<?xml version="1.0" encoding="UTF-8"?>
<?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 | amgumen's degassing collection</title><link>http://clipmarks.com/clipper/amgumen/clipcast/degassing/</link><feedUrl>http://rss.clipmarks.com/clipper/amgumen/clipcast/degassing/</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>Boiling Hot Water Found in Frigid Arctic Sea</title><link>http://clipmarks.com/clipmark/D7BE1162-075C-4A37-8005-836B27142B85/</link><description>&lt;b&gt;clipped by:&lt;/b&gt; &lt;a href="http://clipmarks.com/clipper/amgumen/"&gt;amgumen&lt;/a&gt;&lt;br&gt;&lt;b&gt;clipper's remarks:&lt;/b&gt;  Scalding liquid rises out of the seafloor at temperatures that are more than twice the boiling point of water. &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/080724-black-smokers.html" title="http://www.livescience.com/environment/080724-black-smokers.html"&gt;www.livescience.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;
The cluster of five hydrothermal vents, also called black smokers, were discovered farther north than any others previously identified.
The vents, one of which towers four stories high, are located on the Mid-Atlantic Ridge between Greenland
and Norway, more than 120 miles farther north than other known vents. 
&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 active chimneys in the new field are mostly black and covered
with white mats of bacteria feasting on the minerals emitted by the
vents. Older chimneys are mottled red as a result of iron oxidization.
All are the result of seawater seeping into the seafloor, coming near
fiery magma and picking up heat and minerals until the water vents back
into the ocean. 
&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 whole deposit is about 825 feet in diameter at its base and
about 300 feet across on the top and might turn out to be the largest
such deposit seen on the seafloor, Lilley said. 
&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;Given the massive sulfide deposit, the vent field must surely have been active for many thousands of years&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.livescience.com/environment/080724-black-smokers.html</clipSource><pubDate>Tue, 29 Jul 2008 04:51:43 GMT</pubDate></item><item><title>Toxic gas caused the Great Dying?</title><link>http://clipmarks.com/clipmark/FEC60F4A-ABE5-464B-AED1-53572111FD05/</link><description>&lt;b&gt;clipped by:&lt;/b&gt; &lt;a href="http://clipmarks.com/clipper/amgumen/"&gt;amgumen&lt;/a&gt;&lt;br&gt;&lt;b&gt;clipper's remarks:&lt;/b&gt;  Once the gas made it to the ocean surface, it could have escaped into the atmosphere, triggering terrestrial extinction, Kump says. “Poisonous clouds of hydrogen sulfide wafting around the continents would have killed animals and vegetation,” he says. The gas also could have damaged the planet’s ozone layer letting destructive radiation reach Earth’s surface. &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.geotimes.org/jan08/article.html?id=nn_toxicgas.html" title="http://www.geotimes.org/jan08/article.html?id=nn_toxicgas.html"&gt;www.geotimes.org&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;  Life on Earth nearly ended 251 million years ago. The end-Permian mass extinction wiped out as much as 90 percent of all marine species as well as large numbers of terrestrial animals and plants. But what caused the catastrophe is still a matter of debate&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/amgumen/512/129A5038-DEED-4414-B84A-5F0E41997006.jpg" alt="Catherine Powers with ancient ocean sediments in Hydra, Greece" /&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;By studying the distribution and diversity of 396 bryozoan assemblages over about a 120-million-year time span, the team found that the organisms’ decline began millions of years before the mass extinction,&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 find “argues against an extraterrestrial impact, such as an asteroid, being the killer,” which had been a popular hypothesis for the wide-scale extinction,&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 records also revealed that those bryozoans that lived in deep waters were the first to go. Organisms living on ocean shelves and reefs followed gradually over time. This pattern hints that “something must have come from the deep ocean to kill these organisms&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 hydrogen sulfide started killing off deep-water organisms first and gradually moved into shallow water&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/optional.++separate+by+commas./" rel="tag"&gt;optional.  separate by commas.&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/environment/" rel="tag"&gt;environment&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/geology/" rel="tag"&gt;geology&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/earth/" rel="tag"&gt;earth&lt;/a&gt;&lt;/div&gt;</description><clipSource>http://www.geotimes.org/jan08/article.html?id=nn_toxicgas.html</clipSource><pubDate>Sun, 27 Jan 2008 00:33:49 GMT</pubDate></item><item><title>Subglatial volcanoes of Iceland</title><link>http://clipmarks.com/clipmark/97477C82-04BB-4322-8262-DFC040653671/</link><description>&lt;b&gt;clipped by:&lt;/b&gt; &lt;a href="http://clipmarks.com/clipper/amgumen/"&gt;amgumen&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.vulkaner.no/v/volcan/grimsvot-e.html" title="http://www.vulkaner.no/v/volcan/grimsvot-e.html"&gt;www.vulkaner.no&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;
          Grimsvotn volcano (N 64.41°, W 17.33°), situated near the center 
          of the Vatnajokull ice cap&lt;BR /&gt;
          in central Iceland, is one of Iceland's most active volcanoes. It has 
          a complex of calderas,&lt;BR /&gt;
          and a subglacial caldera lake sustained by geothermal heat. Small eruptions 
          have occurred&lt;BR /&gt;
          at the volcano in 1983 and 1998 (around 0.1 km3). In 1996, the Gjalp 
          subglacial eruption&lt;BR /&gt;
          occurred north of the volcano. The most recent eruption triggered by 
          a pressure release as&lt;BR /&gt;
          the current eruption occurred in 1934.&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;
          Vatnajökull covers an area of 8.100 km². The volume of the icecap is 
          almost 3.000 km³.&lt;BR /&gt;
          The icecover is about 400 m thick (average), and at the most about 950 
          meters!&lt;BR /&gt;
          Since 70 % of the surface is above 1.100 m asl, it is still alive.&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 eruption at Grimsvötn volcano ceased 
          between Friday night and Saturday morning,&lt;BR /&gt;&lt;DIV&gt;
          November 6, 2004.&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/amgumen/512/2184BC81-6689-4ED8-BCB7-1AE7D81F0DFC.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;FONT size="2" face="Arial, Helvetica, sans-serif" color="#990000"&gt;Grimsvötn 
          crater on November 5th.&lt;/FONT&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/amgumen/512/6CA14D0D-7616-49F0-A72C-D2BEFC5CDED4.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;B&gt;November 5th, 2004&lt;/B&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 explosion in the morning of November 4th.&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/amgumen/512/7E901144-3859-4C50-9A41-C10DAF337863.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;FONT size="2" face="Arial, Helvetica, sans-serif" color="#990000"&gt;A 
              second cauldron near Grimsvötn.&lt;/FONT&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/amgumen/512/14DB279E-881D-41E7-85AE-876A249148DC.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;FONT size="2" face="Arial, Helvetica, sans-serif" color="#990000"&gt;In 
                      the morning of November 2nd&lt;BR /&gt;
                      &lt;/FONT&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;B&gt;2.november 2004&lt;/B&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/amgumen/512/89F0CE5E-D7E4-4FFA-BD79-E966EAA0DD47.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/amgumen/512/816137C6-68DF-4337-B8F5-192913381FE8.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/amgumen/512/152216E5-3C48-4B31-B421-ABF3F7A8CB72.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/amgumen/512/B209486D-004B-4244-9244-540252D709F5.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/amgumen/512/0B27AEC6-B274-40F2-93DA-AE89BBD1542A.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/amgumen/512/70509E5B-6AD0-4319-BC49-C013566F25FD.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/amgumen/512/181BDA70-EF39-4299-95AE-34D2222942E3.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/amgumen/512/FFD64AAB-551C-4BF9-A06B-5F054C368A51.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/amgumen/512/6AAB6E60-957D-4BE9-8B12-0E07BF2E74A5.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/amgumen/512/71F7D656-44B3-4F1A-B37D-211A81652169.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/amgumen/512/96BDF557-2A5A-47E0-8FD1-502DDA941A8D.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/amgumen/512/C0E7BC78-3BB5-4A02-BB67-F643A149EB27.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/amgumen/512/D660F078-A287-4AE0-8450-E957A19ACC94.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/amgumen/512/0766302D-D904-4423-B1B7-608B69F29B75.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/amgumen/512/AEE662D8-E5FD-49E5-B888-E277AAAEE160.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;Tags: &lt;a href="http://clipmarks.com/tags/volcanoes/" rel="tag"&gt;volcanoes&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/geology/" rel="tag"&gt;geology&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/environment/" rel="tag"&gt;environment&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/climate+change/" rel="tag"&gt;climate change&lt;/a&gt;&lt;/div&gt;</description><clipSource>http://www.vulkaner.no/v/volcan/grimsvot-e.html</clipSource><pubDate>Thu, 24 Jan 2008 00:18:18 GMT</pubDate></item><item><title>Underground coal fires: pictures</title><link>http://clipmarks.com/clipmark/275CE5A5-BF8B-485F-8E4C-1F39D9C28980/</link><description>&lt;b&gt;clipped by:&lt;/b&gt; &lt;a href="http://clipmarks.com/clipper/amgumen/"&gt;amgumen&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.itc.nl/~coalfire/photos/overview.html" title="http://www.itc.nl/~coalfire/photos/overview.html"&gt;www.itc.nl&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/amgumen/512/E2737386-27E4-4C86-80A0-BC4256E20F03.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;P class="caption"&gt;Clouds of noxious gases coming out of an exhalation crack above a near-surface coal fire.&lt;/P&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/amgumen/512/21C9A9DA-5A18-40F2-B8AC-25E10EEBB8DC.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;P class="caption"&gt;Exhalation crack above a sub-surface coal fire. Sublimation minerals along exhalation crack are mainly salmiac (white) and sulfur (yellow).&lt;/P&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/amgumen/512/D4816FAA-1042-48C3-AED3-B61BF9429BCA.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;P class="caption"&gt;Subsidence above progressed coal fire. The void left behind by the burnt-away near-surface coal layer collapses under the load of the sandstone layers above. &lt;/P&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/amgumen/512/5F2A444F-57BD-46D3-B810-0D04977A6727.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;P class="caption"&gt;Near surface coal fire as seen from surface.&lt;/P&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/amgumen/512/15ED3464-9474-4382-BF08-58CD49688667.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;P class="caption"&gt;Temperature measurements in a coal fire area with a radiant thermometer under hazardous conditions.&lt;/P&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/amgumen/512/2D49BB8F-5973-42D8-A695-6D34D2E0C807.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;P class="caption"&gt;Temperature measurements in a coal fire area with a radiant thermometer under hazardous conditions. 
					Salmiac exhalation minerals form a white crust on the rocks around this exhalation vent of an underground coal fire. 
					Photo credit: DFD/DLR Germany.&lt;/P&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/amgumen/512/F04CD24C-AE5C-4F0A-9AC7-970F7A5F2F32.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;Infrared picture of hilly terrain in the Wuda region. 
					Blue colours represent the cold sky; shades of yellow and green the normal temperatures of the rocks. 
					The clusters of red patches are caused by underground coal fires&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/optional.++separate+by+commas./" rel="tag"&gt;optional.  separate by commas.&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/earth/" rel="tag"&gt;earth&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/environment/" rel="tag"&gt;environment&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/nature/" rel="tag"&gt;nature&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/geology/" rel="tag"&gt;geology&lt;/a&gt;&lt;/div&gt;</description><clipSource>http://www.itc.nl/~coalfire/photos/overview.html</clipSource><pubDate>Sun, 20 Jan 2008 00:21:37 GMT</pubDate></item><item><title>Surprisingly hot phenomenon</title><link>http://clipmarks.com/clipmark/96D4AC2D-D36F-48B3-B736-B6242A6790FD/</link><description>&lt;b&gt;clipped by:&lt;/b&gt; &lt;a href="http://clipmarks.com/clipper/amgumen/"&gt;amgumen&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.oregonlive.com/news/oregonian/index.ssf?/base/news/1199514313113650.xml&amp;coll=7&amp;thispage=1" title="http://www.oregonlive.com/news/oregonian/index.ssf?/base/news/1199514313113650.xml&amp;coll=7&amp;thispage=1"&gt;www.oregonlive.com&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;For the past three years, the researchers have journeyed to
the Antarctic to deploy hydrophones designed and built at
this tiny science center on Newport's Yaquina Bay&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;Earthquakes and magma spewing on the seafloor
go hand in hand, and what we are seeing is, there are new
heat sources right off the coast of Deception Island that no
one was aware of before&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;It's the only place on the planet where active
seafloor and subaerial (above sea level) volcanoes are near
large icebergs and ice sheets.&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 team's studies lead to new information
about how the seafloor volcanoes and earthquakes contribute
to the breakup of ice in the region&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;If it wasn't for our work, these deep-sea
eruptions would be completely unknown&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;three-quarters of the Earth is covered by ocean,
the vast majority of volcanic activity on Earth is occurring
without our knowledge undersea&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;So it's unknown
how much heat and chemicals the underwater volcanoes spew
into the ocean and atmosphere, affecting global ocean
temperatures and climat&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/climate/" rel="tag"&gt;climate&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/environment/" rel="tag"&gt;environment&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/geology/" rel="tag"&gt;geology&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/interesting/" rel="tag"&gt;interesting&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/nature/" rel="tag"&gt;nature&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/ocean/" rel="tag"&gt;ocean&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/science/" rel="tag"&gt;science&lt;/a&gt;&lt;/div&gt;</description><clipSource>http://www.oregonlive.com/news/oregonian/index.ssf?/base/news/1199514313113650.xml&amp;coll=7&amp;thispage=1</clipSource><pubDate>Fri, 11 Jan 2008 23:40:11 GMT</pubDate></item><item><title>  Hawaiian Volcanoes: Beauty &amp; Terror</title><link>http://clipmarks.com/clipmark/C947187B-CFA3-4DEE-8D03-21159F77CAB8/</link><description>&lt;b&gt;clipped by:&lt;/b&gt; &lt;a href="http://clipmarks.com/clipper/amgumen/"&gt;amgumen&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.darkroastedblend.com/2007/11/hawaiian-volcanoes-beauty-terror.html" title="http://www.darkroastedblend.com/2007/11/hawaiian-volcanoes-beauty-terror.html"&gt;www.darkroastedblend.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;Pu'u 'O'o cone on Kilauea, Big Island of Hawaii (aerial view) -&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/amgumen/512/1BF6A09A-2A8D-41B2-8D61-2E66911ED8B2.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&gt;Eruptions in the Hawaiian volcanoes are normally preceded by multiple earthquakes which create fissures and facilitate the magma's flow to 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;img src="http://clipmarks.com/image_cache/amgumen/512/9C805467-A73B-4763-AFFD-04DD63B73EB1.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/amgumen/512/E9FE6A69-C0F0-4C82-9BCE-0915D008A16E.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&gt;The Paoehoe (pah-ho-ay-ho-ay) lava flows reach the seawater and explode, as ocean waves enter the fiery lava tubes.&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 semi-solidified lava structures may look as curious lava-lamp oddities, but conceal behind their fanciful shapes a highly dangerous nature. The lava tongues and "tentacles" may look solid but often they remain incredibly hot and unstable for long time. &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;Like alien bread dough they creep forward, quickly cooling off and adding perplexing shapes here and there. The imaginary sequel to "The Blob" movie could certainly use such visuals:&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/amgumen/512/3E838964-621B-4125-B18B-1CA95386D663.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/amgumen/512/CAC32AE1-49A3-4F7D-BD65-9AE6B731F356.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/amgumen/512/46E3225A-34FF-4BC2-A633-F78B6A632926.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&gt;A creeping lava tongue... A fiery waterfall curtain...&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/amgumen/512/11F99F66-BB12-4B09-A1DD-4F2DA449444F.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/amgumen/512/513B70EA-2768-4251-B44E-E93D60849838.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/amgumen/512/EC4DFD38-64EA-4CE9-B843-F1F534790360.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&gt;The bizarre coloring observed in the lava flowing in the tubes: &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/amgumen/512/ED8454E7-6D2D-4153-9745-72F4751E94EB.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&gt;Such openings are called "skylights", offering a view into a hellish kingdom below:&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/amgumen/512/54DAC36D-BB08-49C9-8272-9348BFC070EB.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/amgumen/512/201918D2-6AA0-4485-A3F2-43B6BDCFFC21.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/amgumen/512/02468B3D-66ED-4F52-8B3D-AD8C2210A988.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/amgumen/512/57486ECF-AC7C-4618-B868-950BA043F8CF.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/amgumen/512/8ED6E960-1536-4F8E-8CB6-6C31DF0E872C.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/amgumen/512/456A23DD-1297-4A84-8CC0-123E4C42D072.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/amgumen/512/BE5AEC3B-37CE-4777-AFDF-4459C4B712BE.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/amgumen/512/0512EA46-1291-4A4E-95E6-68EFFB405AB2.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/amgumen/512/A4505A2C-E8B2-46D6-8F8C-E0F177999431.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/amgumen/512/47A4E658-DE5D-4782-950B-8729CC3795A9.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/amgumen/512/E3BAFBD1-2D17-4394-9834-00C3CBE63750.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/amgumen/512/75F5D988-1606-4945-AEF5-059B4FB81E23.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/amgumen/512/56CC438A-C4F3-4F26-B298-64E2700F12D4.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/amgumen/512/4F325667-DCE2-4C14-9025-24F556DD8220.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/amgumen/512/904C3A59-F303-485B-96DC-80552BD2E983.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/amgumen/512/52936BBC-22E1-48E9-83E4-94F733249FE2.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/amgumen/512/8B86953B-32E8-4165-B3B5-2B27FC403B13.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/amgumen/512/74E0AE5E-2DD8-4A15-AF5C-D7A28D08DC55.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/amgumen/512/737BD2AA-72D1-4D0D-AB9F-738A053522E2.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;Tags: &lt;a href="http://clipmarks.com/tags/optional.++separate+by+commas./" rel="tag"&gt;optional.  separate by commas.&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/geology/" rel="tag"&gt;geology&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/interesting/" rel="tag"&gt;interesting&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/nature/" rel="tag"&gt;nature&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/science/" rel="tag"&gt;science&lt;/a&gt;&lt;/div&gt;</description><clipSource>http://www.darkroastedblend.com/2007/11/hawaiian-volcanoes-beauty-terror.html</clipSource><pubDate>Sun, 23 Dec 2007 23:28:27 GMT</pubDate></item><item><title>Alaska Lake Boils With Escaping Methane</title><link>http://clipmarks.com/clipmark/BF0E8338-C7AB-4030-8297-5FA6105861D0/</link><description>&lt;b&gt;clipped by:&lt;/b&gt; &lt;a href="http://clipmarks.com/clipper/amgumen/"&gt;amgumen&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.ens-newswire.com/ens/sep2007/2007-09-11-096.asp" title="http://www.ens-newswire.com/ens/sep2007/2007-09-11-096.asp"&gt;www.ens-newswire.com&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;


Last month, University of Alaska-Fairbanks researcher Katey Walter brought a National Public Radio crew to Alaska's North Slope to show them how methane is released when permafrost thaws beneath lakes.&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 crew found a lake violently boiling with escaping methane.&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;It was cold, wet and windy. We were dropped off in the middle of nowhere by a helicopter and paddled out to a huge methane plume in the middle of the lake with no idea what to expect, how strong the bubbling plume would be, whether or not our raft would stay afloat, how dangerous it would be to breath the gas&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 violent streams of bubbles made the lake appear as if it were boiling, but the water was pretty cold&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;this summer's fieldwork indicates that methane hotspots can come from various sources, not just thawing permafrost.&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;It is unlikely that this methane plume was related to permafrost thaw," said Walter, adding that the methane boiling out of the lake was more likely related to natural gas seepage.&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/environment/" rel="tag"&gt;environment&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/geology/" rel="tag"&gt;geology&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/interesting/" rel="tag"&gt;interesting&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/nature/" rel="tag"&gt;nature&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/science/" rel="tag"&gt;science&lt;/a&gt;&lt;/div&gt;</description><clipSource>http://www.ens-newswire.com/ens/sep2007/2007-09-11-096.asp</clipSource><pubDate>Sat, 15 Sep 2007 04:28:23 GMT</pubDate></item><item><title>The atmosphere before and after the Mt. Pinatubo eruption</title><link>http://clipmarks.com/clipmark/30B6E290-4B37-4F94-8692-C666A3FD5E89/</link><description>&lt;b&gt;clipped by:&lt;/b&gt; &lt;a href="http://clipmarks.com/clipper/amgumen/"&gt;amgumen&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.gsfc.nasa.gov/gsfc/earth/pictures/pinatubo/atmosphere%20before.jpg" title="http://www.gsfc.nasa.gov/gsfc/earth/pictures/pinatubo/atmosphere%20before.jpg"&gt;www.gsfc.nasa.gov&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/amgumen/512/2C3F5B4B-C744-4548-9915-E7D85DA47D50.jpg" alt="The image “http://www.gsfc.nasa.gov/gsfc/earth/pictures/pinatubo/atmosphere%20before.jpg” cannot be displayed, because it contains errors." /&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.gsfc.nasa.gov/gsfc/earth/pictures/pinatubo/atmosphere%20after.jpg" title="http://www.gsfc.nasa.gov/gsfc/earth/pictures/pinatubo/atmosphere%20after.jpg"&gt;www.gsfc.nasa.gov&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/amgumen/512/265CD5B8-A46A-4873-946C-EEAA2FFCD53B.jpg" alt="http://www.gsfc.nasa.gov/gsfc/earth/pictures/pinatubo/atmosphere%20after.jpg" /&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.gsfc.nasa.gov/gsfc/earth/pinatuboimages.htm" title="http://www.gsfc.nasa.gov/gsfc/earth/pinatuboimages.htm"&gt;www.gsfc.nasa.gov&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;FONT size="3" face="Arial"&gt;These images highlight the
                  difference in the atmosphere before and after the Mt. Pinatubo
                  eruption. Showing the earth’s limb at sunset, first in
                  September 1984, the atmosphere is relatively clear. The second
                  image, taken in August of 1991, a little more than a month
                  after the eruption, shows distinct layers of aerosols in the
                  upper reaches of the atmosphere. These aerosols eventually
                  made their way around the globe, contributing to a temporary
                  worldwide cooling.&lt;/FONT&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/volcanoes/" rel="tag"&gt;volcanoes&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/environment/" rel="tag"&gt;environment&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/geology/" rel="tag"&gt;geology&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/nature/" rel="tag"&gt;nature&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/interesting/" rel="tag"&gt;interesting&lt;/a&gt;&lt;/div&gt;</description><clipSource>http://www.gsfc.nasa.gov/gsfc/earth/pictures/pinatubo/atmosphere%20before.jpg</clipSource><pubDate>Tue, 29 May 2007 00:49:26 GMT</pubDate></item><item><title>Azeri mud volcano flares</title><link>http://clipmarks.com/clipmark/974860F0-45DC-41B6-80E8-223F5DD81739/</link><description>&lt;b&gt;clipped by:&lt;/b&gt; &lt;a href="http://clipmarks.com/clipper/amgumen/"&gt;amgumen&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/1626310.stm" title="http://news.bbc.co.uk/1/hi/sci/tech/1626310.stm"&gt;news.bbc.co.uk&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/amgumen/512/548C62AF-D715-43D7-B183-A6AEDE644A5C.jpg" alt="Azeri mud volcano, Phil Hardy" /&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;The picture doesn't lie.  It was an impressive volcanic eruption in Azerbaijan in the southern Caucasus&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;volcanic activity under the Caspian Sea off the Azeri coast created a whole new island&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;Azerbaijan and the Caspian Sea are home to nearly four hundred mud volcanoes - more than half the total throughout 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;Every twenty years or so, a mud volcano may explode with great force, shooting flames hundreds of metres into the sky, and depositing tonnes of mud on the surrounding area.&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 flame was unbelievably big, about three hundred metres high. It was surrounded by dense, black smoke, and lots of mud was being thrown into the air.&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/volcanoes/" rel="tag"&gt;volcanoes&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/geology/" rel="tag"&gt;geology&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/interesting/" rel="tag"&gt;interesting&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/environment/" rel="tag"&gt;environment&lt;/a&gt;&lt;/div&gt;</description><clipSource>http://news.bbc.co.uk/1/hi/sci/tech/1626310.stm</clipSource><pubDate>Fri, 25 May 2007 15:26:17 GMT</pubDate></item><item><title>Giant Volcanic Plume Bursts From Jupiter Moon</title><link>http://clipmarks.com/clipmark/6849E931-0635-4035-BC5C-D917D345BDC6/</link><description>&lt;b&gt;clipped by:&lt;/b&gt; &lt;a href="http://clipmarks.com/clipper/amgumen/"&gt;amgumen&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.nationalgeographic.com/news/2007/05/070502-volcano-io.html" title="http://news.nationalgeographic.com/news/2007/05/070502-volcano-io.html"&gt;news.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/amgumen/512/C301ABE9-8B4A-4517-A7DE-47CF2B2E7185.jpg" alt="Giant volcano plume on Jupiter moon Io picture" /&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;Jupiter's most turbulent moon, Io, is renowned among scientists for its flashy volcanic displays. But even experts were surprised when they saw this plume of gas vaulting nearly 200 miles (320 kilometers) over the moon's north pole&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 of the Tvashtar plume is the best and most detailed plume image that any of us—including longtime Jupiter experts—have ever seen," &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 plume likely formed when sulfurous gases released by the volcano crystallized in the frigid vacuum of space&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/interesting/" rel="tag"&gt;interesting&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/geology/" rel="tag"&gt;geology&lt;/a&gt;&lt;/div&gt;</description><clipSource>http://news.nationalgeographic.com/news/2007/05/070502-volcano-io.html</clipSource><pubDate>Wed, 23 May 2007 02:03:27 GMT</pubDate></item><item><title>Submarine volcanoes and more in the Mariana Arc</title><link>http://clipmarks.com/clipmark/8AB223DA-4000-42B5-A64E-886D8C1368E0/</link><description>&lt;b&gt;clipped by:&lt;/b&gt; &lt;a href="http://clipmarks.com/clipper/amgumen/"&gt;amgumen&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.vulkaner.no/v/volcan/submarin/mariana-arc.html" title="http://www.vulkaner.no/v/volcan/submarin/mariana-arc.html"&gt;www.vulkaner.no&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/amgumen/512/EB85198A-204C-43B4-B0C8-82003F032A71.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/amgumen/512/F4967154-F556-4396-93E7-E7672FD5FAFF.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;FONT size="2" face="Arial, Helvetica, sans-serif" color="#990000"&gt;Left&lt;/FONT&gt;&lt;FONT size="2" face="Arial, Helvetica, sans-serif" color="#990000"&gt;: 
    The vertical column in the center of the image, called a dike, rises from 
    below sea level to the pinnacle at the top &lt;BR /&gt;
    of the ridge. Interlaid massive lavas (darker horizontal bands) and ash-rich 
    lava units (reddish) are also exposed&lt;BR /&gt;
    on the islets of Maug &lt;BR /&gt;
    Right: Three-dimensional view of the Maug caldera, ranging in depth from 241 
    to 25 m &lt;/FONT&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/amgumen/512/50EB3768-ECAA-4D9A-819B-91C40CE6A363.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;Active 
    “smoker” chimneys precipitating iron, copper and zinc sulfides from 
    230ºC fluid. &lt;BR /&gt;
    They are 9 m tall from the base to the top of the chimneys. Dark beehive-type 
    chimneys, &lt;BR /&gt;
    here about 30 cm tall, commonly sit on top of these structures.&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/amgumen/512/4C36282E-3636-442D-A715-114A84DDC8D3.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;FONT size="2" face="Arial, Helvetica, sans-serif" color="#990000"&gt;This may 
    be a unique photograph of a shallow-water tropical fish swimming among active&lt;BR /&gt;
    black smoker chimneys at Black Forest vent field. The chimneys rise up to 
    7 m tall.&lt;/FONT&gt;&lt;BR /&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/amgumen/512/9BB338A0-F680-4536-8A7E-33E4312C799B.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/amgumen/512/DCC9DBD1-B858-4D28-A96E-341C9CB4436A.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/amgumen/512/F254FBAD-C9E1-4E38-BA22-D44E44CEDDCC.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/amgumen/512/8BB48072-6F8D-410A-8D38-AD170B8258ED.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;Tags: &lt;a href="http://clipmarks.com/tags/science/" rel="tag"&gt;science&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/nature/" rel="tag"&gt;nature&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/geology/" rel="tag"&gt;geology&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/volcanoes/" rel="tag"&gt;volcanoes&lt;/a&gt;&lt;/div&gt;</description><clipSource>http://www.vulkaner.no/v/volcan/submarin/mariana-arc.html</clipSource><pubDate>Mon, 21 May 2007 01:14:58 GMT</pubDate></item><item><title>Amazing geologic features on the deep seafloor</title><link>http://clipmarks.com/clipmark/0477A4B3-51EA-48D6-A03F-2DF4EC11DD86/</link><description>&lt;b&gt;clipped by:&lt;/b&gt; &lt;a href="http://clipmarks.com/clipper/amgumen/"&gt;amgumen&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.oceanexplorer.noaa.gov/explorations/02fire/logs/jul31/media/495.html" title="http://www.oceanexplorer.noaa.gov/explorations/02fire/logs/jul31/media/495.html"&gt;www.oceanexplorer.noaa.gov&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/amgumen/512/F0C1D1AF-D41F-4F04-ACAB-DE3183D20D30.jpg" alt="Inactive chimney sample embedded with "fossilized" tubeworms" /&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;manipulator arm holds a sample of an inactive chimney in which "fossilized" tubeworms are embedded&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.oceanexplorer.noaa.gov/explorations/02fire/logs/jul31/media/754.html" title="http://www.oceanexplorer.noaa.gov/explorations/02fire/logs/jul31/media/754.html"&gt;www.oceanexplorer.noaa.gov&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/amgumen/512/4AB501F6-ED23-459D-BB0A-CF15A5A5E287.jpg" alt="ROPOS arm sampling hot fluid" /&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;hot fluid sampling at this black smoker vent&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.oceanexplorer.noaa.gov/explorations/02fire/logs/jul26/media/oldchmny.html" title="http://www.oceanexplorer.noaa.gov/explorations/02fire/logs/jul26/media/oldchmny.html"&gt;www.oceanexplorer.noaa.gov&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/amgumen/512/67DF12B0-9607-49CF-A12F-5BB922022B2E.jpg" alt="The ROPOS manipulator arm prepares to sample an inactive chimney" /&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.oceanexplorer.noaa.gov/explorations/04fire/logs/april12/media/champagne_vent.html" title="http://www.oceanexplorer.noaa.gov/explorations/04fire/logs/april12/media/champagne_vent.html"&gt;www.oceanexplorer.noaa.gov&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/amgumen/512/0874419E-4B94-4850-9BF3-D3B2A5F8370F.jpg" alt="These microbial mats are similar in composition to those as seen at the Yellow Top Vent site." /&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;extremely gassy, high-temperature (&amp;gt;100°C, 212°F) white smokers at Champagne Vent.&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.oceanexplorer.noaa.gov/explorations/04fire/logs/april10/media/chimneys.html" title="http://www.oceanexplorer.noaa.gov/explorations/04fire/logs/april10/media/chimneys.html"&gt;www.oceanexplorer.noaa.gov&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/amgumen/512/E627831A-DAA3-4508-AE28-8D015F2B0E6A.jpg" alt="White chimneys at Champagne vent site, NW Eifuku volcano." /&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;The chimneys are ~20 cm (8 in) across and ~50 cm (20 in) high, venting fluids at 103ºC (217ºF). &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.oceanexplorer.noaa.gov/explorations/04fire/logs/april10/media/bubbles.html" title="http://www.oceanexplorer.noaa.gov/explorations/04fire/logs/april10/media/bubbles.html"&gt;www.oceanexplorer.noaa.gov&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/amgumen/512/DAEFBE73-F340-4BC8-9610-C9512E9FA7D8.jpg" alt="Close-up of bubbles at the Champagne vent site." /&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;bubbles at the Champagne vent site&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.oceanexplorer.noaa.gov/explorations/04fire/logs/april05/media/five_towers.html" title="http://www.oceanexplorer.noaa.gov/explorations/04fire/logs/april05/media/five_towers.html"&gt;www.oceanexplorer.noaa.gov&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/amgumen/512/8D1BC0E2-585B-4CBD-915E-CFA1BFEEDD9F.jpg" alt="Active “smoker” chimneys precipitating iron, copper and zinc sulfides from 230ºC fluid." /&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;
		    Active “smoker” chimneys precipitating iron, copper and zinc sulfides from 230ºC fluid&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.oceanexplorer.noaa.gov/explorations/04fire/logs/april04/media/ash_layers.html" title="http://www.oceanexplorer.noaa.gov/explorations/04fire/logs/april04/media/ash_layers.html"&gt;www.oceanexplorer.noaa.gov&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/amgumen/512/3D3262A7-BD4D-48D9-850C-75C94A094BB7.jpg" alt="Interlayered basaltic (dark) and felsic (light) ash layers in the east wall of West Rota caldera." /&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;
		    Interlayered basaltic (dark) and felsic (light) ash layers&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.oceanexplorer.noaa.gov/explorations/04fire/logs/march30/media/craterplume2.html" title="http://www.oceanexplorer.noaa.gov/explorations/04fire/logs/march30/media/craterplume2.html"&gt;www.oceanexplorer.noaa.gov&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/amgumen/512/5234C177-7BA7-44F7-B6AC-EAD6596E1FC7.jpg" alt="Giant smoky plume discovered near the summit of NW Rota 1 volcano." /&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;
Giant smoky plume&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/interesting/" rel="tag"&gt;interesting&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/geology/" rel="tag"&gt;geology&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/volcanoes/" rel="tag"&gt;volcanoes&lt;/a&gt;&lt;/div&gt;</description><clipSource>http://www.oceanexplorer.noaa.gov/explorations/02fire/logs/jul31/media/495.html</clipSource><pubDate>Sun, 20 May 2007 23:54:07 GMT</pubDate></item><item><title>Gassy blast from prehistoric volcanoes heated Earth</title><link>http://clipmarks.com/clipmark/9FA3AD73-EB1E-487B-B750-392299F0213B/</link><description>&lt;b&gt;clipped by:&lt;/b&gt; &lt;a href="http://clipmarks.com/clipper/amgumen/"&gt;amgumen&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.yahoo.com/s/nm/20070426/sc_nm/volcanoes_warming_dc_1" title="http://news.yahoo.com/s/nm/20070426/sc_nm/volcanoes_warming_dc_1"&gt;news.yahoo.com&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;Ancient volcanoes may have caused a
dramatic warming of the Earth's atmosphere that raised sea
temperatures and killed off many marine species, resulting in a
"planetary emergency,"&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;That triggered a 222,000-year period of warming that raised
sea surface temperatures by 5 degrees Celsius (9 degrees F) in
the tropics and more than 6 degrees Celsius (11 degrees F) in
the Arctic and increased the acidity of the oceans.&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 resulting "planetary emergency," as scientists have
called it, wiped out 30 percent to 50 percent of the planet's
deep sea creatures.&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;volcanic eruptions began about 61
million years ago and then it took another 5 million years for
the mantle to weaken, the continent to thin and the molten
material to rise to the surface&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;Scientists made the link between the volcanoes and the
warming period, known as the Paleocene-Eocene thermal maximum,
by matching layers of ash in east Greenland with those in
marine sediments in the Atlantic Ocean.&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/climate/" rel="tag"&gt;climate&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/disasters/" rel="tag"&gt;disasters&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/environment/" rel="tag"&gt;environment&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/geology/" rel="tag"&gt;geology&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/nature/" rel="tag"&gt;nature&lt;/a&gt;&lt;/div&gt;</description><clipSource>http://news.yahoo.com/s/nm/20070426/sc_nm/volcanoes_warming_dc_1</clipSource><pubDate>Fri, 27 Apr 2007 15:56:05 GMT</pubDate></item><item><title>Atmospheric Levels of Methane now have leveled off</title><link>http://clipmarks.com/clipmark/AD63AAD9-79D4-494D-A323-A8ECC51684E7/</link><description>&lt;b&gt;clipped by:&lt;/b&gt; &lt;a href="http://clipmarks.com/clipper/amgumen/"&gt;amgumen&lt;/a&gt;&lt;br&gt;&lt;b&gt;clipper's remarks:&lt;/b&gt;  Methane, a potent greenhouse gas, have been constant for five years after two centuries of steady increases. Scientists do not know why the pattern of increase has stopped.&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://cdiac.esd.ornl.gov/trends/otheratg/blake/methane/methane.html" title="http://cdiac.esd.ornl.gov/trends/otheratg/blake/methane/methane.html"&gt;cdiac.esd.ornl.gov&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/amgumen/512/40C2BD52-2C11-4B1D-B24A-D86E0DCC4C5D.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;Tags: &lt;a href="http://clipmarks.com/tags/climate+change/" rel="tag"&gt;climate change&lt;/a&gt;&lt;/div&gt;</description><clipSource>http://cdiac.esd.ornl.gov/trends/otheratg/blake/methane/methane.html</clipSource><pubDate>Sun, 22 Apr 2007 01:54:05 GMT</pubDate></item><item><title>Volcanic co2 Emission Vs Human</title><link>http://clipmarks.com/clipmark/2D72819F-F8A3-46BB-BB55-82504DEF65BA/</link><description>&lt;b&gt;clipped by:&lt;/b&gt; &lt;a href="http://clipmarks.com/clipper/Kingsmob77/"&gt;Kingsmob77&lt;/a&gt;&lt;br&gt;&lt;b&gt;clipper's remarks:&lt;/b&gt;  This is from the Department of the interior, USGS.  their findings show that humans generate a significantly higher amount of greenhouse gases than volcanoes.  &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://volcanoes.usgs.gov/Hazards/What/VolGas/volgas.html" title="http://volcanoes.usgs.gov/Hazards/What/VolGas/volgas.html"&gt;volcanoes.usgs.gov&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;H3&gt;Volcanic gases are the driving force of eruptions&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;P&gt;
&lt;B&gt;Comparison of CO&lt;FONT size="2"&gt;&lt;SUB&gt;2&lt;/SUB&gt;&lt;/FONT&gt; emissions from volcanoes vs. 
human activities.&lt;/B&gt;&lt;BR /&gt;
Scientists have calculated that volcanoes emit between 
about 130-230 million tonnes (145-255 million tons) of 
CO&lt;FONT size="2"&gt;&lt;SUB&gt;2&lt;/SUB&gt;&lt;/FONT&gt; into the atmosphere 
every year (&lt;A href="#reference"&gt;Gerlach, 1999,  
1992&lt;/A&gt;). This estimate includes both subaerial and 
submarine volcanoes, about in equal amounts. Emissions of 
CO&lt;FONT size="2"&gt;&lt;SUB&gt;2&lt;/SUB&gt;&lt;/FONT&gt; by human activities, including 
fossil fuel burning, cement production, and gas flaring, 
amount to about 22 billion tonnes per year (24 billion tons) [ (&lt;A href="#reference"&gt; Marland, et al., 1998&lt;/A&gt;) - The reference gives the amount of released carbon (C), rather than CO&lt;SUB&gt;2&lt;/SUB&gt;.].
Human activities release more than 150 times the amount of 
CO&lt;FONT size="2"&gt;&lt;SUB&gt;2&lt;/SUB&gt;&lt;/FONT&gt; emitted by volcanoes--the equivalent of nearly 17,000 additional volcanoes like Kilauea 
(Kilauea emits about 13.2 million tonnes/year)!&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/politics/" rel="tag"&gt;politics&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/nature/" rel="tag"&gt;nature&lt;/a&gt;&lt;/div&gt;</description><clipSource>http://volcanoes.usgs.gov/Hazards/What/VolGas/volgas.html</clipSource><pubDate>Tue, 06 Mar 2007 21:06:30 GMT</pubDate></item></channel></rss>