary.php#location" target="_blank"&gt;Location&lt;/a&gt;&lt;/td&gt;    &lt;td&gt;23.271S  64.272W&lt;/td&gt;   &lt;/tr&gt;
&lt;tr&gt;    &lt;td valign="top"&gt;&lt;a href="http://earthquake.usgs.gov/eqcenter/glossary.php#depth" target="_blank"&gt;Depth&lt;/a&gt;&lt;/td&gt;    &lt;td&gt;22 km&lt;/td&gt;   &lt;/tr&gt;
&lt;tr&gt;    &lt;td valign="top"&gt;&lt;a href="http://earthquake.usgs.gov/eqcenter/glossary.php#distances" target="_blank"&gt;Distances&lt;/a&gt;&lt;/td&gt;    &lt;td&gt;&lt;ul&gt;&lt;li&gt; 185 km (115 miles) ENE (58 degrees) of San Salvador de Jujuy, Argentina&lt;/li&gt;
&lt;li&gt; 198 km (123 miles) SSE (166 degrees) of Tarija, Bolivia&lt;/li&gt;
&lt;li&gt; 206 km (128 miles) NE (36 degrees) of Salta, Argentina&lt;/li&gt;
&lt;/ul&gt;&lt;/td&gt;&lt;/tr&gt;
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&lt;a href="http://feedads.g.doubleclick.net/~a/nzH8vWx9eLJoz0Cyqbgr8W-FeCU/1/da"&gt;&lt;img src="http://feedads.g.doubleclick.net/~a/nzH8vWx9eLJoz0Cyqbgr8W-FeCU/1/di" border="0" ismap="true"&gt;&lt;/img&gt;&lt;/a&gt;&lt;/p&gt;&lt;img src="http://feeds.feedburner.com/~r/blogspot/surOo/~4/NFgrQ_lLTBo" height="1" width="1"/&gt;</content><link rel="replies" type="application/atom+xml" href="http://tremordeterra.blogspot.com/feeds/4558128904624111399/comments/default" title="Postar comentários" /><link rel="replies" type="text/html" href="http://tremordeterra.blogspot.com/2011/12/tremor-na-argentina-com-probabilidade.html#comment-form" title="0 Comentários" /><link rel="edit" type="application/atom+xml" href="http://www.blogger.com/feeds/8683684774032524979/posts/default/4558128904624111399?v=2" /><link rel="self" type="application/atom+xml" href="http://www.blogger.com/feeds/8683684774032524979/posts/default/4558128904624111399?v=2" /><link rel="alternate" type="text/html" href="http://feedproxy.google.com/~r/blogspot/surOo/~3/NFgrQ_lLTBo/tremor-na-argentina-com-probabilidade.html" title="Tremor na Argentina, com probabilidade de ser sentido em São Paulo." /><author><name>Prof.  George Sand França (Universidade de Brasília)</name><uri>http://www.blogger.com/profile/13658186359698780690</uri><email>noreply@blogger.com</email><gd:image rel="http://schemas.google.com/g/2005#thumbnail" width="32" height="24" src="http://bp0.blogger.com/_YWldrkTV_x8/R_ho6CYm-WI/AAAAAAAABas/e3S7LPid2TU/S220/mar%C3%A7o2008+015.jpg" /></author><thr:total>0</thr:total><feedburner:origLink>http://tremordeterra.blogspot.com/2011/12/tremor-na-argentina-com-probabilidade.html</feedburner:origLink></entry><entry gd:etag="W/&quot;AkIEQnc5eyp7ImA9WhRWEks.&quot;"><id>tag:blogger.com,1999:blog-8683684774032524979.post-4315376083000881545</id><published>2011-12-30T16:08:00.000-02:00</published><updated>2011-12-30T16:08:23.923-02:00</updated><app:edited xmlns:app="http://www.w3.org/2007/app">2011-12-30T16:08:23.923-02:00</app:edited><title>2012 sem Terremotos para todos! É impossível!</title><content type="html">É impossível, mas pelo menos sem desastres!&lt;br /&gt;
&amp;nbsp;Agora vamos colorir! Feliz 2012!!&lt;br /&gt;
&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://1.bp.blogspot.com/-lgmvBWB4_Xk/Tv398C9tSMI/AAAAAAAAGqo/fDFNr4NQ69I/s1600/terremoto.gif" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"&gt;&lt;img border="0" height="640" src="http://1.bp.blogspot.com/-lgmvBWB4_Xk/Tv398C9tSMI/AAAAAAAAGqo/fDFNr4NQ69I/s640/terremoto.gif" width="432" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/8683684774032524979-4315376083000881545?l=tremordeterra.blogspot.com' alt='' /&gt;&lt;/div&gt;
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&lt;/span&gt;&lt;/span&gt;&lt;span class="Apple-style-span" style="font-family: arial, helvetica, clean, sans-serif; font-size: 11px; line-height: 16px;"&gt;&lt;span style="background-attachment: initial; background-clip: initial; background-color: initial; background-image: none; background-origin: initial; background-position: -3px -81px; background-repeat: no-repeat no-repeat; color: #0f4d8b; display: inline !important; height: 18px; padding-bottom: 2px; padding-left: 18px; padding-right: 3px; padding-top: 4px; text-decoration: none;"&gt;&lt;span class="Apple-style-span" style="color: black; font-family: Georgia, Times, 'Times New Roman', serif; font-size: 14px; line-height: 22px;"&gt;&lt;a class="ymsb-print-btn" href="http://br.noticias.yahoo.com/terremoto-arrasou-jap%C3%A3o-mar%C3%A7o-foi-sentido-sat%C3%A9lites-%C3%B3rbita-150402991.html" role="button" style="background-attachment: initial; background-clip: initial; background-color: initial; background-image: url(http://l.yimg.com/a/i/us/mit/widgets/sprite_soc_btn.png); background-origin: initial; background-position: -3px -81px; background-repeat: no-repeat no-repeat; color: #0f4d8b; display: inline !important; height: 18px; text-decoration: none;" title="Imprimir"&gt;A destruição não ocorreu apenas no Japão&lt;/a&gt;&amp;nbsp; Fonte: yahoo.com.br&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/cite&gt;&lt;/div&gt;&lt;/div&gt;&lt;div class="yog-wrap yom-art-bd" id="yui_3_3_0_5_1323934395593212" style="border-top-color: initial; border-top-style: none; border-top-width: initial; font-family: arial, helvetica, clean, sans-serif; font-size: 13px; line-height: 16px; margin-bottom: 20px; margin-left: 0px; margin-right: -10px; margin-top: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; zoom: 1;"&gt;&lt;div class="yog-col yog-11u" id="yui_3_3_0_5_1323934395593211" style="float: none; margin-bottom: 0px; margin-left: 0px; margin-right: 10px; margin-top: 0px; overflow-x: visible; overflow-y: visible; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; width: auto;"&gt;&lt;div class="yom-mod yom-art-content " style="border-bottom-color: rgb(52, 78, 127); border-left-color: rgb(52, 78, 127); border-right-color: rgb(52, 78, 127); border-top-color: rgb(52, 78, 127); border-top-style: none; border-top-width: initial; margin-bottom: 5px; margin-left: 0px; margin-right: 0px; margin-top: 0px; padding-bottom: 20px; padding-left: 0px; padding-right: 0px; padding-top: 0px; zoom: 0;"&gt;&lt;div class="bd" style="font-family: Georgia, Times, 'Times New Roman', serif; font-size: 14px; line-height: 1.6em; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; zoom: 0;"&gt;&lt;div style="margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 11px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px;"&gt;Por Guilherme Abati&lt;/div&gt;&lt;div style="margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 11px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px;"&gt;O terremoto que matou milhares de japoneses em março dessa ano não gerou destruição apenas no Japão. Satélites que orbitavam o planeta também foram afetados pela força destruidora do terremoto.&lt;/div&gt;&lt;div style="margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 11px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px;"&gt;A força dele foi tanta que o choque foi sentido por dois satélites, os quais tiveram suas trajetórias e sensores alterados. A informação somente foi divulgada agora, quase nove meses depois da ocorrência da tragédia.&lt;/div&gt;&lt;div style="margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 11px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px;"&gt;Satélites também sofreram com o terremoto em março (Dvice)&lt;/div&gt;&lt;div style="margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 11px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px;"&gt;Os dois satélites mensuravam o campo magnético terrestre e faziam parte do projeto chamado GRACE (Gravity Recovery and Climate Experiment), cujos responsáveis são os Estados Unidos e a Alemanha. O terremoto fez com que as leituras dos satélites fossem completamente alteradas, prejudicando o trabalho, segundo o Dvice.&lt;/div&gt;&lt;div style="margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 11px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px;"&gt;De acordo com o New Scientist, a NASA e a DLR, agência espacial alemã, acreditam que o incidente pode ajudar os cientistas a medir de forma mais apurada a magnitude de terremotos.&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/8683684774032524979-6511236158038573961?l=tremordeterra.blogspot.com' alt='' /&gt;&lt;/div&gt;
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&lt;a href="http://feedads.g.doubleclick.net/~a/3MiLa8N3EybzDn8VsS-wCCgo9GA/1/da"&gt;&lt;img src="http://feedads.g.doubleclick.net/~a/3MiLa8N3EybzDn8VsS-wCCgo9GA/1/di" border="0" ismap="true"&gt;&lt;/img&gt;&lt;/a&gt;&lt;/p&gt;&lt;img src="http://feeds.feedburner.com/~r/blogspot/surOo/~4/SMqajk-MmNk" height="1" width="1"/&gt;</content><link rel="replies" type="application/atom+xml" href="http://tremordeterra.blogspot.com/feeds/6511236158038573961/comments/default" title="Postar comentários" /><link rel="replies" type="text/html" href="http://tremordeterra.blogspot.com/2011/12/terremoto-que-arrasou-japao-em-marco.html#comment-form" title="0 Comentários" /><link rel="edit" type="application/atom+xml" href="http://www.blogger.com/feeds/8683684774032524979/posts/default/6511236158038573961?v=2" /><link rel="self" type="application/atom+xml" href="http://www.blogger.com/feeds/8683684774032524979/posts/default/6511236158038573961?v=2" /><link rel="alternate" type="text/html" href="http://feedproxy.google.com/~r/blogspot/surOo/~3/SMqajk-MmNk/terremoto-que-arrasou-japao-em-marco.html" title="Terremoto que arrasou Japão em março foi sentido por satélites na órbita terrestre" /><author><name>Prof.  George Sand França (Universidade de Brasília)</name><uri>http://www.blogger.com/profile/13658186359698780690</uri><email>noreply@blogger.com</email><gd:image rel="http://schemas.google.com/g/2005#thumbnail" width="32" height="24" src="http://bp0.blogger.com/_YWldrkTV_x8/R_ho6CYm-WI/AAAAAAAABas/e3S7LPid2TU/S220/mar%C3%A7o2008+015.jpg" /></author><thr:total>0</thr:total><feedburner:origLink>http://tremordeterra.blogspot.com/2011/12/terremoto-que-arrasou-japao-em-marco.html</feedburner:origLink></entry><entry gd:etag="W/&quot;DkUGQXcyfyp7ImA9WhRQGU4.&quot;"><id>tag:blogger.com,1999:blog-8683684774032524979.post-6676096137989325264</id><published>2011-12-15T05:30:00.000-02:00</published><updated>2011-12-15T05:30:20.997-02:00</updated><app:edited xmlns:app="http://www.w3.org/2007/app">2011-12-15T05:30:20.997-02:00</app:edited><title>Hotel é evacuado após grupo sentir tremor em evento escolar</title><content type="html">&lt;span class="Apple-style-span" style="color: #222222; font-family: arial, sans-serif; font-size: 13px;"&gt;&lt;a href="http://www.google.com/url?sa=X&amp;amp;q=http://eptv.globo.com/noticias/NOT,4,4,384007,Hotel%2Be%2Bevacuado%2Bapos%2Bgrupo%2Bsentir%2Btremor%2Bem%2Bevento%2Bescolar.aspx&amp;amp;ct=ga&amp;amp;cad=CAcQAhgAIAAoATACOAJAl9Sk9wRIAVAAWABiBXB0LUJS&amp;amp;cd=Irj2Yh3mesQ&amp;amp;usg=AFQjCNEHQvAmyQqCJHEOfMYAnV2RCCR7pA" style="color: #1111cc;" target="_blank"&gt;Hotel é evacuado após grupo sentir&amp;nbsp;&lt;b&gt;tremor&lt;/b&gt;&amp;nbsp;em evento escolar&lt;/a&gt;&lt;/span&gt;&lt;span class="Apple-style-span" style="color: #222222;"&gt;&lt;span class="Apple-style-span" style="font-family: arial, sans-serif; font-size: x-small;"&gt;&lt;br /&gt;
&lt;/span&gt;&lt;/span&gt;&lt;span class="Apple-style-span" style="color: #222222; font-family: arial, sans-serif; font-size: 13px;"&gt;&lt;span&gt;&lt;a href="" style="color: #777777; text-decoration: none;"&gt;EPTV&lt;/a&gt;&lt;/span&gt;&lt;/span&gt;&lt;br /&gt;
&lt;span class="Apple-style-span" style="font-family: arial, sans-serif; font-size: 13px;"&gt;&lt;span&gt;&lt;span class="Apple-style-span" style="color: #777777;"&gt;&lt;br /&gt;
&lt;/span&gt;&lt;span class="Apple-style-span" style="color: #222222;"&gt;O Observatório Sismológico da Universidade de Brasília (UNB) informou que não registrou nenhuma ocorrência de&amp;nbsp;&lt;/span&gt;&lt;b style="color: #222222;"&gt;tremor de terra&lt;/b&gt;&lt;span class="Apple-style-span" style="color: #222222;"&gt;&amp;nbsp;no Sul de Minas. Na hora do incidente, acontecia no hotel uma festa de encerramento de ano letivo do ensino infantil e&amp;nbsp;&lt;/span&gt;&lt;b style="color: #222222;"&gt;...&lt;/b&gt;&lt;/span&gt;&lt;/span&gt;&lt;br /&gt;
&lt;span class="Apple-style-span" style="font-family: arial, sans-serif; font-size: 13px;"&gt;&lt;span&gt;&lt;b style="color: #222222;"&gt;&lt;br /&gt;
&lt;/b&gt;&lt;/span&gt;&lt;/span&gt;&lt;br /&gt;
&lt;span class="Apple-style-span" style="font-family: arial, sans-serif; font-size: 13px;"&gt;&lt;span&gt;&lt;b style="color: #222222;"&gt;Não existe registro desse provável tremor.&lt;/b&gt;&lt;/span&gt;&lt;/span&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/8683684774032524979-6676096137989325264?l=tremordeterra.blogspot.com' alt='' /&gt;&lt;/div&gt;
&lt;p&gt;&lt;a href="http://feedads.g.doubleclick.net/~a/oR7upCHW4obdkgt5yKcZFwFChFI/0/da"&gt;&lt;img src="http://feedads.g.doubleclick.net/~a/oR7upCHW4obdkgt5yKcZFwFChFI/0/di" border="0" ismap="true"&gt;&lt;/img&gt;&lt;/a&gt;&lt;br/&gt;
&lt;a href="http://feedads.g.doubleclick.net/~a/oR7upCHW4obdkgt5yKcZFwFChFI/1/da"&gt;&lt;img src="http://feedads.g.doubleclick.net/~a/oR7upCHW4obdkgt5yKcZFwFChFI/1/di" border="0" ismap="true"&gt;&lt;/img&gt;&lt;/a&gt;&lt;/p&gt;&lt;img src="http://feeds.feedburner.com/~r/blogspot/surOo/~4/NMTM4hYynaY" height="1" width="1"/&gt;</content><link rel="replies" type="application/atom+xml" href="http://tremordeterra.blogspot.com/feeds/6676096137989325264/comments/default" title="Postar comentários" /><link rel="replies" type="text/html" href="http://tremordeterra.blogspot.com/2011/12/hotel-e-evacuado-apos-grupo-sentir.html#comment-form" title="0 Comentários" /><link rel="edit" type="application/atom+xml" href="http://www.blogger.com/feeds/8683684774032524979/posts/default/6676096137989325264?v=2" /><link rel="self" type="application/atom+xml" href="http://www.blogger.com/feeds/8683684774032524979/posts/default/6676096137989325264?v=2" /><link rel="alternate" type="text/html" href="http://feedproxy.google.com/~r/blogspot/surOo/~3/NMTM4hYynaY/hotel-e-evacuado-apos-grupo-sentir.html" title="Hotel é evacuado após grupo sentir tremor em evento escolar" /><author><name>Prof.  George Sand França (Universidade de Brasília)</name><uri>http://www.blogger.com/profile/13658186359698780690</uri><email>noreply@blogger.com</email><gd:image rel="http://schemas.google.com/g/2005#thumbnail" width="32" height="24" src="http://bp0.blogger.com/_YWldrkTV_x8/R_ho6CYm-WI/AAAAAAAABas/e3S7LPid2TU/S220/mar%C3%A7o2008+015.jpg" /></author><thr:total>0</thr:total><feedburner:origLink>http://tremordeterra.blogspot.com/2011/12/hotel-e-evacuado-apos-grupo-sentir.html</feedburner:origLink></entry><entry gd:etag="W/&quot;CEEBRnk_eyp7ImA9WhRQFUU.&quot;"><id>tag:blogger.com,1999:blog-8683684774032524979.post-7460403219606214486</id><published>2011-12-11T03:50:00.000-02:00</published><updated>2011-12-11T03:50:57.743-02:00</updated><app:edited xmlns:app="http://www.w3.org/2007/app">2011-12-11T03:50:57.743-02:00</app:edited><title>6.7 Guerrero Mexico - 166 km da cidade do México.</title><content type="html">&lt;div style="text-align: center;"&gt;&lt;span class="Apple-style-span" style="color: #333333; font-family: Helvetica; font-size: 13px; line-height: 19px;"&gt;&lt;img alt="Earthquake Location" src="http://neic.usgs.gov/neis/eq_depot/2011/eq_111211_c000753u/neic_c000753u.jpg" style="border-bottom-width: 0px; border-color: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; font-family: inherit; font-size: 13px; font-style: inherit; font-weight: inherit; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; vertical-align: baseline;" /&gt;&lt;/span&gt;&lt;/div&gt;&lt;br /&gt;
&lt;br /&gt;
Bem Sentido na Cidade do México devido está sobre uma grande bacia - "Pântano" - deixando a cidade mais frágil a terremotos distantes.&lt;br /&gt;
&lt;span class="Apple-style-span" style="color: #333333; font-family: Helvetica; font-size: 13px; line-height: 19px;"&gt;&lt;/span&gt;&lt;br /&gt;
&lt;table id="parameters" style="-webkit-border-horizontal-spacing: 0px; -webkit-border-vertical-spacing: 0px; border-bottom-width: 0px; border-collapse: separate; border-color: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; font-family: inherit; font-size: 13px; font-style: inherit; font-weight: inherit; margin-bottom: 1em; margin-left: 0px; margin-right: 0px; margin-top: 1em; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; vertical-align: baseline;" summary="Earthquake Details"&gt;&lt;tbody style="border-bottom-width: 0px; border-color: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; font-family: inherit; font-size: 13px; font-style: inherit; font-weight: inherit; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; vertical-align: baseline;"&gt;
&lt;tr style="border-bottom-width: 0px; border-color: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; font-family: inherit; font-size: 13px; font-style: inherit; font-weight: inherit; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; vertical-align: baseline;"&gt;&lt;th style="background-attachment: initial; background-clip: initial; background-color: #dddddd; background-image: initial; background-origin: initial; background-position: initial initial; background-repeat: initial initial; border-bottom-color: rgb(255, 255, 255); border-bottom-style: solid; border-bottom-width: 1px; border-color: initial; border-left-color: rgb(255, 255, 255); border-left-style: solid; border-left-width: 1px; border-right-color: rgb(255, 255, 255); border-right-style: solid; border-right-width: 1px; border-style: initial; border-top-color: rgb(255, 255, 255); border-top-style: solid; border-top-width: 1px; font-family: inherit; font-size: 13px; font-style: inherit; font-weight: 400; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; padding-bottom: 3px; padding-left: 8px; padding-right: 8px; padding-top: 3px; text-align: left; vertical-align: baseline; width: 134px;"&gt;&lt;a href="http://earthquake.usgs.gov/earthquakes/glossary.php#magnitude" style="border-bottom-width: 0px; border-color: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: black; display: block; font-family: inherit; font-size: 13px; font-style: inherit; font-weight: bold; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; text-align: right; vertical-align: baseline;"&gt;Magnitude&lt;/a&gt;&lt;/th&gt;&lt;td style="background-attachment: initial; background-clip: initial; background-color: #eeeeee; background-image: initial; background-origin: initial; background-position: initial initial; background-repeat: initial initial; border-bottom-color: rgb(255, 255, 255); border-bottom-style: solid; border-bottom-width: 1px; border-color: initial; border-left-color: rgb(255, 255, 255); border-left-style: solid; border-left-width: 1px; border-right-color: rgb(255, 255, 255); border-right-style: solid; border-right-width: 1px; border-style: initial; border-top-color: rgb(255, 255, 255); border-top-style: solid; border-top-width: 1px; font-family: inherit; font-size: 13px; font-style: inherit; font-weight: 400; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; padding-bottom: 3px; padding-left: 8px; padding-right: 8px; padding-top: 3px; text-align: left; vertical-align: baseline;"&gt;&lt;strong&gt;6.5&lt;/strong&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr style="border-bottom-width: 0px; border-color: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; font-family: inherit; font-size: 13px; font-style: inherit; font-weight: inherit; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; vertical-align: baseline;"&gt;&lt;th style="background-attachment: initial; background-clip: initial; background-color: #dddddd; background-image: initial; background-origin: initial; background-position: initial initial; background-repeat: initial initial; border-bottom-color: rgb(255, 255, 255); border-bottom-style: solid; border-bottom-width: 1px; border-color: initial; border-left-color: rgb(255, 255, 255); border-left-style: solid; border-left-width: 1px; border-right-color: rgb(255, 255, 255); border-right-style: solid; border-right-width: 1px; border-style: initial; border-top-color: rgb(255, 255, 255); border-top-style: solid; border-top-width: 1px; font-family: inherit; font-size: 13px; font-style: inherit; font-weight: 400; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; padding-bottom: 3px; padding-left: 8px; padding-right: 8px; padding-top: 3px; text-align: left; vertical-align: baseline; width: 134px;"&gt;&lt;a href="http://earthquake.usgs.gov/earthquakes/glossary.php#date" style="border-bottom-width: 0px; border-color: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: black; display: block; font-family: inherit; font-size: 13px; font-style: inherit; font-weight: bold; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; text-align: right; vertical-align: baseline;"&gt;Dia-Tempo&lt;/a&gt;&lt;/th&gt;&lt;td style="background-attachment: initial; background-clip: initial; background-color: #eeeeee; background-image: initial; background-origin: initial; background-position: initial initial; background-repeat: initial initial; border-bottom-color: rgb(255, 255, 255); border-bottom-style: solid; border-bottom-width: 1px; border-color: initial; border-left-color: rgb(255, 255, 255); border-left-style: solid; border-left-width: 1px; border-right-color: rgb(255, 255, 255); border-right-style: solid; border-right-width: 1px; border-style: initial; border-top-color: rgb(255, 255, 255); border-top-style: solid; border-top-width: 1px; font-family: inherit; font-size: 13px; font-style: inherit; font-weight: 400; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; padding-bottom: 3px; padding-left: 8px; padding-right: 8px; padding-top: 3px; text-align: left; vertical-align: baseline;"&gt;&lt;ul style="border-bottom-width: 0px; border-color: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; font-family: inherit; font-size: 13px; font-style: inherit; font-weight: inherit; list-style-image: initial; list-style-position: initial; list-style-type: none; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 1em; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; vertical-align: baseline;"&gt;&lt;li style="border-bottom-width: 0px; border-color: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; font-family: inherit; font-size: 13px; font-style: inherit; font-weight: inherit; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; vertical-align: baseline;"&gt;&lt;strong&gt;Domingo, 11 de Dezembro de 2011 às 01:47:26 UTC&lt;/strong&gt;&lt;/li&gt;
&lt;/ul&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr style="border-bottom-width: 0px; border-color: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; font-family: inherit; font-size: 13px; font-style: inherit; font-weight: inherit; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; vertical-align: baseline;"&gt;&lt;th style="background-attachment: initial; background-clip: initial; background-color: #dddddd; background-image: initial; background-origin: initial; background-position: initial initial; background-repeat: initial initial; border-bottom-color: rgb(255, 255, 255); border-bottom-style: solid; border-bottom-width: 1px; border-color: initial; border-left-color: rgb(255, 255, 255); border-left-style: solid; border-left-width: 1px; border-right-color: rgb(255, 255, 255); border-right-style: solid; border-right-width: 1px; border-style: initial; border-top-color: rgb(255, 255, 255); border-top-style: solid; border-top-width: 1px; font-family: inherit; font-size: 13px; font-style: inherit; font-weight: 400; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; padding-bottom: 3px; padding-left: 8px; padding-right: 8px; padding-top: 3px; text-align: left; vertical-align: baseline; width: 134px;"&gt;&lt;a href="http://earthquake.usgs.gov/earthquakes/glossary.php#location" style="border-bottom-width: 0px; border-color: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: black; display: block; font-family: inherit; font-size: 13px; font-style: inherit; font-weight: bold; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; text-align: right; vertical-align: baseline;"&gt;Localização&lt;/a&gt;&lt;/th&gt;&lt;td style="background-attachment: initial; background-clip: initial; background-color: #eeeeee; background-image: initial; background-origin: initial; background-position: initial initial; background-repeat: initial initial; border-bottom-color: rgb(255, 255, 255); border-bottom-style: solid; border-bottom-width: 1px; border-color: initial; border-left-color: rgb(255, 255, 255); border-left-style: solid; border-left-width: 1px; border-right-color: rgb(255, 255, 255); border-right-style: solid; border-right-width: 1px; border-style: initial; border-top-color: rgb(255, 255, 255); border-top-style: solid; border-top-width: 1px; font-family: inherit; font-size: 13px; font-style: inherit; font-weight: 400; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; padding-bottom: 3px; padding-left: 8px; padding-right: 8px; padding-top: 3px; text-align: left; vertical-align: baseline;"&gt;18.038°N, 99.796°W&lt;/td&gt;&lt;/tr&gt;
&lt;tr style="border-bottom-width: 0px; border-color: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; font-family: inherit; font-size: 13px; font-style: inherit; font-weight: inherit; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; vertical-align: baseline;"&gt;&lt;th style="background-attachment: initial; background-clip: initial; background-color: #dddddd; background-image: initial; background-origin: initial; background-position: initial initial; background-repeat: initial initial; border-bottom-color: rgb(255, 255, 255); border-bottom-style: solid; border-bottom-width: 1px; border-color: initial; border-left-color: rgb(255, 255, 255); border-left-style: solid; border-left-width: 1px; border-right-color: rgb(255, 255, 255); border-right-style: solid; border-right-width: 1px; border-style: initial; border-top-color: rgb(255, 255, 255); border-top-style: solid; border-top-width: 1px; font-family: inherit; font-size: 13px; font-style: inherit; font-weight: 400; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; padding-bottom: 3px; padding-left: 8px; padding-right: 8px; padding-top: 3px; text-align: left; vertical-align: baseline; width: 134px;"&gt;&lt;a href="http://earthquake.usgs.gov/earthquakes/glossary.php#depth" style="border-bottom-width: 0px; border-color: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: black; display: block; font-family: inherit; font-size: 13px; font-style: inherit; font-weight: bold; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; text-align: right; vertical-align: baseline;"&gt;Profundidade&lt;/a&gt;&lt;/th&gt;&lt;td style="background-attachment: initial; background-clip: initial; background-color: #eeeeee; background-image: initial; background-origin: initial; background-position: initial initial; background-repeat: initial initial; border-bottom-color: rgb(255, 255, 255); border-bottom-style: solid; border-bottom-width: 1px; border-color: initial; border-left-color: rgb(255, 255, 255); border-left-style: solid; border-left-width: 1px; border-right-color: rgb(255, 255, 255); border-right-style: solid; border-right-width: 1px; border-style: initial; border-top-color: rgb(255, 255, 255); border-top-style: solid; border-top-width: 1px; font-family: inherit; font-size: 13px; font-style: inherit; font-weight: 400; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; padding-bottom: 3px; padding-left: 8px; padding-right: 8px; padding-top: 3px; text-align: left; vertical-align: baseline;"&gt;64.9 km&amp;nbsp;&lt;/td&gt;&lt;/tr&gt;
&lt;tr style="border-bottom-width: 0px; border-color: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; font-family: inherit; font-size: 13px; font-style: inherit; font-weight: inherit; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; vertical-align: baseline;"&gt;&lt;th style="background-attachment: initial; background-clip: initial; background-color: #dddddd; background-image: initial; background-origin: initial; background-position: initial initial; background-repeat: initial initial; border-bottom-color: rgb(255, 255, 255); border-bottom-style: solid; border-bottom-width: 1px; border-color: initial; border-left-color: rgb(255, 255, 255); border-left-style: solid; border-left-width: 1px; border-right-color: rgb(255, 255, 255); border-right-style: solid; border-right-width: 1px; border-style: initial; border-top-color: rgb(255, 255, 255); border-top-style: solid; border-top-width: 1px; font-family: inherit; font-size: 13px; font-style: inherit; font-weight: 400; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; padding-bottom: 3px; padding-left: 8px; padding-right: 8px; padding-top: 3px; text-align: left; vertical-align: baseline; width: 134px;"&gt;&lt;a href="http://earthquake.usgs.gov/earthquakes/glossary.php#region" style="border-bottom-width: 0px; border-color: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: black; display: block; font-family: inherit; font-size: 13px; font-style: inherit; font-weight: bold; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; text-align: right; vertical-align: baseline;"&gt;Região&lt;/a&gt;&lt;/th&gt;&lt;td style="background-attachment: initial; background-clip: initial; background-color: #eeeeee; background-image: initial; background-origin: initial; background-position: initial initial; background-repeat: initial initial; border-bottom-color: rgb(255, 255, 255); border-bottom-style: solid; border-bottom-width: 1px; border-color: initial; border-left-color: rgb(255, 255, 255); border-left-style: solid; border-left-width: 1px; border-right-color: rgb(255, 255, 255); border-right-style: solid; border-right-width: 1px; border-style: initial; border-top-color: rgb(255, 255, 255); border-top-style: solid; border-top-width: 1px; font-family: inherit; font-size: 13px; font-style: inherit; font-weight: 400; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; padding-bottom: 3px; padding-left: 8px; padding-right: 8px; padding-top: 3px; text-align: left; vertical-align: baseline;"&gt;GUERRERO, MEXICO&lt;/td&gt;&lt;/tr&gt;
&lt;tr style="border-bottom-width: 0px; border-color: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; font-family: inherit; font-size: 13px; font-style: inherit; font-weight: inherit; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; vertical-align: baseline;"&gt;&lt;th style="background-attachment: initial; background-clip: initial; background-color: #dddddd; background-image: initial; background-origin: initial; background-position: initial initial; background-repeat: initial initial; border-bottom-color: rgb(255, 255, 255); border-bottom-style: solid; border-bottom-width: 1px; border-color: initial; border-left-color: rgb(255, 255, 255); border-left-style: solid; border-left-width: 1px; border-right-color: rgb(255, 255, 255); border-right-style: solid; border-right-width: 1px; border-style: initial; border-top-color: rgb(255, 255, 255); border-top-style: solid; border-top-width: 1px; font-family: inherit; font-size: 13px; font-style: inherit; font-weight: 400; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; padding-bottom: 3px; padding-left: 8px; padding-right: 8px; padding-top: 3px; text-align: left; vertical-align: baseline; width: 134px;"&gt;&lt;a href="http://earthquake.usgs.gov/earthquakes/glossary.php#distances" style="border-bottom-width: 0px; border-color: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: black; display: block; font-family: inherit; font-size: 13px; font-style: inherit; font-weight: bold; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; text-align: right; vertical-align: baseline;"&gt;Distancias&lt;/a&gt;&lt;/th&gt;&lt;td style="background-attachment: initial; background-clip: initial; background-color: #eeeeee; background-image: initial; background-origin: initial; background-position: initial initial; background-repeat: initial initial; border-bottom-color: rgb(255, 255, 255); border-bottom-style: solid; border-bottom-width: 1px; border-color: initial; border-left-color: rgb(255, 255, 255); border-left-style: solid; border-left-width: 1px; border-right-color: rgb(255, 255, 255); border-right-style: solid; border-right-width: 1px; border-style: initial; border-top-color: rgb(255, 255, 255); border-top-style: solid; border-top-width: 1px; font-family: inherit; font-size: 13px; font-style: inherit; font-weight: 400; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; padding-bottom: 3px; padding-left: 8px; padding-right: 8px; padding-top: 3px; text-align: left; vertical-align: baseline;"&gt;42 km SW de&amp;nbsp;&lt;b&gt;Iguala, Guerrero, Mexico&lt;/b&gt;&lt;br /&gt;
56 km ESE de&amp;nbsp;&lt;b&gt;Arcelia, Guerrero, Mexico&lt;/b&gt;&lt;br /&gt;
166 km SSW da Cidade do&amp;nbsp;&lt;b&gt;MEXICO, D.F., Mexico&lt;/b&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr style="border-bottom-width: 0px; border-color: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; font-family: inherit; font-size: 13px; font-style: inherit; font-weight: inherit; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; vertical-align: baseline;"&gt;&lt;th style="background-attachment: initial; background-clip: initial; background-color: #dddddd; background-image: initial; background-origin: initial; background-position: initial initial; background-repeat: initial initial; border-bottom-color: rgb(255, 255, 255); border-bottom-style: solid; border-bottom-width: 1px; border-color: initial; border-left-color: rgb(255, 255, 255); border-left-style: solid; border-left-width: 1px; border-right-color: rgb(255, 255, 255); border-right-style: solid; border-right-width: 1px; border-style: initial; border-top-color: rgb(255, 255, 255); border-top-style: solid; border-top-width: 1px; font-family: inherit; font-size: 13px; font-style: inherit; font-weight: 400; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; padding-bottom: 3px; padding-left: 8px; padding-right: 8px; padding-top: 3px; text-align: left; vertical-align: baseline; width: 134px;"&gt;&lt;a href="http://earthquake.usgs.gov/earthquakes/glossary.php#uncertainty" style="border-bottom-width: 0px; border-color: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: black; display: block; font-family: inherit; font-size: 13px; font-style: inherit; font-weight: bold; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; text-align: right; vertical-align: baseline;"&gt;Incerteza da Localização&lt;/a&gt;&lt;/th&gt;&lt;td style="background-attachment: initial; background-clip: initial; background-color: #eeeeee; background-image: initial; background-origin: initial; background-position: initial initial; background-repeat: initial initial; border-bottom-color: rgb(255, 255, 255); border-bottom-style: solid; border-bottom-width: 1px; border-color: initial; border-left-color: rgb(255, 255, 255); border-left-style: solid; border-left-width: 1px; border-right-color: rgb(255, 255, 255); border-right-style: solid; border-right-width: 1px; border-style: initial; border-top-color: rgb(255, 255, 255); border-top-style: solid; border-top-width: 1px; font-family: inherit; font-size: 13px; font-style: inherit; font-weight: 400; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; padding-bottom: 3px; padding-left: 8px; padding-right: 8px; padding-top: 3px; text-align: left; vertical-align: baseline;"&gt;horizontal +/- 14.5 km; profundidade +/- 9.8 km&lt;/td&gt;&lt;/tr&gt;
&lt;tr style="border-bottom-width: 0px; border-color: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; font-family: inherit; font-size: 13px; font-style: inherit; font-weight: inherit; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; vertical-align: baseline;"&gt;&lt;th style="background-attachment: initial; background-clip: initial; background-color: #dddddd; background-image: initial; background-origin: initial; background-position: initial initial; background-repeat: initial initial; border-bottom-color: rgb(255, 255, 255); border-bottom-style: solid; border-bottom-width: 1px; border-color: initial; border-left-color: rgb(255, 255, 255); border-left-style: solid; border-left-width: 1px; border-right-color: rgb(255, 255, 255); border-right-style: solid; border-right-width: 1px; border-style: initial; border-top-color: rgb(255, 255, 255); border-top-style: solid; border-top-width: 1px; font-family: inherit; font-size: 13px; font-style: inherit; font-weight: 400; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; padding-bottom: 3px; padding-left: 8px; padding-right: 8px; padding-top: 3px; text-align: left; vertical-align: baseline; width: 134px;"&gt;&lt;a href="http://earthquake.usgs.gov/earthquakes/glossary.php#parameters" style="border-bottom-width: 0px; border-color: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: black; display: block; font-family: inherit; font-size: 13px; font-style: inherit; font-weight: bold; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; text-align: right; vertical-align: baseline;"&gt;Parâmetros&lt;/a&gt;&lt;/th&gt;&lt;td style="background-attachment: initial; background-clip: initial; background-color: #eeeeee; background-image: initial; background-origin: initial; background-position: initial initial; background-repeat: initial initial; border-bottom-color: rgb(255, 255, 255); border-bottom-style: solid; border-bottom-width: 1px; border-color: initial; border-left-color: rgb(255, 255, 255); border-left-style: solid; border-left-width: 1px; border-right-color: rgb(255, 255, 255); border-right-style: solid; border-right-width: 1px; border-style: initial; border-top-color: rgb(255, 255, 255); border-top-style: solid; border-top-width: 1px; font-family: inherit; font-size: 13px; font-style: inherit; font-weight: 400; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; padding-bottom: 3px; padding-left: 8px; padding-right: 8px; padding-top: 3px; text-align: left; vertical-align: baseline;"&gt;NST=488, Nph=488, Dmin=140.3 km, Rmss=0.78 sec, Gp= 43°,&lt;br /&gt;
M-type=regional moment magnitude (Mw), Version=8&lt;/td&gt;&lt;/tr&gt;
&lt;tr style="border-bottom-width: 0px; border-color: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; font-family: inherit; font-size: 13px; font-style: inherit; font-weight: inherit; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; vertical-align: baseline;"&gt;&lt;th style="background-attachment: initial; background-clip: initial; background-color: #dddddd; background-image: initial; background-origin: initial; background-position: initial initial; background-repeat: initial initial; border-bottom-color: rgb(255, 255, 255); border-bottom-style: solid; border-bottom-width: 1px; border-color: initial; border-left-color: rgb(255, 255, 255); border-left-style: solid; border-left-width: 1px; border-right-color: rgb(255, 255, 255); border-right-style: solid; border-right-width: 1px; border-style: initial; border-top-color: rgb(255, 255, 255); border-top-style: solid; border-top-width: 1px; font-family: inherit; font-size: 13px; font-style: inherit; font-weight: 400; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; padding-bottom: 3px; padding-left: 8px; padding-right: 8px; padding-top: 3px; text-align: left; vertical-align: baseline; width: 134px;"&gt;&lt;a href="http://earthquake.usgs.gov/earthquakes/glossary.php#source" style="border-bottom-width: 0px; border-color: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; color: black; display: block; font-family: inherit; font-size: 13px; font-style: inherit; font-weight: bold; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; text-align: right; vertical-align: baseline;"&gt;Fonte&lt;/a&gt;&lt;/th&gt;&lt;td style="background-attachment: initial; background-clip: initial; background-color: #eeeeee; background-image: initial; background-origin: initial; background-position: initial initial; background-repeat: initial initial; border-bottom-color: rgb(255, 255, 255); border-bottom-style: solid; border-bottom-width: 1px; border-color: initial; border-left-color: rgb(255, 255, 255); border-left-style: solid; border-left-width: 1px; border-right-color: rgb(255, 255, 255); border-right-style: solid; border-right-width: 1px; border-style: initial; border-top-color: rgb(255, 255, 255); border-top-style: solid; border-top-width: 1px; font-family: inherit; font-size: 13px; font-style: inherit; font-weight: 400; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; padding-bottom: 3px; padding-left: 8px; padding-right: 8px; padding-top: 3px; text-align: left; vertical-align: baseline;"&gt;&lt;ul style="border-bottom-width: 0px; border-color: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; font-family: inherit; font-size: 13px; font-style: inherit; font-weight: inherit; list-style-image: initial; list-style-position: initial; list-style-type: none; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 1em; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; vertical-align: baseline;"&gt;&lt;li style="border-bottom-width: 0px; border-color: initial; border-left-width: 0px; border-right-width: 0px; border-style: initial; border-top-width: 0px; font-family: inherit; font-size: 13px; font-style: inherit; font-weight: inherit; margin-bottom: 0px; margin-left: 0px; margin-right: 0px; margin-top: 0px; padding-bottom: 0px; padding-left: 0px; padding-right: 0px; padding-top: 0px; vertical-align: baseline;"&gt;&lt;b&gt;Magnitude:&lt;/b&gt;&amp;nbsp;USGS NEIC (WDCS-D)&lt;br /&gt;
&lt;b&gt;Localização:&lt;/b&gt;&amp;nbsp;USGS NEIC (WDCS-D)&lt;/li&gt;
&lt;/ul&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/tbody&gt;&lt;/table&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/8683684774032524979-7460403219606214486?l=tremordeterra.blogspot.com' alt='' /&gt;&lt;/div&gt;
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&lt;a href="http://feedads.g.doubleclick.net/~a/60J1kYdq7Ojmpc5jGLBcOUrVcyw/1/da"&gt;&lt;img src="http://feedads.g.doubleclick.net/~a/60J1kYdq7Ojmpc5jGLBcOUrVcyw/1/di" border="0" ismap="true"&gt;&lt;/img&gt;&lt;/a&gt;&lt;/p&gt;&lt;img src="http://feeds.feedburner.com/~r/blogspot/surOo/~4/JEmxalK9dLM" height="1" width="1"/&gt;</content><link rel="replies" type="application/atom+xml" href="http://tremordeterra.blogspot.com/feeds/7460403219606214486/comments/default" title="Postar comentários" /><link rel="replies" type="text/html" href="http://tremordeterra.blogspot.com/2011/12/67-guerrero-mexico-166-km-da-cidade-do.html#comment-form" title="0 Comentários" /><link rel="edit" type="application/atom+xml" href="http://www.blogger.com/feeds/8683684774032524979/posts/default/7460403219606214486?v=2" /><link rel="self" type="application/atom+xml" href="http://www.blogger.com/feeds/8683684774032524979/posts/default/7460403219606214486?v=2" /><link rel="alternate" type="text/html" href="http://feedproxy.google.com/~r/blogspot/surOo/~3/JEmxalK9dLM/67-guerrero-mexico-166-km-da-cidade-do.html" title="6.7 Guerrero Mexico - 166 km da cidade do México." /><author><name>Prof.  George Sand França (Universidade de Brasília)</name><uri>http://www.blogger.com/profile/13658186359698780690</uri><email>noreply@blogger.com</email><gd:image rel="http://schemas.google.com/g/2005#thumbnail" width="32" height="24" src="http://bp0.blogger.com/_YWldrkTV_x8/R_ho6CYm-WI/AAAAAAAABas/e3S7LPid2TU/S220/mar%C3%A7o2008+015.jpg" /></author><thr:total>0</thr:total><feedburner:origLink>http://tremordeterra.blogspot.com/2011/12/67-guerrero-mexico-166-km-da-cidade-do.html</feedburner:origLink></entry><entry gd:etag="W/&quot;DEYMSXkyfyp7ImA9WhRQEU8.&quot;"><id>tag:blogger.com,1999:blog-8683684774032524979.post-2558208558723931384</id><published>2011-12-05T21:03:00.000-02:00</published><updated>2011-12-05T21:03:08.797-02:00</updated><app:edited xmlns:app="http://www.w3.org/2007/app">2011-12-05T21:03:08.797-02:00</app:edited><title>Tremor de terra na Zona Rural de Petrolina foi de magnitude igual 3.1</title><content type="html">Um tremor de terra com magnitude de 3.1 de magnitude foi sentido às 12h48 do último sábado (03).&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/8683684774032524979-2558208558723931384?l=tremordeterra.blogspot.com' alt='' /&gt;&lt;/div&gt;
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&lt;a href="http://feedads.g.doubleclick.net/~a/sHPlU10cq5MDhuuoUdUagXiDwyU/1/da"&gt;&lt;img src="http://feedads.g.doubleclick.net/~a/sHPlU10cq5MDhuuoUdUagXiDwyU/1/di" border="0" ismap="true"&gt;&lt;/img&gt;&lt;/a&gt;&lt;/p&gt;&lt;img src="http://feeds.feedburner.com/~r/blogspot/surOo/~4/sLghojRFq_I" height="1" width="1"/&gt;</content><link rel="replies" type="application/atom+xml" href="http://tremordeterra.blogspot.com/feeds/2558208558723931384/comments/default" title="Postar comentários" /><link rel="replies" type="text/html" href="http://tremordeterra.blogspot.com/2011/12/tremor-de-terra-na-zona-rural-de.html#comment-form" title="1 Comentários" /><link rel="edit" type="application/atom+xml" href="http://www.blogger.com/feeds/8683684774032524979/posts/default/2558208558723931384?v=2" /><link rel="self" type="application/atom+xml" href="http://www.blogger.com/feeds/8683684774032524979/posts/default/2558208558723931384?v=2" /><link rel="alternate" type="text/html" href="http://feedproxy.google.com/~r/blogspot/surOo/~3/sLghojRFq_I/tremor-de-terra-na-zona-rural-de.html" title="Tremor de terra na Zona Rural de Petrolina foi de magnitude igual 3.1" /><author><name>Prof.  George Sand França (Universidade de Brasília)</name><uri>http://www.blogger.com/profile/13658186359698780690</uri><email>noreply@blogger.com</email><gd:image rel="http://schemas.google.com/g/2005#thumbnail" width="32" height="24" src="http://bp0.blogger.com/_YWldrkTV_x8/R_ho6CYm-WI/AAAAAAAABas/e3S7LPid2TU/S220/mar%C3%A7o2008+015.jpg" /></author><thr:total>1</thr:total><feedburner:origLink>http://tremordeterra.blogspot.com/2011/12/tremor-de-terra-na-zona-rural-de.html</feedburner:origLink></entry><entry gd:etag="W/&quot;DUABR3s5eCp7ImA9WhRRGEo.&quot;"><id>tag:blogger.com,1999:blog-8683684774032524979.post-7027137406245845661</id><published>2011-12-02T23:59:00.001-02:00</published><updated>2011-12-03T00:02:36.520-02:00</updated><app:edited xmlns:app="http://www.w3.org/2007/app">2011-12-03T00:02:36.520-02:00</app:edited><title>Sapos conseguem prever tremores de terra com dias de antecedência</title><content type="html">&lt;div class="ECOSFERA_MANCHETE"&gt;&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://3.bp.blogspot.com/-RtHBKsRyYDs/TtmDE66n8SI/AAAAAAAAGqQ/C3n6PIEB1QE/s1600/sapos.jpg" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://3.bp.blogspot.com/-RtHBKsRyYDs/TtmDE66n8SI/AAAAAAAAGqQ/C3n6PIEB1QE/s1600/sapos.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;br /&gt;
&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;/div&gt;&lt;span class="ECOSFERA_texto_01"&gt;&lt;br /&gt;
Helena Geraldes do &lt;a href="http://ecosfera.publico.clix.pt/noticia.aspx?id=1523490"&gt;Ecosfera&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp; &lt;/a&gt;&lt;/span&gt;Clique&amp;nbsp; para fonte original                 &lt;/div&gt;&lt;div class="ECOSFERA_texto_01"&gt;A debandada geral de uma colónia de sapos num  lago em L'Aquila, Itália, dias antes de um sismo em 2009 surpreendeu uma  equipa de investigadores. Depois de anos de estudo concluíram que estes  anfíbios conseguem prever os tremores de terra com vários dias de  antecedência.&lt;br /&gt;
&lt;br /&gt;
A bióloga da Universidade Aberta do Reino Unido, Rachel Grant, monitorizava uma colónia de sapos-comuns (&lt;i&gt;Bufo bufo&lt;/i&gt;)  num lago em L’Aquila, Itália, quando tudo aconteceu. “Foi dramático. Em  apenas três dias, a colónia passou de 96 sapos para zero”, disse a  investigadora à BBC, que publicou os seus dados na revista &lt;i&gt;Journal of Zoology&lt;/i&gt;.&lt;br /&gt;
&lt;br /&gt;
&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://3.bp.blogspot.com/-mxhEc4x6L20/TtmDHN3zFqI/AAAAAAAAGqY/elOYNxltM3Y/s1600/sapos-15.gif" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"&gt;&lt;img border="0" height="272" src="http://3.bp.blogspot.com/-mxhEc4x6L20/TtmDHN3zFqI/AAAAAAAAGqY/elOYNxltM3Y/s320/sapos-15.gif" width="320" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
O  estudo revela que os sapos “mostraram um comportamento muito pouco  habitual antes do sismo de magnitude 6.3 na escala de Richter em  L’Aquila, em Itália, a 6 de Abril de 2009”. “Dias antes do sismo, os  sapos desapareceram subitamente dos seus locais de reprodução num  pequeno lago a 75 quilômetros do epicentro e só regressaram depois de  uma série de réplicas”, acrescenta o estudo.&lt;br /&gt;
&lt;br /&gt;
Pouco tempo depois,  Rachel Grant foi contactada pela NASA (agência espacial  norte-americana), que estudava as alterações químicas que ocorrem quando  as rochas estão sob stress extremo.&lt;br /&gt;
&lt;br /&gt;
Com base em testes em  laboratório, a equipa de sete investigadores coordenada pelo geofísico  Friedemann Freund, da NASA, &lt;b&gt;concluiu que os animais detectam as  alterações químicas na água subterrânea, causadas pela libertação de  partículas através das rochas na crosta terrestre que estão em tensão&lt;/b&gt;,  devido às forças tectônicas antes de um sismo. Esta cadeia química pode  afetar o material orgânico dissolvido nas águas de um lago,  transformando materiais inofensivos em substâncias que são tóxicas para  os animais aquáticos.&lt;br /&gt;
&lt;br /&gt;
Segundo a equipa de investigação, que publicou as suas conclusões na revista &lt;i&gt;Journal of Environmental Research and Public Health&lt;/i&gt;, os animais que vivem nessas águas ou perto delas são extremamente sensíveis às mudanças na sua composição química. &lt;br /&gt;
&lt;br /&gt;
Os  investigadores acreditam que biólogos e geólogos podem trabalhar em  conjunto para preparar melhor a chegada de um sismo. Freund diz que o  comportamento destes animais pode ser apenas um de uma cadeia de eventos  que podem prever um sismo. “Quando compreendermos de que forma estes  sinais estão ligados e se virmos quatro ou cinco a apontar na mesma  direcção, então podemos dizer que algo está para acontecer.”&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/8683684774032524979-7027137406245845661?l=tremordeterra.blogspot.com' alt='' /&gt;&lt;/div&gt;
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&lt;a href="http://feedads.g.doubleclick.net/~a/wv8EmISvoMpSHIMLSuNCs0YSY0c/1/da"&gt;&lt;img src="http://feedads.g.doubleclick.net/~a/wv8EmISvoMpSHIMLSuNCs0YSY0c/1/di" border="0" ismap="true"&gt;&lt;/img&gt;&lt;/a&gt;&lt;/p&gt;&lt;img src="http://feeds.feedburner.com/~r/blogspot/surOo/~4/lc4XesuYgQI" height="1" width="1"/&gt;</content><link rel="replies" type="application/atom+xml" href="http://tremordeterra.blogspot.com/feeds/7027137406245845661/comments/default" title="Postar comentários" /><link rel="replies" type="text/html" href="http://tremordeterra.blogspot.com/2011/12/sapos-conseguem-prever-tremores-de.html#comment-form" title="0 Comentários" /><link rel="edit" type="application/atom+xml" href="http://www.blogger.com/feeds/8683684774032524979/posts/default/7027137406245845661?v=2" /><link rel="self" type="application/atom+xml" href="http://www.blogger.com/feeds/8683684774032524979/posts/default/7027137406245845661?v=2" /><link rel="alternate" type="text/html" href="http://feedproxy.google.com/~r/blogspot/surOo/~3/lc4XesuYgQI/sapos-conseguem-prever-tremores-de.html" title="Sapos conseguem prever tremores de terra com dias de antecedência" /><author><name>Prof.  George Sand França (Universidade de Brasília)</name><uri>http://www.blogger.com/profile/13658186359698780690</uri><email>noreply@blogger.com</email><gd:image rel="http://schemas.google.com/g/2005#thumbnail" width="32" height="24" src="http://bp0.blogger.com/_YWldrkTV_x8/R_ho6CYm-WI/AAAAAAAABas/e3S7LPid2TU/S220/mar%C3%A7o2008+015.jpg" /></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="http://3.bp.blogspot.com/-RtHBKsRyYDs/TtmDE66n8SI/AAAAAAAAGqQ/C3n6PIEB1QE/s72-c/sapos.jpg" height="72" width="72" /><thr:total>0</thr:total><feedburner:origLink>http://tremordeterra.blogspot.com/2011/12/sapos-conseguem-prever-tremores-de.html</feedburner:origLink></entry><entry gd:etag="W/&quot;D04DRXY9eyp7ImA9WhRRFUQ.&quot;"><id>tag:blogger.com,1999:blog-8683684774032524979.post-2675308378756421642</id><published>2011-11-29T17:45:00.001-02:00</published><updated>2011-11-29T17:46:14.863-02:00</updated><app:edited xmlns:app="http://www.w3.org/2007/app">2011-11-29T17:46:14.863-02:00</app:edited><title>25 anos do Tremor de João Câmara</title><content type="html">&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://3.bp.blogspot.com/-weE2XjxkFzU/TtUvc-1uyaI/AAAAAAAAGqA/yuZW02FnTFg/s1600/0%252C%252C1138709%252C00.jpg" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://3.bp.blogspot.com/-weE2XjxkFzU/TtUvc-1uyaI/AAAAAAAAGqA/yuZW02FnTFg/s1600/0%252C%252C1138709%252C00.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;br /&gt;
&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://4.bp.blogspot.com/-FgapurpqI9o/TtUvjrnCXkI/AAAAAAAAGqI/uz5lpVCI9DY/s1600/JC_TN85827.jpg" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"&gt;&lt;img border="0" height="213" src="http://4.bp.blogspot.com/-FgapurpqI9o/TtUvjrnCXkI/AAAAAAAAGqI/uz5lpVCI9DY/s320/JC_TN85827.jpg" width="320" /&gt;&lt;/a&gt;&lt;/div&gt;&amp;nbsp;Foto:Tribuna do Norte&lt;br /&gt;
Porque comemoramos anos de Terremotos? Principalmente esse raro terremoto no Brasil. Lembrar sempre é bom, para que possamos não repetir o passado. &lt;br /&gt;
&lt;br /&gt;
Na época do Terremoto, eu estudava no Colegio APEC, no Tirol, hoje está a UNIP. Minha sala do segundo andar tremeu. Não imaginava que depois de 25 anos estaria estudos esses fenômenos tão instigantes. &lt;br /&gt;
&lt;br /&gt;
O melhor desse Terremoto é que não teve vítimas fatais! Então comemoramos!&lt;br /&gt;
&lt;br /&gt;
sites que divulgam esse evento: &lt;a href="http://tribunadonorte.com.br/noticia/tremor-em-joao-camara-completa-25-anos-conte-sua-historia/204107"&gt;Tribuna do Norte &amp;nbsp;&lt;/a&gt; e &lt;br /&gt;
&lt;a href="http://www.diariodenatal.com.br/2011/11/27/cidades3_0.php"&gt;Diário de Natal&lt;/a&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/8683684774032524979-2675308378756421642?l=tremordeterra.blogspot.com' alt='' /&gt;&lt;/div&gt;
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&lt;br /&gt;
Eu vou comprar! Parabéns pela iniciativa, isso que precisamos! Escrever Escrever e Escrever!!&lt;br /&gt;
&lt;br /&gt;
Leia a entrevista! &lt;br /&gt;
Lançamento será no dia 30/11 em Natal-RN&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
Entrevista; Alberto Veloso                                               &lt;br /&gt;
&lt;div class="internasOlhoAssina"&gt;&lt;br /&gt;
&lt;br clear="all" /&gt;&lt;/div&gt;&lt;br /&gt;
&lt;b&gt;Como iniciou o estudo da sismologia em João Câmara? &lt;br /&gt;
&lt;/b&gt;O  primeiro abalo foi registrado em agosto de 1986. Decidimos então  implantar uma estação de sismologia em João Câmara para que esses  movimentos da terra fossem registrados. No mês de setembro outros  pequenos tremores também foram detectados pelo equipamento durante  alguns dias consecutivos. No mês de outubro os abalos deram uma trégua e  em novembro foi registrado o maior deles de magnitude 5.1.&lt;br /&gt;
&lt;br /&gt;
&lt;b&gt;O senhor esteve no município acompanhando a equipe da Universidade Federal do Rio Grande do Norte.&lt;br /&gt;
&lt;/b&gt;Sim,  logo que soube do abalo decidi participar dos estudos na área. Cheguei  por volta das 15h em João Câmara. A cidade estava muito destruída.  Centenas de pessoas perderam suas casas e resolveram se mudar para  outras cidades com medo do que poderia acontecer. A escola teve que ser  demolida depois porque a estrutura estava bem comprometida. Até a  delegacia que havia sido construída recentemente e ainda não havia sido  inaugurada teve que ser demolida. Cerca de 400 casas foram afetadas e  mais de 26 mil pessoas deixaram a cidade. &lt;br /&gt;
&lt;br /&gt;
&lt;b&gt;Como foi a repercussão do terremoto?&lt;br /&gt;
&lt;/b&gt;  O tremor foi repercutido em toda a mídia nacional. João Câmara ficou  conhecida, em evidência mesmo. Autoridades políticas como o governador  Radir Pereira e o presidente José Sarney estiveram lá para acompanhar os  estudos e ajudar os desabrigados. O Exército ficou com a  responsabilidade de construir as residências para as famílias  desalojadas ou que tiveram as construções abaladas. &lt;br /&gt;
&lt;br /&gt;
&lt;b&gt;O senhor ficou quanto tempo em João Câmara nessa época?&lt;br /&gt;
&lt;/b&gt;Cheguei  no dia 30 de novembro por volta das 15h e só voltei para Brasília duas  semanas depois. Nesses dias aproveitei para conversar e gravar  depoimentos com moradores e é esse material que está incluso no livro e  que o leitor vai poder ver imagens reais do local feito por um  cinegrafista amador: eu! O vídeo foi editado da melhor forma possível  para que pudesse manter a originalidade do fato em 16 minutos.&lt;br /&gt;
&lt;br /&gt;
&lt;b&gt;O Brasil fica quase no centro de uma placa tectônica. Isso diminui a quantidade de tremores?&lt;br /&gt;
&lt;/b&gt;Digamos  que suaviza, mas nenhum lugar do mundo pode garantir ter estabilidade  absoluta. Isso é muito relativo porque depende tanto da natureza quanto  das ações do homem. Por ano são registrados no mundo cerca de 500 mil  tremores. A partir de agosto de 1986, João Câmara registrou sete anos de  abalos. Desde que instalamos a estação em João Câmara foram registrados  mais de 40 mil.&lt;br /&gt;
&lt;br /&gt;
&lt;b&gt;Qual o motivo de João Câmara e cidades da região registrar tantos abalos?      &lt;br /&gt;
&lt;/b&gt;Existe  uma falha geológica encontrada em João Câmara que não pode ser  detectada a olho nu, somente com estudos e fotografias detalhadas. Mas  ela está localizada entre 1 km e 7 km de profundidade e tem  aproximadamente 30 quilômetros de extensão. Alguns dos abalos  registrados no município foram sentidos em João Pessoa (PB).&lt;br /&gt;
&lt;br /&gt;
&lt;a href="http://www.diariodenatal.com.br/2011/11/27/cidades3_2.php"&gt;Fonte original:Diario de Natal &lt;/a&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/8683684774032524979-4623590227238502784?l=tremordeterra.blogspot.com' alt='' /&gt;&lt;/div&gt;
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&lt;br /&gt;
&lt;a href="http://produto.mercadolivre.com.br/MLB-210992895-escultura-detector-de-terremoto-porcelana-japonesa-antiga-_JM"&gt;&amp;nbsp;Clique aqui para ver no Mercado Livre&lt;/a&gt;&lt;br /&gt;
&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://2.bp.blogspot.com/-Jk8vrgxPZcs/TtC_QmHh3mI/AAAAAAAAGp4/li-27DfNYq0/s1600/s_MLB_v_F_f_210992895_3865.jpg" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"&gt;&lt;img border="0" height="320" src="http://2.bp.blogspot.com/-Jk8vrgxPZcs/TtC_QmHh3mI/AAAAAAAAGp4/li-27DfNYq0/s320/s_MLB_v_F_f_210992895_3865.jpg" width="240" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/8683684774032524979-7023378453087010001?l=tremordeterra.blogspot.com' alt='' /&gt;&lt;/div&gt;
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&lt;br /&gt;
&lt;br /&gt;
O horário de Brasília por volta 16:48 (provavelmente na Avenida Paulista tenha sentido também)&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/8683684774032524979-4363882802793242047?l=tremordeterra.blogspot.com' alt='' /&gt;&lt;/div&gt;
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&lt;a href="http://feedads.g.doubleclick.net/~a/qZ3kwOZGqvK3UJfMT4iIUVk4JlE/1/da"&gt;&lt;img src="http://feedads.g.doubleclick.net/~a/qZ3kwOZGqvK3UJfMT4iIUVk4JlE/1/di" border="0" ismap="true"&gt;&lt;/img&gt;&lt;/a&gt;&lt;/p&gt;&lt;img src="http://feeds.feedburner.com/~r/blogspot/surOo/~4/5g961m-BjaE" height="1" width="1"/&gt;</content><link rel="replies" type="application/atom+xml" href="http://tremordeterra.blogspot.com/feeds/4363882802793242047/comments/default" title="Postar comentários" /><link rel="replies" type="text/html" href="http://tremordeterra.blogspot.com/2011/11/tremor-de-62-na-bolivia-tem-reflexo-em.html#comment-form" title="0 Comentários" /><link rel="edit" type="application/atom+xml" href="http://www.blogger.com/feeds/8683684774032524979/posts/default/4363882802793242047?v=2" /><link rel="self" type="application/atom+xml" href="http://www.blogger.com/feeds/8683684774032524979/posts/default/4363882802793242047?v=2" /><link rel="alternate" type="text/html" href="http://feedproxy.google.com/~r/blogspot/surOo/~3/5g961m-BjaE/tremor-de-62-na-bolivia-tem-reflexo-em.html" title="Tremor de 6.2 na Bolívia tem reflexo em Campinas, Brasília e Rondônia" /><author><name>Prof.  George Sand França (Universidade de Brasília)</name><uri>http://www.blogger.com/profile/13658186359698780690</uri><email>noreply@blogger.com</email><gd:image rel="http://schemas.google.com/g/2005#thumbnail" width="32" height="24" src="http://bp0.blogger.com/_YWldrkTV_x8/R_ho6CYm-WI/AAAAAAAABas/e3S7LPid2TU/S220/mar%C3%A7o2008+015.jpg" /></author><thr:total>0</thr:total><feedburner:origLink>http://tremordeterra.blogspot.com/2011/11/tremor-de-62-na-bolivia-tem-reflexo-em.html</feedburner:origLink></entry><entry gd:etag="W/&quot;DkEFR3k6fCp7ImA9WhRREEw.&quot;"><id>tag:blogger.com,1999:blog-8683684774032524979.post-1774965375285895828</id><published>2011-11-23T00:08:00.002-02:00</published><updated>2011-11-23T00:16:56.714-02:00</updated><app:edited xmlns:app="http://www.w3.org/2007/app">2011-11-23T00:16:56.714-02:00</app:edited><title>EMSC - Informa um tremor de magnitude 5.8 no MT à 128 km de Aripuanã! Será?</title><content type="html">Incrível, mas hoje tremeu em Mato Grosso de acordo com Centro Sismológico Europeu (EMSC) e não confirmado! Esse seria o maior tremor de terra do Brasil desse século. Será? &lt;br /&gt;
&lt;br /&gt;
Para um tremor nessa magnitude, certamente já teríamos notícias de Mato Grosso. Espero que EMSC esteja errado e o Serviço Geológico Americano (USGS) esteja correto, pois não notificou tal evento e nem o Observatório Sismológico (Eu irei ver isso amanhã). &lt;br /&gt;
&lt;br /&gt;
&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://4.bp.blogspot.com/-UkyHeUlkXTY/TsxVjXJS7vI/AAAAAAAAGpo/05_mo372fRM/s1600/245578.local.jpg" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"&gt;&lt;img border="0" height="266" src="http://4.bp.blogspot.com/-UkyHeUlkXTY/TsxVjXJS7vI/AAAAAAAAGpo/05_mo372fRM/s320/245578.local.jpg" width="320" /&gt;&lt;/a&gt;&lt;/div&gt;Caso confirme o erro, percebemos que EMSC não está ainda consolidado para regiões estáveis.&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
informações do EMSC abaixo&lt;br /&gt;
Magnitude&amp;nbsp;5.8&lt;br /&gt;
RegionMATO GROSSO, BRAZIL&lt;br /&gt;
Date time2011-11-22   18:57:40.5 UTC&lt;br /&gt;
Location9.96 S ; 59.79 W&lt;br /&gt;
Depth33 km&lt;br /&gt;
Distances258 km NE Ji-paraná  (pop 100,118 ; local time 14:57:40.5 2011-11-22)&lt;br /&gt;
128 km SE Aripuanã  (pop 26,983 ; local time 15:57:40.5 2011-11-22)&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/8683684774032524979-1774965375285895828?l=tremordeterra.blogspot.com' alt='' /&gt;&lt;/div&gt;
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&lt;a href="http://feedads.g.doubleclick.net/~a/uBvCNqABHu4iIRg65ey5uXsqrZ0/1/da"&gt;&lt;img src="http://feedads.g.doubleclick.net/~a/uBvCNqABHu4iIRg65ey5uXsqrZ0/1/di" border="0" ismap="true"&gt;&lt;/img&gt;&lt;/a&gt;&lt;/p&gt;&lt;img src="http://feeds.feedburner.com/~r/blogspot/surOo/~4/PwoOhZ-m-9U" height="1" width="1"/&gt;</content><link rel="replies" type="application/atom+xml" href="http://tremordeterra.blogspot.com/feeds/1774965375285895828/comments/default" title="Postar comentários" /><link rel="replies" type="text/html" href="http://tremordeterra.blogspot.com/2011/11/emsc-informa-um-tremor-de-magnitude-58.html#comment-form" title="6 Comentários" /><link rel="edit" type="application/atom+xml" href="http://www.blogger.com/feeds/8683684774032524979/posts/default/1774965375285895828?v=2" /><link rel="self" type="application/atom+xml" href="http://www.blogger.com/feeds/8683684774032524979/posts/default/1774965375285895828?v=2" /><link rel="alternate" type="text/html" href="http://feedproxy.google.com/~r/blogspot/surOo/~3/PwoOhZ-m-9U/emsc-informa-um-tremor-de-magnitude-58.html" title="EMSC - Informa um tremor de magnitude 5.8 no MT à 128 km de Aripuanã! Será?" /><author><name>Prof.  George Sand França (Universidade de Brasília)</name><uri>http://www.blogger.com/profile/13658186359698780690</uri><email>noreply@blogger.com</email><gd:image rel="http://schemas.google.com/g/2005#thumbnail" width="32" height="24" src="http://bp0.blogger.com/_YWldrkTV_x8/R_ho6CYm-WI/AAAAAAAABas/e3S7LPid2TU/S220/mar%C3%A7o2008+015.jpg" /></author><media:thumbnail xmlns:media="http://search.yahoo.com/mrss/" url="http://4.bp.blogspot.com/-UkyHeUlkXTY/TsxVjXJS7vI/AAAAAAAAGpo/05_mo372fRM/s72-c/245578.local.jpg" height="72" width="72" /><thr:total>6</thr:total><feedburner:origLink>http://tremordeterra.blogspot.com/2011/11/emsc-informa-um-tremor-de-magnitude-58.html</feedburner:origLink></entry><entry gd:etag="W/&quot;DUUFQXs7fip7ImA9WhRSFEQ.&quot;"><id>tag:blogger.com,1999:blog-8683684774032524979.post-7830351571961488610</id><published>2011-11-17T00:31:00.002-02:00</published><updated>2011-11-17T00:33:30.506-02:00</updated><app:edited xmlns:app="http://www.w3.org/2007/app">2011-11-17T00:33:30.506-02:00</app:edited><title>Mitos e Lendas</title><content type="html">O terremoto ocorre:&lt;br /&gt;
&lt;blockquote class="tr_bq"&gt;&lt;ul&gt;&lt;li&gt;Quando um dos oito elefantes que transportam a Terra se cansa. (Hindu) &lt;/li&gt;
&lt;/ul&gt;&lt;/blockquote&gt;&lt;blockquote class="tr_bq"&gt;&lt;ul&gt;&lt;li&gt;Quando o sapo, que segura a terra, se move. (Mongolia)&lt;/li&gt;
&lt;/ul&gt;&lt;/blockquote&gt;&lt;blockquote class="tr_bq"&gt;&lt;ul&gt;&lt;li&gt;Quando o gigante em que vivemos sobre sua cabeça, espirra ou coça (Africa)&lt;/li&gt;
&lt;/ul&gt;&lt;/blockquote&gt;&lt;blockquote class="tr_bq"&gt;&lt;ul&gt;&lt;li&gt;&lt;span class="" id="result_box" lang="pt"&gt;&lt;span class="hps"&gt;Quando&lt;/span&gt; &lt;span class="hps"&gt;a atenção do&lt;/span&gt; &lt;span class="hps"&gt;Deus Kashima&lt;/span&gt; &lt;span class="hps atn"&gt;(&lt;/span&gt;&lt;span class=""&gt;que cuida do&lt;/span&gt; peixe gigante &lt;span class="hps"&gt;Namazu&lt;/span&gt;&lt;span class="hps"&gt; &lt;/span&gt;&lt;span class="hps"&gt;que suporta&lt;/span&gt; &lt;span class="hps"&gt;a Terra&lt;/span&gt; &lt;span class="hps"&gt;e impede &lt;/span&gt;&lt;span class="hps"&gt;ela de afundar&lt;/span&gt; &lt;span class="hps"&gt;no oceano&lt;/span&gt;) &lt;span class="hps"&gt;enfraquece&lt;/span&gt; &lt;span class="hps"&gt;e Namazu move&lt;/span&gt; &lt;span class="hps"&gt;&lt;/span&gt;&lt;span class="hps"&gt;(Japão)&lt;/span&gt;&lt;/span&gt;&lt;/li&gt;
&lt;/ul&gt;&lt;/blockquote&gt;&lt;br /&gt;
&lt;br /&gt;
&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://4.bp.blogspot.com/-QByeT12-F50/TsRuv05mPTI/AAAAAAAAGpU/mei1v9mnTO8/s1600/lixo.png" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"&gt;&lt;img border="0" height="400" src="http://4.bp.blogspot.com/-QByeT12-F50/TsRuv05mPTI/AAAAAAAAGpU/mei1v9mnTO8/s400/lixo.png" width="280" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;br /&gt;
&lt;ul&gt;&lt;li&gt;&lt;span class="" id="result_box" lang="pt"&gt;&lt;span class="hps"&gt;Quando o&lt;/span&gt; &lt;span class="hps"&gt;Deus&lt;/span&gt; &lt;span class="hps"&gt;Maimas&lt;/span&gt; &lt;span class="hps"&gt;decide&lt;/span&gt; &lt;span class="hps"&gt;contar a população&lt;/span&gt; no Peru e &lt;span class="hps"&gt;&lt;/span&gt;&lt;span class="hps"&gt;seus passos&lt;/span&gt; &lt;span class="hps"&gt;&lt;/span&gt;&lt;span class="hps"&gt;sacodem a terra&lt;/span&gt;. &lt;span class="hps"&gt;Em seguida,&lt;/span&gt; os nativos &lt;span class="hps"&gt;correm de suas casas e gritam &lt;/span&gt;&lt;span class="hps"&gt;&lt;/span&gt;&lt;span class="hps"&gt;&lt;/span&gt;: "Eu &lt;span class="hps"&gt;estou aqui&lt;/span&gt;&lt;span class=""&gt;, estou aqui&lt;/span&gt;!"&amp;nbsp;&lt;/span&gt;&lt;/li&gt;
&lt;/ul&gt;&lt;span class="" id="result_box" lang="pt"&gt;Tirados de livros de Sismologia.&amp;nbsp; &lt;/span&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/8683684774032524979-7830351571961488610?l=tremordeterra.blogspot.com' alt='' /&gt;&lt;/div&gt;
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&lt;tr align="center"&gt;&lt;td style="background: url(&amp;quot;https://picasaweb.google.com/s/c/transparent_album_background.gif&amp;quot;) no-repeat scroll left center transparent; height: 194px;"&gt;&lt;a href="https://picasaweb.google.com/georgefranca/MostraSismologica2010?authuser=0&amp;amp;feat=embedwebsite"&gt;&lt;img height="160" src="https://lh5.googleusercontent.com/-9ZDb7t7gWNY/TH1xkdwj0NE/AAAAAAAAGFI/0ugDH6RxtEs/s160-c/MostraSismologica2010.jpg" style="margin: 1px 0 0 4px;" width="160" /&gt;&lt;/a&gt;&lt;/td&gt;&lt;/tr&gt;
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&amp;lt;&lt;br /&gt;
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&lt;/h3&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/8683684774032524979-3506874753096280587?l=tremordeterra.blogspot.com' alt='' /&gt;&lt;/div&gt;
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&lt;br /&gt;
&amp;nbsp;Um estação sismográfica somente não adianta para estudar essa atividade, precisa rapidamente (atividade atenua com os dias)&amp;nbsp; de uma equipe e instalar uma rede com mínimo 6 estações para entender essa atividade. Entretanto, não tem como impedi que esses tremores parem de acontecem.&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
Abraços&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/8683684774032524979-7578433684701444185?l=tremordeterra.blogspot.com' alt='' /&gt;&lt;/div&gt;
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