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<?xml-stylesheet href="/style/rss/rss_feed.xsl" type="text/xsl" media="screen"?><?xml-stylesheet href="/style/rss/rss_feed.css" type="text/css" media="screen" ?><rss version="2.0"><channel><title>Clipmarks | Volcanoes Clips</title><link>http://clipmarks.com/tags/volcanoes/</link><feedUrl>http://rss.clipmarks.com/tags/volcanoes/</feedUrl><ttl>15</ttl><description>Clip, tag and save information that's important to you. Bookmarks save entire pages...Clipmarks save the specific content that matters to you!</description><language>en-us</language><item><title>30 Examples of Things by Lava and Ash (pics)</title><link>http://clipmarks.com/clipmark/D3A311D7-FC58-47B2-8D19-EA75A95660C2/</link><description>&lt;b&gt;clipped by:&lt;/b&gt; &lt;a href="http://clipmarks.com/clipper/digitalfever/"&gt;digitalfever&lt;/a&gt;&lt;br&gt;&lt;div border="2" style="margin-top: 10px; border:#000000 1px solid;" width="90%"&gt;&lt;div style="background-color:"&gt;&lt;div align="center" width="100%" style="padding:4px;margin-bottom:4px;background-color:#666666;overflow:hidden;"&gt;&lt;span style="color:#FFFFFF;font-weight:bold;"&gt;Clip Source: &lt;a style="color:#FFFFFF;" href="http://www.environmentalgraffiti.com/featured/30-objects-swallowed-lava-and-pyroclastic-ash/1716" title="http://www.environmentalgraffiti.com/featured/30-objects-swallowed-lava-and-pyroclastic-ash/1716"&gt;www.environmentalgraffiti.com&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/digitalfever/512/DCD2C35B-A184-4125-8E1D-9F68CF167CB3.jpg" alt="Soufriere Hills, Monserrat" /&gt;&lt;br /&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;P&gt;There must be few things more frightening than being caught up in the deadly path of an all-absorbing lava flow. Imagine the intense heat, being spattered with skin-scalding magma that’s erupting from the depths beneath or being covered in blistering hot ash spewed forth from the gaping mouth of the giant fiery furnace.&lt;/P&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;P&gt;We’ve unearthed some fascinating images of the devastation and destruction caused by the devouring nature of eruptive volcanoes. We hope you’ll agree they make for compulsive viewing.&lt;/P&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;br&gt;&lt;div style="margin-bottom: 40px;"&gt;Tags: &lt;a href="http://clipmarks.com/tags/hawaii+lava+roads/" rel="tag"&gt;hawaii lava roads&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/lava+beds/" rel="tag"&gt;lava beds&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/lava+flows/" rel="tag"&gt;lava flows&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/lava+flows+ocean/" rel="tag"&gt;lava flows ocean&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/molten+lava/" rel="tag"&gt;molten lava&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/mount+etna/" rel="tag"&gt;mount etna&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/mount+pinatubo/" rel="tag"&gt;mount pinatubo&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/pompeii+volcano/" rel="tag"&gt;pompeii volcano&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/pyroclastic+ash+falls/" rel="tag"&gt;pyroclastic ash falls&lt;/a&gt;&lt;/div&gt;</description><clipSource>http://www.environmentalgraffiti.com/featured/30-objects-swallowed-lava-and-pyroclastic-ash/1716</clipSource><pubDate>Thu, 04 Sep 2008 13:43:55 GMT</pubDate></item><item><title>what lives in a 'lost world' five kilometres beneath the Caribbean?.</title><link>http://clipmarks.com/clipmark/B6471A88-2882-4048-AAA3-16DFE75432D2/</link><description>&lt;b&gt;clipped by:&lt;/b&gt; &lt;a href="http://clipmarks.com/clipper/einbar/"&gt;einbar&lt;/a&gt;&lt;br&gt;&lt;div border="2" style="margin-top: 10px; border:#000000 1px solid;" width="90%"&gt;&lt;div style="background-color:"&gt;&lt;div align="center" width="100%" style="padding:4px;margin-bottom:4px;background-color:#666666;overflow:hidden;"&gt;&lt;span style="color:#FFFFFF;font-weight:bold;"&gt;Clip Source: &lt;a style="color:#FFFFFF;" href="http://www.sciencedaily.com/releases/2008/08/080830211000.htm" title="http://www.sciencedaily.com/releases/2008/08/080830211000.htm"&gt;www.sciencedaily.com&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/einbar/512/F3F0248A-4297-4680-BDF1-1C8A33A22CA0.jpg" alt="" /&gt;&lt;br /&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;Scientists at the National Oceanography Centre, Southampton, are set to explore the world's deepest undersea volcanoes and find out what lives in a 'lost world' five kilometres beneath the Caribbean.&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;P&gt;The team of researchers led by Dr Jon Copley has been awarded £462,000 by the Natural Environment Research Council to explore the Cayman Trough, which lies between Jamaica and the Cayman Islands. This rift in the Caribbean seafloor plunges to a depth of more than 5000 metres below sea level. It contains the world's deepest chain of undersea volcanoes, which have yet to be explored.&lt;/P&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;P&gt;"The deep ocean is the largest ecosystem on our planet, so we need to understand its patterns of life," says Dr Copley. "Deep-sea exploration has also given us new cancer treatments and better fibre-optic cables for the internet, both thanks to deep-sea creatures."&lt;/P&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;"The Cayman Trough may be a 'lost world' that will give us the missing piece in a global puzzle of deep-sea life," &lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;br&gt;&lt;div style="margin-bottom: 40px;"&gt;&lt;/div&gt;</description><clipSource>http://www.sciencedaily.com/releases/2008/08/080830211000.htm</clipSource><pubDate>Wed, 03 Sep 2008 06:41:24 GMT</pubDate></item><item><title>20 Most Incredible Volcanic Satellite Images</title><link>http://clipmarks.com/clipmark/C41713A8-B5C8-4468-B068-B6655928FC9D/</link><description>&lt;b&gt;clipped by:&lt;/b&gt; &lt;a href="http://clipmarks.com/clipper/digitalfever/"&gt;digitalfever&lt;/a&gt;&lt;br&gt;&lt;div border="2" style="margin-top: 10px; border:#000000 1px solid;" width="90%"&gt;&lt;div style="background-color:"&gt;&lt;div align="center" width="100%" style="padding:4px;margin-bottom:4px;background-color:#666666;overflow:hidden;"&gt;&lt;span style="color:#FFFFFF;font-weight:bold;"&gt;Clip Source: &lt;a style="color:#FFFFFF;" href="http://www.environmentalgraffiti.com/featured/20-most-incredible-volcanic-satellite-images/2081" title="http://www.environmentalgraffiti.com/featured/20-most-incredible-volcanic-satellite-images/2081"&gt;www.environmentalgraffiti.com&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/digitalfever/512/10BBA3D7-0FF9-4C48-8412-0F2B9C304836.jpg" alt="Mount Vesuvius" /&gt;&lt;br /&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;P&gt;Few things in nature are as unpredictable as the majestic volcano. Unleashing billowing ash, &lt;A href="http://www.environmentalgraffiti.com/featured/30-objects-swallowed-lava-and-pyroclastic-ash/1716"&gt;lava&lt;/A&gt; and &lt;A href="http://www.environmentalgraffiti.com/featured/30-objects-swallowed-lava-and-pyroclastic-ash/1716"&gt;pyroclastic flows&lt;/A&gt; when the Earth’s tectonics plates push and shove at each other like bullies in a playground, volcanoes are testament to the devastating and deadly forces of nature. Their power and might have seen them worshipped in the past, feared always and trusted, never, yet we still are drawn by their beauty, even in the face of destruction.&lt;/P&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;P&gt;We’ve unearthed some of NASA’s best satellite images of volcanoes from around the world, revealing the other side of these fiery demons. Their allure remains uncanny but not unsurprising.&lt;/P&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;br&gt;&lt;div style="margin-bottom: 40px;"&gt;Tags: &lt;a href="http://clipmarks.com/tags/volcano/" rel="tag"&gt;volcano&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/nasa+images/" rel="tag"&gt;nasa images&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/satellite+images/" rel="tag"&gt;satellite images&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/american+volanoes/" rel="tag"&gt;american volanoes&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/asian+volcanoes/" rel="tag"&gt;asian volcanoes&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/lava/" rel="tag"&gt;lava&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/african+volcanoes/" rel="tag"&gt;african volcanoes&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/ash/" rel="tag"&gt;ash&lt;/a&gt;&lt;/div&gt;</description><clipSource>http://www.environmentalgraffiti.com/featured/20-most-incredible-volcanic-satellite-images/2081</clipSource><pubDate>Tue, 02 Sep 2008 09:20:17 GMT</pubDate></item><item><title>Spectacular Chile Volcano Eruption</title><link>http://clipmarks.com/clipmark/E405FA0E-0778-46E1-8095-BF6F50AAC305/</link><description>&lt;b&gt;clipped by:&lt;/b&gt; &lt;a href="http://clipmarks.com/clipper/Smoke+TNT/"&gt;Smoke TNT&lt;/a&gt;&lt;br&gt;&lt;div border="2" style="margin-top: 10px; border:#000000 1px solid;" width="90%"&gt;&lt;div style="background-color:"&gt;&lt;div align="center" width="100%" style="padding:4px;margin-bottom:4px;background-color:#666666;overflow:hidden;"&gt;&lt;span style="color:#FFFFFF;font-weight:bold;"&gt;Clip Source: &lt;a style="color:#FFFFFF;" href="http://mysterytopia.com/2008/08/spectacular-chile-volcano-eruption.html" title="http://mysterytopia.com/2008/08/spectacular-chile-volcano-eruption.html"&gt;mysterytopia.com&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;DIV&gt;&lt;SPAN&gt;&lt;SPAN&gt;&lt;SPAN&gt;&lt;DIV&gt;Nature still has the  best special effects....&lt;/DIV&gt;
&lt;BR /&gt;
Chile Volcano eruption!!&lt;BR /&gt;
Several  weeks ago, a volcano that had been dormant for 9,000 years near  the&lt;BR /&gt;
coast of Chile erupted spectacularly, hurling  liquefied rocks many miles&lt;BR /&gt;
into the sky with lightning. The  results, which you see here, are called a&lt;BR /&gt;&lt;DIV&gt;
'dirty thunderstorm,' and are  quite rare.&lt;/DIV&gt;
&lt;BR /&gt;
Nobody is certain what causes them, but according to  National Geographic&lt;BR /&gt;
it's believed to be 'the result of rock fragments,  ash, and ice particles in&lt;BR /&gt;
the plume colliding to produce static  charges-just as ice particles collide&lt;BR /&gt;
to create charges in regular  thunderstorms.'&lt;/SPAN&gt;&lt;/SPAN&gt;&lt;/SPAN&gt;&lt;BR /&gt;
&lt;BR /&gt;
&lt;/DIV&gt;&lt;DIV class="separator"&gt;&lt;A imageanchor="1" href="http://1.bp.blogspot.com/_-TskqTch9MQ/SLAsSXstuVI/AAAAAAAAB4w/C-tWH7i-D3o/s1600-h/1.jpg"&gt;&lt;IMG border="0" src="http://1.bp.blogspot.com/_-TskqTch9MQ/SLAsSXstuVI/AAAAAAAAB4w/WlxOdq3PU5U/s400-R/1.jpg" /&gt;&lt;/A&gt; &lt;/DIV&gt;&lt;DIV class="separator"&gt; &lt;A imageanchor="1" href="http://4.bp.blogspot.com/_-TskqTch9MQ/SLAsUS9wl_I/AAAAAAAAB44/4tHJw9freKQ/s1600-h/2.jpg"&gt;&lt;IMG border="0" src="http://4.bp.blogspot.com/_-TskqTch9MQ/SLAsUS9wl_I/AAAAAAAAB44/9Oxz39ONLtg/s400-R/2.jpg" /&gt;&lt;/A&gt; &lt;/DIV&gt;&lt;DIV class="separator"&gt; &lt;A imageanchor="1" href="http://4.bp.blogspot.com/_-TskqTch9MQ/SLAsWcsEOxI/AAAAAAAAB5A/pFRnJbs8ZhY/s1600-h/3.jpg"&gt;&lt;IMG border="0" src="http://4.bp.blogspot.com/_-TskqTch9MQ/SLAsWcsEOxI/AAAAAAAAB5A/D21fShb_8tI/s400-R/3.jpg" /&gt;&lt;/A&gt; &lt;/DIV&gt;&lt;DIV class="separator"&gt; &lt;A imageanchor="1" href="http://3.bp.blogspot.com/_-TskqTch9MQ/SLAsYkMa1qI/AAAAAAAAB5I/wDpLwqgmW-o/s1600-h/4.jpg"&gt;&lt;IMG border="0" src="http://3.bp.blogspot.com/_-TskqTch9MQ/SLAsYkMa1qI/AAAAAAAAB5I/AA3IMUW5IZ0/s400-R/4.jpg" /&gt;&lt;/A&gt; &lt;/DIV&gt;&lt;DIV class="separator"&gt; &lt;A imageanchor="1" href="http://4.bp.blogspot.com/_-TskqTch9MQ/SLAsazzq7gI/AAAAAAAAB5Q/sLwnJiBMeYs/s1600-h/5.jpg"&gt;&lt;IMG border="0" src="http://4.bp.blogspot.com/_-TskqTch9MQ/SLAsazzq7gI/AAAAAAAAB5Q/Ceec5_8DUaA/s400-R/5.jpg" /&gt;&lt;/A&gt; &lt;/DIV&gt;&lt;DIV class="separator"&gt; &lt;A imageanchor="1" href="http://1.bp.blogspot.com/_-TskqTch9MQ/SLAsdjMwPnI/AAAAAAAAB5Y/9_S-amlCs3I/s1600-h/6.jpg"&gt;&lt;IMG border="0" src="http://1.bp.blogspot.com/_-TskqTch9MQ/SLAsdjMwPnI/AAAAAAAAB5Y/IKdg14knkY8/s400-R/6.jpg" /&gt;&lt;/A&gt;&lt;/DIV&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;br&gt;&lt;div style="margin-bottom: 40px;"&gt;Tags: &lt;a href="http://clipmarks.com/tags/science/" rel="tag"&gt;science&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/volcanoes/" rel="tag"&gt;volcanoes&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/chile/" rel="tag"&gt;chile&lt;/a&gt;&lt;/div&gt;</description><clipSource>http://mysterytopia.com/2008/08/spectacular-chile-volcano-eruption.html</clipSource><pubDate>Sun, 24 Aug 2008 10:09:11 GMT</pubDate></item><item><title>The Mars Webcam</title><link>http://clipmarks.com/clipmark/ACAC543E-9650-440A-9D33-6BDBD45563B9/</link><description>&lt;b&gt;clipped by:&lt;/b&gt; &lt;a href="http://clipmarks.com/clipper/sahara/"&gt;sahara&lt;/a&gt;&lt;br&gt;&lt;b&gt;clipper's remarks:&lt;/b&gt;   The VMC is operated by the Mars Express Flight Control Team, based at ESOC, Darmstadt, Germany. This activity is conducted on a 'best-effort, last-priority' basis given the availability of planning time, command upload time and data down-link capacity.&lt;br/&gt;&lt;br/&gt;This is a unique situation, as Flight Control Teams for ESA missions usually do not 'operate' payload instruments; this is done by dedicated, specialised science teams. But the VMC is different: it had a purely operational purpose (successfully completed in 2003 with Beagle's separation) and as such it is not operated by scientists, but by flight controllers.  &lt;br&gt;&lt;div border="2" style="margin-top: 10px; border:#000000 1px solid;" width="90%"&gt;&lt;div style="background-color:"&gt;&lt;div align="center" width="100%" style="padding:4px;margin-bottom:4px;background-color:#666666;overflow:hidden;"&gt;&lt;span style="color:#FFFFFF;font-weight:bold;"&gt;Clip Source: &lt;a style="color:#FFFFFF;" href="http://www.esa.int/SPECIALS/VMC/SEMZVSXIPIF_mg_1.html" title="http://www.esa.int/SPECIALS/VMC/SEMZVSXIPIF_mg_1.html"&gt;www.esa.int&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;P id="gallabs"&gt;A gallery of the best images captured by the Mars Express Visual Monitoring Camera (VMC) during testing and optimisation in 2007. The selection includes a crescent Mars, Mars' rotation and views of the Red Planet's 'volcano family' (we've also included a few images taken by the VMC in 2003).&lt;/P&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;table background="undefined" bgcolor=""&gt;&lt;tr&gt;&lt;TD class="pleft"&gt; &lt;A href="http://www.esa.int/SPECIALS/VMC/SEMZVSXIPIF_mg_1_s.html" class="imgwram"&gt;&lt;SPAN&gt; &lt;SPAN&gt;&lt;/SPAN&gt;&lt;IMG width="120" height="89" alt="" src="http://www.esa.int/SPECIALS/VMC/../../images/07-152_014330_01_small,0.png" /&gt;&lt;/SPAN&gt;&lt;/A&gt;&lt;DIV class="tosingle"&gt;&lt;A href="http://www.esa.int/SPECIALS/VMC/SEMZVSXIPIF_mg_1_s.html" class="ico"&gt;&lt;IMG width="34" height="16" alt="info" src="http://www.esa.int/SPECIALS/VMC/../../global_imgs/infoo1.gif" /&gt;&lt;/A&gt;&lt;A href="http://www.esa.int/SPECIALS/VMC/SEMZVSXIPIF_mg_1_s_b.html" class="ico"&gt;&lt;IMG width="34" height="16" alt="view" src="http://www.esa.int/SPECIALS/VMC/../../global_imgs/lview1.gif" /&gt;&lt;/A&gt;&lt;A target="download" href="http://www.esa.int/images/07-152_014330_01.png" class="lh1"&gt;&lt;IMG width="10" height="16" alt="hires" src="http://www.esa.int/SPECIALS/VMC/../../global_imgs/arw10wh.gif" /&gt;&lt;SPAN&gt;Hi-res&lt;/SPAN&gt;&lt;/A&gt;&lt;/DIV&gt;&lt;DIV class="caption"&gt;Sunburst at Mars 1 Jun 2007&lt;/DIV&gt; &lt;/TD&gt;&lt;/tr&gt;&lt;/table&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;table background="undefined" bgcolor=""&gt;&lt;tr&gt;&lt;TD&gt; &lt;A href="http://www.esa.int/SPECIALS/VMC/SEMZVSXIPIF_mg_2_s.html" class="imgwram"&gt;&lt;SPAN&gt; &lt;SPAN&gt;&lt;/SPAN&gt;&lt;IMG width="120" height="120" alt="" src="http://www.esa.int/SPECIALS/VMC/../../images/MTP_44_Rotation_ani_sq.gif" /&gt;&lt;/SPAN&gt;&lt;/A&gt;&lt;DIV class="tosingle"&gt;&lt;A href="http://www.esa.int/SPECIALS/VMC/SEMZVSXIPIF_mg_2_s.html" class="ico"&gt;&lt;IMG width="34" height="16" alt="info" src="http://www.esa.int/SPECIALS/VMC/../../global_imgs/infoo1.gif" /&gt;&lt;/A&gt;&lt;A href="http://www.esa.int/SPECIALS/VMC/SEMZVSXIPIF_mg_2_s_b.html" class="ico"&gt;&lt;IMG width="34" height="16" alt="view" src="http://www.esa.int/SPECIALS/VMC/../../global_imgs/lview1.gif" /&gt;&lt;/A&gt;&lt;A target="download" href="http://www.esa.int/images/MTP_44_Rotation_ani.gif" class="lh1"&gt;&lt;IMG width="10" height="16" alt="hires" src="http://www.esa.int/SPECIALS/VMC/../../global_imgs/arw10wh.gif" /&gt;&lt;SPAN&gt;Hi-res&lt;/SPAN&gt;&lt;/A&gt;&lt;/DIV&gt;&lt;DIV class="caption"&gt;Mars rotation 12 Sep - 8 Oct 2007&lt;/DIV&gt; &lt;/TD&gt;&lt;/tr&gt;&lt;/table&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;table background="undefined" bgcolor=""&gt;&lt;tr&gt;&lt;TD class="pright"&gt; &lt;A href="http://www.esa.int/SPECIALS/VMC/SEMZVSXIPIF_mg_3_s.html" class="imgwram"&gt;&lt;SPAN&gt; &lt;SPAN&gt;&lt;/SPAN&gt;&lt;IMG width="90" height="120" alt="" src="http://www.esa.int/SPECIALS/VMC/../../images/07-087_032615_29_small,0.png" /&gt;&lt;/SPAN&gt;&lt;/A&gt;&lt;DIV class="tosingle"&gt;&lt;A href="http://www.esa.int/SPECIALS/VMC/SEMZVSXIPIF_mg_3_s.html" class="ico"&gt;&lt;IMG width="34" height="16" alt="info" src="http://www.esa.int/SPECIALS/VMC/../../global_imgs/infoo1.gif" /&gt;&lt;/A&gt;&lt;A href="http://www.esa.int/SPECIALS/VMC/SEMZVSXIPIF_mg_3_s_b.html" class="ico"&gt;&lt;IMG width="34" height="16" alt="view" src="http://www.esa.int/SPECIALS/VMC/../../global_imgs/lview1.gif" /&gt;&lt;/A&gt;&lt;A target="download" href="http://www.esa.int/images/07-087_032615_29.png" class="lh1"&gt;&lt;IMG width="10" height="16" alt="hires" src="http://www.esa.int/SPECIALS/VMC/../../global_imgs/arw10wh.gif" /&gt;&lt;SPAN&gt;Hi-res&lt;/SPAN&gt;&lt;/A&gt;&lt;/DIV&gt;&lt;DIV class="caption"&gt;First image of Mars volcanoes 23 Mar 2007&lt;/DIV&gt; &lt;/TD&gt;&lt;/tr&gt;&lt;/table&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;table background="undefined" bgcolor=""&gt;&lt;tr&gt;&lt;TD class="pleft"&gt; &lt;A href="http://www.esa.int/SPECIALS/VMC/SEMZVSXIPIF_mg_4_s.html" class="imgwram"&gt;&lt;SPAN&gt; &lt;SPAN&gt;&lt;/SPAN&gt;&lt;IMG width="120" height="89" alt="" src="http://www.esa.int/SPECIALS/VMC/../../images/07-358_115934_01_small,0.png" /&gt;&lt;/SPAN&gt;&lt;/A&gt;&lt;DIV class="tosingle"&gt;&lt;A href="http://www.esa.int/SPECIALS/VMC/SEMZVSXIPIF_mg_4_s.html" class="ico"&gt;&lt;IMG width="34" height="16" alt="info" src="http://www.esa.int/SPECIALS/VMC/../../global_imgs/infoo1.gif" /&gt;&lt;/A&gt;&lt;A href="http://www.esa.int/SPECIALS/VMC/SEMZVSXIPIF_mg_4_s_b.html" class="ico"&gt;&lt;IMG width="34" height="16" alt="view" src="http://www.esa.int/SPECIALS/VMC/../../global_imgs/lview1.gif" /&gt;&lt;/A&gt;&lt;A target="download" href="http://www.esa.int/images/07-358_115934_01.png" class="lh1"&gt;&lt;IMG width="10" height="16" alt="hires" src="http://www.esa.int/SPECIALS/VMC/../../global_imgs/arw10wh.gif" /&gt;&lt;SPAN&gt;Hi-res&lt;/SPAN&gt;&lt;/A&gt;&lt;/DIV&gt;&lt;DIV class="caption"&gt;'Family' view of the Martian volcanoes 11 Dec 2007&lt;/DIV&gt; &lt;/TD&gt;&lt;/tr&gt;&lt;/table&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;table background="undefined" bgcolor=""&gt;&lt;tr&gt;&lt;TD&gt; &lt;A href="http://www.esa.int/SPECIALS/VMC/SEMZVSXIPIF_mg_5_s.html" class="imgwram"&gt;&lt;SPAN&gt; &lt;SPAN&gt;&lt;/SPAN&gt;&lt;IMG width="120" height="89" alt="" src="http://www.esa.int/SPECIALS/VMC/../../images/07-288_170115_01_small,0.png" /&gt;&lt;/SPAN&gt;&lt;/A&gt;&lt;DIV class="tosingle"&gt;&lt;A href="http://www.esa.int/SPECIALS/VMC/SEMZVSXIPIF_mg_5_s.html" class="ico"&gt;&lt;IMG width="34" height="16" alt="info" src="http://www.esa.int/SPECIALS/VMC/../../global_imgs/infoo1.gif" /&gt;&lt;/A&gt;&lt;A href="http://www.esa.int/SPECIALS/VMC/SEMZVSXIPIF_mg_5_s_b.html" class="ico"&gt;&lt;IMG width="34" height="16" alt="view" src="http://www.esa.int/SPECIALS/VMC/../../global_imgs/lview1.gif" /&gt;&lt;/A&gt;&lt;A target="download" href="http://www.esa.int/images/07-288_170115_01.png" class="lh1"&gt;&lt;IMG width="10" height="16" alt="hires" src="http://www.esa.int/SPECIALS/VMC/../../global_imgs/arw10wh.gif" /&gt;&lt;SPAN&gt;Hi-res&lt;/SPAN&gt;&lt;/A&gt;&lt;/DIV&gt;&lt;DIV class="caption"&gt;First glimpse of Olympus Mons 15 Oct 2007&lt;/DIV&gt; &lt;/TD&gt;&lt;/tr&gt;&lt;/table&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;table background="undefined" bgcolor=""&gt;&lt;tr&gt;&lt;TD class="pright"&gt; &lt;A href="http://www.esa.int/SPECIALS/VMC/SEMZVSXIPIF_mg_6_s.html" class="imgwram"&gt;&lt;SPAN&gt; &lt;SPAN&gt;&lt;/SPAN&gt;&lt;IMG width="120" height="89" alt="" src="http://www.esa.int/SPECIALS/VMC/../../images/07-313_081858_01_small,0.png" /&gt;&lt;/SPAN&gt;&lt;/A&gt;&lt;DIV class="tosingle"&gt;&lt;A href="http://www.esa.int/SPECIALS/VMC/SEMZVSXIPIF_mg_6_s.html" class="ico"&gt;&lt;IMG width="34" height="16" alt="info" src="http://www.esa.int/SPECIALS/VMC/../../global_imgs/infoo1.gif" /&gt;&lt;/A&gt;&lt;A href="http://www.esa.int/SPECIALS/VMC/SEMZVSXIPIF_mg_6_s_b.html" class="ico"&gt;&lt;IMG width="34" height="16" alt="view" src="http://www.esa.int/SPECIALS/VMC/../../global_imgs/lview1.gif" /&gt;&lt;/A&gt;&lt;A target="download" href="http://www.esa.int/images/07-313_081858_01.png" class="lh1"&gt;&lt;IMG width="10" height="16" alt="hires" src="http://www.esa.int/SPECIALS/VMC/../../global_imgs/arw10wh.gif" /&gt;&lt;SPAN&gt;Hi-res&lt;/SPAN&gt;&lt;/A&gt;&lt;/DIV&gt;&lt;DIV class="caption"&gt;Olympus Mons face-on 9 Nov 2007&lt;/DIV&gt; &lt;/TD&gt;&lt;/tr&gt;&lt;/table&gt;&lt;/div&gt;&lt;/div&gt;&lt;div align="center" width="100%" style="padding:4px;margin-bottom:4px;background-color:#666666;overflow:hidden;"&gt;&lt;span style="color:#FFFFFF;font-weight:bold;"&gt;Clip Source: &lt;a style="color:#FFFFFF;" href="http://www.esa.int/SPECIALS/VMC/index.html" title="http://www.esa.int/SPECIALS/VMC/index.html"&gt;www.esa.int&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/sahara/512/E72EF68D-EAA7-4DBF-B92D-753D9A4BB527.png" alt="Mars Express VMC - the Mars Webcam" /&gt;&lt;br /&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;DIV&gt; &lt;SPAN class="datear"&gt;22 August 2008&lt;/SPAN&gt;   The Visual Monitoring Camera (VMC) is mounted on Mars Express, ESA's deep-space probe now orbiting the Red Planet. It originally provided simple, low-tech images of Beagle lander separation, and is now back in action as the 'Mars Webcam'. It's not a scientific instrument, but it does provide fantastic views of Mars - including crescent views of the planet not obtainable from Earth.&lt;/DIV&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;An ordinary camera in an extraordinary place&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;br&gt;&lt;div style="margin-bottom: 40px;"&gt;Tags: &lt;a href="http://clipmarks.com/tags/mars/" rel="tag"&gt;mars&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/science/" rel="tag"&gt;science&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/space/" rel="tag"&gt;space&lt;/a&gt;&lt;/div&gt;</description><clipSource>http://www.esa.int/SPECIALS/VMC/SEMZVSXIPIF_mg_1.html</clipSource><pubDate>Sat, 23 Aug 2008 01:45:51 GMT</pubDate></item><item><title>Volcanoes. Wow!</title><link>http://clipmarks.com/clipmark/C46EB1AF-4E47-46D8-ABA5-F17626466BF2/</link><description>&lt;b&gt;clipped by:&lt;/b&gt; &lt;a href="http://clipmarks.com/clipper/JohnWaterman/"&gt;JohnWaterman&lt;/a&gt;&lt;br&gt;&lt;b&gt;clipper's remarks:&lt;/b&gt;  Great Pics. &lt;br&gt;&lt;div border="2" style="margin-top: 10px; border:#000000 1px solid;" width="90%"&gt;&lt;div style="background-color:"&gt;&lt;div align="center" width="100%" style="padding:4px;margin-bottom:4px;background-color:#666666;overflow:hidden;"&gt;&lt;span style="color:#FFFFFF;font-weight:bold;"&gt;Clip Source: &lt;a style="color:#FFFFFF;" href="http://www.boston.com/bigpicture/2008/07/recent_volcanic_activity.html" title="http://www.boston.com/bigpicture/2008/07/recent_volcanic_activity.html"&gt;www.boston.com&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;H2&gt;&lt;A href="http://www.boston.com/bigpicture/2008/07/recent_volcanic_activity.html"&gt;Recent Volcanic Activity&lt;/A&gt;&lt;/H2&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;DIV class="bpBody"&gt;Several volcanoes have erupted in the past few months - two in Chile (Chaiten and Llaima) and one in Alaska (Okmok). At any given time, approximately 20 to 50 volcanoes are active worldwide (depending on the definition of "active"). Collected here are photos of volcanic events from the the past several years, seen from many angles, including low Earth Orbit. (&lt;A href="http://www.boston.com/bigpicture/2008/07/recent_volcanic_activity.html"&gt;15 photos total&lt;/A&gt;)&lt;/DIV&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/JohnWaterman/512/71B91101-BF0C-43BE-8D5C-C7DC5F80CD4E.jpg" alt="" /&gt;&lt;br /&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;Lava explodes from the Llaima volcano, one of Chile's most active volcanoes, in Cherquenco, Chile, early Thursday, July 10, 2008&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/JohnWaterman/512/9D61535E-42B1-4B8B-BFBC-129CF39FC9AE.jpg" alt="" /&gt;&lt;br /&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;Okmok Caldera in Alaska as viewed from an Alaska Airlines jet in early June, 2007. The 3,500-foot Okmok Caldera, which consists of a 6-mile-wide circular crater about 1,600 feet deep, erupted with little warning Saturday morning July 12, 2008&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/JohnWaterman/512/E47FABDE-5E57-478B-BF5D-A0A3D4447545.jpg" alt="" /&gt;&lt;br /&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;July 13, 2008&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;the Okmok Caldera erupting&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/JohnWaterman/512/0E7DB83E-1905-4E23-8D0E-97CDE6C1BEE8.jpg" alt="" /&gt;&lt;br /&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/JohnWaterman/512/C630BA3F-CFB5-446E-81AB-0BA274A348D8.jpg" alt="" /&gt;&lt;br /&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;Rabaul volcano, near Kokopo, Papua New Guinea on Sunday, April 13, 2008&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/JohnWaterman/512/C4679B16-7BC6-4D01-9D76-5888BF357741.jpg" alt="" /&gt;&lt;br /&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/JohnWaterman/512/8E4A0F2D-5410-42CD-9734-23FA40DCFA9E.jpg" alt="" /&gt;&lt;br /&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt; Mt. Etna's eruption on October 30th, 2002&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/JohnWaterman/512/980A21BC-EDFD-4F29-BB70-72E134431CD1.jpg" alt="" /&gt;&lt;br /&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;Mt Augustine&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt; 2006&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/JohnWaterman/512/7638B2EF-2FC8-4E24-B211-BB2312FBDD3D.jpg" alt="" /&gt;&lt;br /&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;Chaiten volcano&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;Chile&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;June 17, 2008&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/JohnWaterman/512/B5A836AE-5736-4B66-8B08-A72BF5E9E674.jpg" alt="" /&gt;&lt;br /&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt; Kliuchevskoi Volcano&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/JohnWaterman/512/F931AE64-1100-4D4E-8232-4DF117427EC9.jpg" alt="" /&gt;&lt;br /&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/JohnWaterman/512/635AF970-C7D7-483E-8130-2F93EC880544.jpg" alt="" /&gt;&lt;br /&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/JohnWaterman/512/0DE53217-F11F-4F68-85CC-37CEE96346E5.jpg" alt="" /&gt;&lt;br /&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/JohnWaterman/512/9514BA79-DE3F-4C9A-97DE-18D765DB23D2.jpg" alt="" /&gt;&lt;br /&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/JohnWaterman/512/EA8719F8-87C0-4F6D-ADEA-0CD1174F62DA.jpg" alt="" /&gt;&lt;br /&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;br&gt;&lt;div style="margin-bottom: 40px;"&gt;&lt;/div&gt;</description><clipSource>http://www.boston.com/bigpicture/2008/07/recent_volcanic_activity.html</clipSource><pubDate>Fri, 22 Aug 2008 16:35:08 GMT</pubDate></item><item><title>MarsCam: World's most distant webcam goes live</title><link>http://clipmarks.com/clipmark/7AF1EB2E-BE84-433F-8A00-C2909F873681/</link><description>&lt;b&gt;clipped by:&lt;/b&gt; &lt;a href="http://clipmarks.com/clipper/JohnWaterman/"&gt;JohnWaterman&lt;/a&gt;&lt;br&gt;&lt;div border="2" style="margin-top: 10px; border:#000000 1px solid;" width="90%"&gt;&lt;div style="background-color:"&gt;&lt;div align="center" width="100%" style="padding:4px;margin-bottom:4px;background-color:#666666;overflow:hidden;"&gt;&lt;span style="color:#FFFFFF;font-weight:bold;"&gt;Clip Source: &lt;a style="color:#FFFFFF;" href="http://blogs.discovermagazine.com/badastronomy/2008/08/22/worlds-most-distant-webcam-goes-live/" title="http://blogs.discovermagazine.com/badastronomy/2008/08/22/worlds-most-distant-webcam-goes-live/"&gt;blogs.discovermagazine.com&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;P&gt;You can use a webcam to sneak peeks at birds’ nests, active volcanoes, watch the Shuttle launch, and even to check traffic. But that’s just local stuff. What if you want more of a far look?&lt;/P&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;Then you need to check out the most distant webcam (so far) in the solar system: &lt;A target="_blank" href="http://www.esa.int/SPECIALS/VMC/index.html"&gt;the Mars Express Visual Monitoring Camera&lt;/A&gt; &lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/JohnWaterman/512/76CA0771-167E-432E-B952-0D1B018B2254.jpg" alt="The crescent Mars, as seen by MEVMC" /&gt;&lt;br /&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;This camera on board Europe’s Mars Express orbiter has been circling the red planet since 2003. It was used to confirm the Beagle lander’s separation from the main spacecraft, and that completed its main mission. But last year, controllers wondered if the camera could be turned back on to provide some tourist views of Mars, so they began a new campaign to check out the camera. It turned on just fine&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt; The image above shows something we never can see from Earth: a crescent Mars, with the Sun peeking over the limb (you need to have Mars between you and the Sun to see this, and Earth is always closer to the Sun than Mars)&lt;/div&gt;&lt;/div&gt;&lt;div align="center" width="100%" style="padding:4px;margin-bottom:4px;background-color:#666666;overflow:hidden;"&gt;&lt;span style="color:#FFFFFF;font-weight:bold;"&gt;Clip Source: &lt;a style="color:#FFFFFF;" href="http://www.esa.int/SPECIALS/VMC/index.html" title="http://www.esa.int/SPECIALS/VMC/index.html"&gt;www.esa.int&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;B&gt;The VMC: An ordinary camera in an extraordinary place!&lt;/B&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;br&gt;&lt;div style="margin-bottom: 40px;"&gt;&lt;/div&gt;</description><clipSource>http://blogs.discovermagazine.com/badastronomy/2008/08/22/worlds-most-distant-webcam-goes-live/</clipSource><pubDate>Fri, 22 Aug 2008 16:16:22 GMT</pubDate></item><item><title>Studying volcanoes with flying balloons :)</title><link>http://clipmarks.com/clipmark/4A6EABF7-1CAD-4E37-BBB7-F1ADCFBABA51/</link><description>&lt;b&gt;clipped by:&lt;/b&gt; &lt;a href="http://clipmarks.com/clipper/einbar/"&gt;einbar&lt;/a&gt;&lt;br&gt;&lt;b&gt;clipper's remarks:&lt;/b&gt;  "The balloons are piloted remotely by satellite link," Durant explained, "with flight visualization using Google Earth. We were looking at tropospheric volcanic emissions of sulfur dioxide, carbon dioxide and water, which can be hazardous to human and animal health and degrade ecosystems." &lt;br&gt;&lt;div border="2" style="margin-top: 10px; border:#000000 1px solid;" width="90%"&gt;&lt;div style="background-color:"&gt;&lt;div align="center" width="100%" style="padding:4px;margin-bottom:4px;background-color:#666666;overflow:hidden;"&gt;&lt;span style="color:#FFFFFF;font-weight:bold;"&gt;Clip Source: &lt;a style="color:#FFFFFF;" href="http://science.nationalgeographic.com/science/photos/volcano-general/volcventcarbon.html" title="http://science.nationalgeographic.com/science/photos/volcano-general/volcventcarbon.html"&gt;science.nationalgeographic.com&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/einbar/512/2A48A41A-E6B4-4087-9431-D9937B338B8A.jpg" alt="Photo: Carbon gas escapes from crust of volcanic vent, New Zealand" /&gt;&lt;br /&gt;&lt;/div&gt;&lt;div align="center" width="100%" style="padding:4px;margin-bottom:4px;background-color:#666666;overflow:hidden;"&gt;&lt;span style="color:#FFFFFF;font-weight:bold;"&gt;Clip Source: &lt;a style="color:#FFFFFF;" href="http://www.bio-medicine.org/biology-news-1/Studying-volcanoes-with-balloons-4467-1/" title="http://www.bio-medicine.org/biology-news-1/Studying-volcanoes-with-balloons-4467-1/"&gt;www.bio-medicine.org&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;P&gt;People do all kinds of crazy things in Hawaii, but flying balloons over a volcano usually isn't one of them. Unless you're Adam Durant, that is. &lt;/P&gt;
	&lt;P&gt;Durant, an adjunct geological sciences faculty member at Michigan Technological University, and colleagues took meteorological balloons to the Kilauea volcano this summer to make the first on-location measurements of volcanic gases as they actually spew from the mouth of the volcano. The Kilauea volcano began erupting in March.  &lt;/P&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;The first flight was a success and made the first in situ measurements of gases in a volcanic plume using meteorological balloons," Durant reported in a talk at Michigan Tech. &lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;P&gt;In addition to seeing volcanoes up closeDurant and his colleagues wear goggles and breathing masks at the infernal mouth of the volcanohe analyzes the plumes using controlled meteorological (CMET) balloons, which have altitude control and drift with winds.&lt;/P&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;br&gt;&lt;div style="margin-bottom: 40px;"&gt;&lt;/div&gt;</description><clipSource>http://science.nationalgeographic.com/science/photos/volcano-general/volcventcarbon.html</clipSource><pubDate>Sat, 16 Aug 2008 13:51:38 GMT</pubDate></item><item><title>Bizarre but true facts about the Earth</title><link>http://clipmarks.com/clipmark/C4115B64-A9D3-451C-9DDC-3E79BD5FFE27/</link><description>&lt;b&gt;clipped by:&lt;/b&gt; &lt;a href="http://clipmarks.com/clipper/swampfoxz/"&gt;swampfoxz&lt;/a&gt;&lt;br&gt;&lt;b&gt;clipper's remarks:&lt;/b&gt;  The oldest living tree is a California bristlecone pine name 'Methuselah'. It is about 4600 years old. The largest tree in the world is a giant sequoia growing in California. It is 84 meters tall and measures 29 meters round the trunk. The fastest growing tree is the eucalyptus. It can grow 10 meters a year.&lt;br/&gt;&lt;br/&gt;The Antartic notothenia fish has a protein in its blood that acts like antifreeze and stops the fish freezing in icy sea.&lt;br/&gt;&lt;br/&gt;The USA uses 29% of the world's petrol and 33% of the world's electricity.  &lt;br&gt;&lt;div border="2" style="margin-top: 10px; border:#000000 1px solid;" width="90%"&gt;&lt;div style="background-color:"&gt;&lt;div align="center" width="100%" style="padding:4px;margin-bottom:4px;background-color:#666666;overflow:hidden;"&gt;&lt;span style="color:#FFFFFF;font-weight:bold;"&gt;Clip Source: &lt;a style="color:#FFFFFF;" href="http://www.boomj.com/articles/14335" title="http://www.boomj.com/articles/14335"&gt;www.boomj.com&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;H1 class="article_title"&gt;Bizarre but true facts about the Earth &lt;/H1&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;DIV&gt;
			&lt;IMG width="190" height="150" alt="Bizarre but true facts about the Earth" src="http://www.boomj.com/html/images/lifestyle/042108/earthfacts.jpg" class="articleImg" /&gt;In 1783 an Icelandic eruption threw up enough dust to temporarily block out the sun over Europe. &lt;/DIV&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;DIV&gt;About 20 to 30 volcanoes erupt each year, mostly under the sea. &lt;/DIV&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/swampfoxz/512/0A08C49D-B23A-443A-B035-4B24A9CCF906.jpg" alt="Bizarre but true facts about the Earth" /&gt;&lt;br /&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;DIV&gt;A huge underground river runs underneath the Nile, with six times more water than the river above. &lt;/DIV&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;DIV&gt;Lake Bosumtwi in Ghana formed in a hollow made by a meteorite. &lt;/DIV&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;DIV&gt;Beaver Lake, in Yellowstone Park, USA, was artificially created by beaver damming. &lt;/DIV&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;DIV&gt;Off the coast of Florida there is an underwater hotel. Guests have to dive to the entrance. &lt;/DIV&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;DIV&gt;Venice in Italy is built on 118 sea islets joined by 400 bridges. It is gradually sinking into the water. &lt;/DIV&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;DIV&gt;The Ancient Egyptians worshipped a sky goddess called Nut.&lt;/DIV&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;DIV&gt;The world's windiest place is Commonwealth Bay, Antartica. &lt;/DIV&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;DIV&gt;In 1934, a gust of wind reached 371 km/h on Mount Washington in New Hampshire, USA. &lt;/DIV&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;DIV&gt;American Roy Sullivan has been struck by lighting a record seven times. &lt;/DIV&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;DIV&gt;The desert baobab tree can store up to 1000 litres of water in its trunk. &lt;/DIV&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;br&gt;&lt;div style="margin-bottom: 40px;"&gt;Tags: &lt;a href="http://clipmarks.com/tags/earth/" rel="tag"&gt;earth&lt;/a&gt;&lt;/div&gt;</description><clipSource>http://www.boomj.com/articles/14335</clipSource><pubDate>Sat, 16 Aug 2008 08:55:50 GMT</pubDate></item><item><title>Ice Volcanoes of Titan May Habor Life</title><link>http://clipmarks.com/clipmark/A3F61145-FDD9-4BA5-B75C-FD36F128BAAF/</link><description>&lt;b&gt;clipped by:&lt;/b&gt; &lt;a href="http://clipmarks.com/clipper/Mohir/"&gt;Mohir&lt;/a&gt;&lt;br&gt;&lt;b&gt;clipper's remarks:&lt;/b&gt;  For almost thirty years, scientists have known that complex carbon compounds called tholins exist on comets and in the atmospheres of the outer planets. Theoretically, tholins might interact with water in a process called hydrolysis to produce complex molecules similar to those found on the early Earth.&lt;br/&gt;&lt;br/&gt;Could tholins formed in Titan's atmosphere react with liquid water temporarily exposed by meteor impacts or ice volcanoes to produce potentially prebiotic complex organic molecules — before the water freezes?&lt;br/&gt;&lt;br/&gt;Laboratory research by Catherine Neish, a graduate student working on her doctorate in planetary science at the University of Arizona, suggests, not without controversy, however, that, over a period of days, compounds similar to tholins can be react with water at near-freezing temperatures.&lt;br/&gt; &lt;br&gt;&lt;div border="2" style="margin-top: 10px; border:#000000 1px solid;" width="90%"&gt;&lt;div style="background-color:"&gt;&lt;div align="center" width="100%" style="padding:4px;margin-bottom:4px;background-color:#666666;overflow:hidden;"&gt;&lt;span style="color:#FFFFFF;font-weight:bold;"&gt;Clip Source: &lt;a style="color:#FFFFFF;" href="http://www.dailygalaxy.com/my_weblog/2008/08/ice-volcanoes-o.html" title="http://www.dailygalaxy.com/my_weblog/2008/08/ice-volcanoes-o.html"&gt;www.dailygalaxy.com&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/Mohir/512/F4260687-6335-4FCE-BEC2-131C33A75553.jpg" alt="148105main_pia08427browse_4" /&gt;&lt;br /&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;
Titan, the sixth and largest moon of the planet Saturn, is thought
to be made largely of ice. Some of that ice may melt during meteor
impacts or in underground processes, producing "ice volcanoes" that
emit a "lava" containing ammonia mixed with water.&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;New observations of Titan by the Cassini spacecraft suggest the presence of cryovolcanism on the moon's surface. Cryovolcanism has important astrobiological implications, as it provides a means of exposing Titan's organics to liquid water, transforming hydrocarbons and nitriles into more evolved and oxidized prebiotic species.&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;P&gt;Ganesa Macula, a mountain on Titan, is 
believed to be an '"ice volcano" that periodically belches "lava"
containing liquid water. Simulated lab research by University of Arizona graduate
student Catherine Neish suggests this water may react with organic
compounds in Titan's atmosphere to create complex molecules similar to
those on the early Earth.&lt;/P&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;br&gt;&lt;div style="margin-bottom: 40px;"&gt;Tags: &lt;a href="http://clipmarks.com/tags/titan/" rel="tag"&gt;titan&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/life/" rel="tag"&gt;life&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/astronomy/" rel="tag"&gt;astronomy&lt;/a&gt;&lt;/div&gt;</description><clipSource>http://www.dailygalaxy.com/my_weblog/2008/08/ice-volcanoes-o.html</clipSource><pubDate>Fri, 15 Aug 2008 21:15:21 GMT</pubDate></item><item><title>Strange Rites</title><link>http://clipmarks.com/clipmark/94CCF65F-8532-482E-B94D-7E0775CD76A3/</link><description>&lt;b&gt;clipped by:&lt;/b&gt; &lt;a href="http://clipmarks.com/clipper/AtlLiberal/"&gt;AtlLiberal&lt;/a&gt;&lt;br&gt;&lt;b&gt;clipper's remarks:&lt;/b&gt;  From an outside perspective, this truly is a bizarre ritual that is reminiscent of old B-movies of virgins being thrown into volcanoes to appease the gods. I would bet that most believers don't share this viewpoint. &lt;br&gt;&lt;div border="2" style="margin-top: 10px; border:#000000 1px solid;" width="90%"&gt;&lt;div style="background-color:"&gt;&lt;div align="center" width="100%" style="padding:4px;margin-bottom:4px;background-color:#666666;overflow:hidden;"&gt;&lt;span style="color:#FFFFFF;font-weight:bold;"&gt;Clip Source: &lt;a style="color:#FFFFFF;" href="http://atheism.about.com/od/liberationatheology/ig/Unapologetics-Posters/Unapologetics--Cannibalism.htm" title="http://atheism.about.com/od/liberationatheology/ig/Unapologetics-Posters/Unapologetics--Cannibalism.htm"&gt;atheism.about.com&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;H1&gt;Cannibalism: I'd Like My God Medium Rare, Please. With a Nice Chianti.&lt;/H1&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/AtlLiberal/512/F7066C08-9FBE-41BA-8EAB-FAA8E89A5772.jpg" alt="Cannibalism, Human Sacrifice, Christian Theology: I'd Like My God Medium Rare. With a Nice Chianti" /&gt;&lt;br /&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;P&gt;Even suggesting a connection between cannibalism and Christian mass may sound extreme to believers, but just as the crucifixion of Jesus has a lot in common with older religious practices of human sacrifice, so too does the idea of transubstantiation — wine and bread becoming the blood and body of Jesus — have a lot in common with older religious practices of cannibalism. Crucifixion and mass are easier to understand if one understands the religious background of human sacrifice and cannibalism.

&lt;/P&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;The concept of sacrificing something important to the gods or spirits was common in religions around the world. &lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;For the Aztecs, consuming human flesh was a type of communion, establishing a sacred relationship between humans and gods. Because the people who were ritually sacrificed were "impersonators" of the gods, the Aztecs saw themselves as not consuming another human being, but as consuming a god.&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;br&gt;&lt;div style="margin-bottom: 40px;"&gt;Tags: &lt;a href="http://clipmarks.com/tags/ritual/" rel="tag"&gt;ritual&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/dogma/" rel="tag"&gt;dogma&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/mass/" rel="tag"&gt;mass&lt;/a&gt;&lt;/div&gt;</description><clipSource>http://atheism.about.com/od/liberationatheology/ig/Unapologetics-Posters/Unapologetics--Cannibalism.htm</clipSource><pubDate>Fri, 15 Aug 2008 16:58:49 GMT</pubDate></item><item><title>sub</title><link>http://clipmarks.com/clipmark/29B77E04-03A6-4AF0-8CAA-F8585AA32EA3/</link><description>&lt;b&gt;clipped by:&lt;/b&gt; &lt;a href="http://clipmarks.com/clipper/Jayne22/"&gt;Jayne22&lt;/a&gt;&lt;br&gt;&lt;div border="2" style="margin-top: 10px; border:#000000 1px solid;" width="90%"&gt;&lt;div style="background-color:"&gt;&lt;div align="center" width="100%" style="padding:4px;margin-bottom:4px;background-color:#666666;overflow:hidden;"&gt;&lt;span style="color:#FFFFFF;font-weight:bold;"&gt;Clip Source: &lt;a style="color:#FFFFFF;" href="http://news.bbc.co.uk/1/hi/sci/tech/7547695.stm" title="http://news.bbc.co.uk/1/hi/sci/tech/7547695.stm"&gt;news.bbc.co.uk&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;B&gt;Scientists are set to explore the world's deepest undersea volcanoes, which lie 6km down in the Caribbean.&lt;/B&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;br&gt;&lt;div style="margin-bottom: 40px;"&gt;&lt;/div&gt;</description><clipSource>http://news.bbc.co.uk/1/hi/sci/tech/7547695.stm</clipSource><pubDate>Sat, 09 Aug 2008 17:51:26 GMT</pubDate></item><item><title>San Andreas Fault Longer Than Thought</title><link>http://clipmarks.com/clipmark/303255F6-BB8D-41A2-9F33-E313A8263B93/</link><description>&lt;b&gt;clipped by:&lt;/b&gt; &lt;a href="http://clipmarks.com/clipper/A53GG4/"&gt;A53GG4&lt;/a&gt;&lt;br&gt;&lt;div border="2" style="margin-top: 10px; border:#000000 1px solid;" width="90%"&gt;&lt;div style="background-color:"&gt;&lt;div align="center" width="100%" style="padding:4px;margin-bottom:4px;background-color:#666666;overflow:hidden;"&gt;&lt;span style="color:#FFFFFF;font-weight:bold;"&gt;Clip Source: &lt;a style="color:#FFFFFF;" href="http://news.aol.com/article/san-andreas-fault-longer-than-thought/108930" title="http://news.aol.com/article/san-andreas-fault-longer-than-thought/108930"&gt;news.aol.com&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;H1 class="smallText" id="articleHdln"&gt;San Andreas Fault Longer Than Thought&lt;/H1&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;SPAN&gt;Robin Lloyd&lt;/SPAN&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;DIV class="articleCrdtLn"&gt;LiveScience&lt;/DIV&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;DIV class="articleDt"&gt;posted: &lt;SPAN&gt; 2 HOURS 1 MINUTE AGO&lt;/SPAN&gt;&lt;/DIV&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;DIV class="articleFildUndr"&gt;filed under: &lt;A href="http://news.aol.com/nation" linkindex="75" set="yes"&gt;National News&lt;/A&gt;, &lt;A href="http://news.aol.com/science" linkindex="76"&gt;Science News&lt;/A&gt;&lt;/DIV&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;DIV class="enhanLeftNoWrap"&gt;
&lt;DIV class="enhanLeftNoWrapInner enhanSmall enhanCmn"&gt;&lt;A target="_blank" href="http://www.livescience.com/" linkindex="77"&gt;&lt;IMG border="0" alt="LiveScience.com" src="http://cdn.digitalcity.com/rl_live_science/live-science-logo-215.gif" /&gt;&lt;/A&gt;
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&lt;/DIV&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;DIV id="articleTxt1" class="articleTxt smallText"&gt;(July 30) - As if the San Andreas Fault weren't long and menacing enough, newly found mud pots and mud volcanoes now suggest it extends another 18 miles, going under the Salton Sea and beyond, in the desert southeast of Palm Springs. &lt;/DIV&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;H3 class="lbgTitle"&gt;California's Earthquake Source&lt;/H3&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;DIV class="lbgBody"&gt;&lt;DIV class="picCont"&gt;&lt;DIV class="lbgImgWrap"&gt;&lt;IMG border="0" alt="San Andreas fault line - map" src="http://o.aolcdn.com/dims-photohub/dims/NEWS/1/408/272/60/http://o.aolcdn.com/photo-hub/news_gallery/5/6/566167/1217444498153.JPEG" /&gt;&lt;CITE&gt;Cassandra Shie, AOL&lt;/CITE&gt;&lt;DIV class="clear"&gt;&lt;/DIV&gt;&lt;/DIV&gt;&lt;/DIV&gt;&lt;P class="lbgCap"&gt;The San Andreas Fault line, which runs roughly 700 miles through California's west coast, is longer than previously thought, researchers found. The line, which separates different plates of land that move in different directions and cause earthquakes, extends another 18 miles in the desert southeast of Palm Springs.&lt;/P&gt;&lt;DIV class="lbgCon"&gt;&lt;A rel="nofollow" title="Next" class="lbgNxt" href="?lbgIndex=1" linkindex="78"&gt;&lt;IMG width="29" height="29" border="0" alt="" src="http://o.aolcdn.com/art/dynanews/lbg-next-btn" /&gt;&lt;/A&gt;&lt;DIV class="lbgCnt"&gt;&lt;EM&gt;1 &lt;I&gt;of&lt;/I&gt; 4&lt;/EM&gt;PHOTOS&lt;/DIV&gt;&lt;/DIV&gt;&lt;DIV class="clear"&gt;&lt;/DIV&gt;&lt;/DIV&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;DIV id="articleTxt3" class="articleTxt smallText"&gt;U.S. Geological Survey researchers David K. Lynch and Kenneth W. Hudnut report this result after a survey of mud pots in the area immediately east of the southeastern-most portion of the Salton Sea in Imperial County, Calif. &lt;/DIV&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;br&gt;&lt;div style="margin-bottom: 40px;"&gt;Tags: &lt;a href="http://clipmarks.com/tags/science/" rel="tag"&gt;science&lt;/a&gt;&lt;/div&gt;</description><clipSource>http://news.aol.com/article/san-andreas-fault-longer-than-thought/108930</clipSource><pubDate>Thu, 31 Jul 2008 06:18:19 GMT</pubDate></item><item><title>Ancient Sunken Islands Found</title><link>http://clipmarks.com/clipmark/F6D9C4E9-91C0-4DE7-8567-99B21D8855EA/</link><description>&lt;b&gt;clipped by:&lt;/b&gt; &lt;a href="http://clipmarks.com/clipper/zippunkygirl/"&gt;zippunkygirl&lt;/a&gt;&lt;br&gt;&lt;div border="2" style="margin-top: 10px; border:#000000 1px solid;" width="90%"&gt;&lt;div style="background-color:"&gt;&lt;div align="center" width="100%" style="padding:4px;margin-bottom:4px;background-color:#666666;overflow:hidden;"&gt;&lt;span style="color:#FFFFFF;font-weight:bold;"&gt;Clip Source: &lt;a style="color:#FFFFFF;" href="http://www.msnbc.msn.com/id/6844056/" title="http://www.msnbc.msn.com/id/6844056/"&gt;www.msnbc.msn.com&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/zippunkygirl/512/DFF6EDAA-65DA-47AF-9A59-5B466359637B.jpg" alt="" /&gt;&lt;br /&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;DIV itxtvisited="1"&gt;An image from the ROV Tiburon shows deep-sea beach sand and lava that appears to have been sculpted by waves — along a shore now nearly a half-mile (680 meters) below the surface.&lt;/DIV&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;
&lt;P class=textBodyBlack itxtvisited="1"&gt;Sandy beaches are plentiful along the 
California coast, but not many are found below the ocean. Scientists just added 
three to the list.&lt;/P&gt;
&lt;P class=textBodyBlack itxtvisited="1"&gt;&lt;SPAN id=byLine 
itxtvisited="1"&gt;&lt;/SPAN&gt;What were once volcanic islands off the coast of 
California now sit at the bottom of sea.&lt;/P&gt;
&lt;P class=textBodyBlack itxtvisited="1"&gt;&lt;SPAN id=byLine 
itxtvisited="1"&gt;&lt;/SPAN&gt;With the help of a robotic submersible, a team of 
researchers captured images of long-sunken sandy beaches at depths exceeding 
2,000 feet (610 meters). The video images and rock samples taken from ocean 
bottom indicate that the beaches were associated with volcanoes that used to 
poke above the surface. &lt;/P&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;By Bjorn Carey&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;P itxtvisited="1" ndPar="[object Object]"&gt;&lt;SPAN id="byLine" itxtvisited="1"&gt;&lt;/SPAN&gt;"They were probably islands for a million years or less and have been submerged for about the last 10 to 14 million years," Clague told LiveScience, adding that his team hasn’t yet finished dating all of the samples hauled up from below.&lt;/P&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;br&gt;&lt;div style="margin-bottom: 40px;"&gt;&lt;/div&gt;</description><clipSource>http://www.msnbc.msn.com/id/6844056/</clipSource><pubDate>Wed, 30 Jul 2008 08:59:42 GMT</pubDate></item><item><title>San Andreas fault longer than previously thought</title><link>http://clipmarks.com/clipmark/89734DBD-AF9C-4DFF-8C06-9B612BF194DF/</link><description>&lt;b&gt;clipped by:&lt;/b&gt; &lt;a href="http://clipmarks.com/clipper/kkcapricorn/"&gt;kkcapricorn&lt;/a&gt;&lt;br&gt;&lt;b&gt;clipper's remarks:&lt;/b&gt;  &lt;blockquote&gt;"The extension of the San Andreas does not appear to be active. It is probably a very old part of the fault, and helps to explain the larger, more complex transition area between the Imperial fault and San Andreas Fault, called the Brawley Seismic Zone," he said.&lt;/blockquote&gt; Weird co-incidence this article appears the same day that a 5.8 quake occurs.&lt;br/&gt;&lt;br/&gt; &lt;br&gt;&lt;div border="2" style="margin-top: 10px; border:#000000 1px solid;" width="90%"&gt;&lt;div style="background-color:"&gt;&lt;div align="center" width="100%" style="padding:4px;margin-bottom:4px;background-color:#666666;overflow:hidden;"&gt;&lt;span style="color:#FFFFFF;font-weight:bold;"&gt;Clip Source: &lt;a style="color:#FFFFFF;" href="http://www.livescience.com/environment/080729-mud-pots.html" title="http://www.livescience.com/environment/080729-mud-pots.html"&gt;www.livescience.com&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/kkcapricorn/512/C5B066B2-4FA5-41C9-B8E5-AFCC09BA4207.jpg" alt="" /&gt;&lt;br /&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;U.S. Geological Survey researchers David K. Lynch and Kenneth W. Hudnut report &lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;Using satellite imagery and a physical examination of the land, they identified a cluster of 33 mud pots, &lt;A href="http://www.livescience.com/php/multimedia/imagedisplay/img_display.php?s=environment&amp;c=&amp;l=on&amp;pic=080729-tall-volcano-02.jpg&amp;cap=Kenneth+Hudnut+studying+a+mud+volcano.+Credit:+%A9+David+Lynch%2C+2006&amp;title="&gt;mud volcanoes&lt;/A&gt;  and sink holes which, when plotted, form a clear linear pattern that suggests an underground rift or fault. 
&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;Water and gas (CO2 mostly) coming up from below the surface must have a source," Lynch explained. "It is usually associated with an opening in the crust that reaches down to a magma body relatively close to the surface (&lt;A href="http://www.livescience.com/php/video/player.php?video_id=yellowstone_quest"&gt;like Yellowstone&lt;/A&gt;). The fact that [the mud pots and mud volcanoes] line up indicates a fault. The fact that they line up with the end of the San Andreas Fault suggests that the two are connected &lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;Seismologists say that enough stress has accumulated at the fault to generate the next "Big One," an&lt;A href="http://www.livescience.com/strangenews/070817_gm_earthquake_insides.html"&gt; earthquake&lt;/A&gt;  of magnitude 7.0 or greater, any day now or 10 years or more from now. &lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt; the region is more complicated than researchers previously thought. 
&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;br&gt;&lt;div style="margin-bottom: 40px;"&gt;Tags: &lt;a href="http://clipmarks.com/tags/earthquake/" rel="tag"&gt;earthquake&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/fault/" rel="tag"&gt;fault&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/mud+hole/" rel="tag"&gt;mud hole&lt;/a&gt;&lt;/div&gt;</description><clipSource>http://www.livescience.com/environment/080729-mud-pots.html</clipSource><pubDate>Tue, 29 Jul 2008 20:34:18 GMT</pubDate></item></channel></rss>