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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 | invictus's 'volcanoes' clips</title><link>http://clipmarks.com/clipper/invictus/search/volcanoes/sort/most-pops/</link><feedUrl>http://rss.clipmarks.com/clipper/invictus/search/volcanoes/sort/most-pops/</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>  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>Sunset on Mars </title><link>http://clipmarks.com/clipmark/C80730A8-6194-489A-A5C0-BB0DD66F1BC3/</link><description>&lt;b&gt;clipped by:&lt;/b&gt; &lt;a href="http://clipmarks.com/clipper/shunyax/"&gt;shunyax&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.nasa.gov/multimedia/imagegallery/image_feature_347.html" title="http://www.nasa.gov/multimedia/imagegallery/image_feature_347.html"&gt;www.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/shunyax/512/1AF31CDF-3B6F-4235-BEE2-7339C97F8128.jpg" alt="Sunset on Mars" /&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;Sunset on Mars&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;On May 19, 2005, NASA's Mars Exploration Rover Spirit captured this stunning view as the Sun sank below the rim of Gusev crater on Mars. This Panoramic Camera mosaic was taken around 6:07 in the evening of the rover's 489th Martian day, or sol.&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; Sunset and twilight images are occasionally acquired by the science team to determine how high into the atmosphere the Martian dust extends, and to look for dust or ice clouds. Other images have shown that the twilight glow remains visible, but increasingly fainter, for up to two hours before sunrise or after sunset. The long Martian twilight (compared to Earth's) is caused by sunlight scattered around to the night side of the planet by abundant high altitude dust. Similar long twilights or extra-colorful sunrises and sunsets sometimes occur on Earth when tiny dust grains that are erupted from powerful volcanoes scatter light high in the atmosphere.&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;&lt;/div&gt;</description><clipSource>http://www.nasa.gov/multimedia/imagegallery/image_feature_347.html</clipSource><pubDate>Sat, 07 Jun 2008 08:51:47 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>Great Volcano Pics</title><link>http://clipmarks.com/clipmark/811501E7-2AE3-4FFD-AA75-60F23FBA2FD9/</link><description>&lt;b&gt;clipped by:&lt;/b&gt; &lt;a href="http://clipmarks.com/clipper/CrazyRedHead/"&gt;CrazyRedHead&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://slightlywarped.com/crapfactory/amazingimages/volcanoes.htm" title="http://slightlywarped.com/crapfactory/amazingimages/volcanoes.htm"&gt;slightlywarped.com&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/CrazyRedHead/512/E6CA0EC2-289B-4FD4-BF87-57AA82B00D19.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 align="left"&gt;
      &lt;B&gt;&lt;FONT face="Verdana"&gt;In those few places in the Earth where the ground 
      opens and rock flows like water, we find a sight so breathtaking in both 
      its beauty and its danger that it holds us captivated at the raw unsurging 
      power beneath our feet.&lt;/FONT&gt;&lt;/B&gt;&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/CrazyRedHead/512/C429051C-D204-432B-B914-D6C01A822152.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/CrazyRedHead/512/4A0931A7-C85B-4958-BC1B-736E4D983F4F.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/CrazyRedHead/512/6105489C-9D1A-4EE5-84E9-9F7165B5CC7C.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/CrazyRedHead/512/7963B8AD-506E-440D-B5ED-2F8C1DE35BF5.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/CrazyRedHead/512/67152A74-2184-4163-BEAB-F5C903D52EEF.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/CrazyRedHead/512/B28E5BF5-571F-4275-BAD6-7AC4F8EE4821.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/CrazyRedHead/512/53DCE1F0-1E56-4AA4-A842-02D6B34421F9.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/CrazyRedHead/512/C0238AD1-9EDB-40C3-9A13-0F397350A8F0.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/CrazyRedHead/512/56DA1DBB-AB9C-402E-BA12-D395BD9D3625.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/photography/" rel="tag"&gt;photography&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://slightlywarped.com/crapfactory/amazingimages/volcanoes.htm</clipSource><pubDate>Wed, 10 Oct 2007 06:16:37 GMT</pubDate></item><item><title>The Earth fights back</title><link>http://clipmarks.com/clipmark/891D237E-4D3C-4531-B74B-28DA597C11CE/</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://www.guardian.co.uk/science/2007/aug/07/disasters?gusrc=rss&amp;feed=science" title="http://www.guardian.co.uk/science/2007/aug/07/disasters?gusrc=rss&amp;feed=science"&gt;www.guardian.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;P id="stand-first"&gt;Never mind higher temperatures, climate change has a few nastier surprises in store. Bill McGuire says we can also expect more earthquakes, volcanoes, landslides and tsunamis&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/JohnWaterman/512/601AF3C4-6EBB-4EFB-BCBC-FDDA1DDA93CA.jpg" alt="The eruption of Augustine Volcano in Alaska " /&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;Unlike most apparently intractable problems, which have a tendency to go away when examined closely and analytically, the climate change predicament just seems to get bigger and scarier the more we learn about it.&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; periods in our planet's history when the climate was swinging about wildly, most notably during the last ice age, it appears that far more than the weather was affected&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 increase in volcanic activity, earthquakes, giant submarine landslides and tsunamis&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;there was a close correlation between how quickly sea levels went up and down during the last ice age and the level of explosive activity at volcanoes in Italy and Greece&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; how can rising sea levels cause volcanoes to erupt?&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;answer lies in the enormous mass of the water pouring into the ocean basins&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;seems to be sufficient to load and bend the underlying crust.&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/earth/" rel="tag"&gt;earth&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/global+warming/" rel="tag"&gt;global warming&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/earthquakes/" rel="tag"&gt;earthquakes&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/volcanooes/" rel="tag"&gt;volcanooes&lt;/a&gt;&lt;/div&gt;</description><clipSource>http://www.guardian.co.uk/science/2007/aug/07/disasters?gusrc=rss&amp;feed=science</clipSource><pubDate>Tue, 07 Aug 2007 17:40:43 GMT</pubDate></item><item><title>Birth of an Island</title><link>http://clipmarks.com/clipmark/4FB943B1-1014-4852-BE7D-33789D67E00C/</link><description>&lt;b&gt;clipped by:&lt;/b&gt; &lt;a href="http://clipmarks.com/clipper/axelsenzon/"&gt;axelsenzon&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.boreme.com/boreme/funny-2007/south-pacific-island-p1.php" title="http://www.boreme.com/boreme/funny-2007/south-pacific-island-p1.php"&gt;www.boreme.com&lt;/a&gt;&lt;/span&gt;&lt;/div&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 align="center" class="v12-black"&gt;
August 2006, the yacht 'Maiken' is travelling in the south Pacific when they came across a weird sight...
&lt;BR /&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;img src="http://clipmarks.com/image_cache/axelsenzon/512/9101AFA2-0D57-466E-A7E6-E664D592A511.jpg" alt="South Pacific island" /&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.boreme.com/boreme/funny-2007/south-pacific-island-p2.php" title="http://www.boreme.com/boreme/funny-2007/south-pacific-island-p2.php"&gt;www.boreme.com&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/axelsenzon/512/6AD5FA4A-3AF2-4C3D-B647-B90B21305378.jpg" alt="South Pacific island" /&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.boreme.com/boreme/funny-2007/south-pacific-island-p3.php" title="http://www.boreme.com/boreme/funny-2007/south-pacific-island-p3.php"&gt;www.boreme.com&lt;/a&gt;&lt;/span&gt;&lt;/div&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 align="center" class="v12-black"&gt;
This is not a beach, it is volcanic stones floating on the water.
&lt;BR /&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;img src="http://clipmarks.com/image_cache/axelsenzon/512/04495A6D-9EFA-45B0-9351-1FC1109E9C36.jpg" alt="South Pacific island" /&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.boreme.com/boreme/funny-2007/south-pacific-island-p4.php" title="http://www.boreme.com/boreme/funny-2007/south-pacific-island-p4.php"&gt;www.boreme.com&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/axelsenzon/512/6C1BEFA2-E6A6-403F-83C9-02C2D82BCB35.jpg" alt="South Pacific island" /&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.boreme.com/boreme/funny-2007/south-pacific-island-p5.php" title="http://www.boreme.com/boreme/funny-2007/south-pacific-island-p5.php"&gt;www.boreme.com&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/axelsenzon/512/0C07CAB4-655D-4BFC-8A93-94AC1810293B.jpg" alt="South Pacific island" /&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.boreme.com/boreme/funny-2007/south-pacific-island-p6.php" title="http://www.boreme.com/boreme/funny-2007/south-pacific-island-p6.php"&gt;www.boreme.com&lt;/a&gt;&lt;/span&gt;&lt;/div&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 align="center" class="v12-black"&gt;
The trail left by the yacht...
&lt;BR /&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;img src="http://clipmarks.com/image_cache/axelsenzon/512/F1D1586E-0075-45AC-AB96-97342076BAC1.jpg" alt="South Pacific island" /&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.boreme.com/boreme/funny-2007/south-pacific-island-p7.php" title="http://www.boreme.com/boreme/funny-2007/south-pacific-island-p7.php"&gt;www.boreme.com&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/axelsenzon/512/6DBB6D0C-B4CC-4F0F-A963-F148714F778F.jpg" alt="South Pacific island" /&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.boreme.com/boreme/funny-2007/south-pacific-island-p8.php" title="http://www.boreme.com/boreme/funny-2007/south-pacific-island-p8.php"&gt;www.boreme.com&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/axelsenzon/512/3D721513-E2BA-44F1-88CF-56BA6DFAA4D7.jpg" alt="South Pacific island" /&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.boreme.com/boreme/funny-2007/south-pacific-island-p9.php" title="http://www.boreme.com/boreme/funny-2007/south-pacific-island-p9.php"&gt;www.boreme.com&lt;/a&gt;&lt;/span&gt;&lt;/div&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 align="center" class="v12-black"&gt;
And then this was spotted... ash and steam rising from the ocean...
&lt;BR /&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;img src="http://clipmarks.com/image_cache/axelsenzon/512/19BBCABB-3C1B-4BF0-B3CD-11C936D126CB.jpg" alt="South Pacific island" /&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.boreme.com/boreme/funny-2007/south-pacific-island-p10.php" title="http://www.boreme.com/boreme/funny-2007/south-pacific-island-p10.php"&gt;www.boreme.com&lt;/a&gt;&lt;/span&gt;&lt;/div&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 align="center" class="v12-black"&gt;
And, while they were watching...
&lt;BR /&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;img src="http://clipmarks.com/image_cache/axelsenzon/512/B9317AA9-BC61-46AC-ADEE-2599BA7F1229.jpg" alt="South Pacific island" /&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.boreme.com/boreme/funny-2007/south-pacific-island-p11.php" title="http://www.boreme.com/boreme/funny-2007/south-pacific-island-p11.php"&gt;www.boreme.com&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/axelsenzon/512/04B7B5C1-2FE9-40FE-AD36-E7193D2A4D8D.jpg" alt="South Pacific island" /&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.boreme.com/boreme/funny-2007/south-pacific-island-p12.php" title="http://www.boreme.com/boreme/funny-2007/south-pacific-island-p12.php"&gt;www.boreme.com&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/axelsenzon/512/1B434531-8684-4F4D-85FE-D57A7A01DAF7.jpg" alt="South Pacific island" /&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.boreme.com/boreme/funny-2007/south-pacific-island-p13.php" title="http://www.boreme.com/boreme/funny-2007/south-pacific-island-p13.php"&gt;www.boreme.com&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/axelsenzon/512/49892F2B-ADEB-40CE-8E76-D2BD16DE584A.jpg" alt="South Pacific island" /&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.boreme.com/boreme/funny-2007/south-pacific-island-p14.php" title="http://www.boreme.com/boreme/funny-2007/south-pacific-island-p14.php"&gt;www.boreme.com&lt;/a&gt;&lt;/span&gt;&lt;/div&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 align="center" class="v12-black"&gt;
A brand new island formed...
&lt;BR /&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;img src="http://clipmarks.com/image_cache/axelsenzon/512/801B4E7D-13FE-4BE4-BD1D-3AB6FF48E909.jpg" alt="South Pacific island" /&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.boreme.com/boreme/funny-2007/south-pacific-island-p15.php" title="http://www.boreme.com/boreme/funny-2007/south-pacific-island-p15.php"&gt;www.boreme.com&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/axelsenzon/512/E24385EA-72DF-4E98-9F73-ED80F1D47E3D.jpg" alt="South Pacific island" /&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.boreme.com/boreme/funny-2007/south-pacific-island-p16.php" title="http://www.boreme.com/boreme/funny-2007/south-pacific-island-p16.php"&gt;www.boreme.com&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/axelsenzon/512/04E0E311-DAF5-431D-9885-8A8B2673A124.jpg" alt="South Pacific island" /&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.boreme.com/boreme/funny-2007/south-pacific-island-p17.php" title="http://www.boreme.com/boreme/funny-2007/south-pacific-island-p17.php"&gt;www.boreme.com&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/axelsenzon/512/B8FDD6CB-F6D9-41DB-BA58-E56AA155F813.jpg" alt="South Pacific island" /&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.boreme.com/boreme/funny-2007/south-pacific-island-p18.php" title="http://www.boreme.com/boreme/funny-2007/south-pacific-island-p18.php"&gt;www.boreme.com&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/axelsenzon/512/8661BC46-6DCA-4EBD-929F-0ADACE95B708.jpg" alt="South Pacific island" /&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/nature/" rel="tag"&gt;nature&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/amazing/" rel="tag"&gt;amazing&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/volcanoes/" rel="tag"&gt;volcanoes&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/pics/" rel="tag"&gt;pics&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/ocean/" rel="tag"&gt;ocean&lt;/a&gt;&lt;/div&gt;</description><clipSource>http://www.boreme.com/boreme/funny-2007/south-pacific-island-p1.php</clipSource><pubDate>Thu, 21 Jun 2007 18:39:17 GMT</pubDate></item><item><title>Bio-Earth: Are Planets Living Super-Organisms?</title><link>http://clipmarks.com/clipmark/39632EA6-C1BB-48E1-8C46-C3157FA551BC/</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;  He believes that expanding the study of life sciences to the core of our world and the depths of outer space will help us find distant relatives of our own Earth -- planets that could also sustain life.&lt;br/&gt;To explain why contintental plates drift on the surface of the Earth's molten mantle, Maruyama argues that continents actually have life cycles. Old, cold plates on continental fringes sink to “plate graveyards” deep in the Earth’s mantle, and then rise again, creating volcanoes fueled by three-dimensional convection movements deep below the 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.dailygalaxy.com/my_weblog/2008/07/bio-earth-plane.html" title="http://www.dailygalaxy.com/my_weblog/2008/07/bio-earth-plane.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/FB498C2B-80D5-4E3A-B914-BA9D2ADED6F3.jpg" alt="Volcano_2" /&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;
Japan's Maruyama Shigenori, one of the world's leading geophysicists, is working on a global formula for a vast new field of study
that would include dozens of disciplines collaborating to produce an
overall picture of the Earth.&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;Maruyama is creating a new institute called the Center for Bio-Earth Planetology will be
launched in 2009 and fully dedicated to creating a new conception of
life in space.He wants to find out if the continents will
merge again in 250 million years to form a single super-continent; how
meteorites change the chemical composition of the Earth; and what the
connection is between the temperature of a planet and its magnetic
field, which protects plants and animals from
being bombarded with cosmic radiation, which in turn influences the
rate of mutations and thus the development of new forms of life.&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;
As he connects the dots from astronomy to life sciences, the outlines
emerge of an all-encompassing image of entire planets, which appear as
living super-organisms.&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/planet/" rel="tag"&gt;planet&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/gaia/" rel="tag"&gt;gaia&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/geophysics/" rel="tag"&gt;geophysics&lt;/a&gt;&lt;/div&gt;</description><clipSource>http://www.dailygalaxy.com/my_weblog/2008/07/bio-earth-plane.html</clipSource><pubDate>Fri, 11 Jul 2008 17:48:23 GMT</pubDate></item><item><title>Our Earth as Art</title><link>http://clipmarks.com/clipmark/D93826CB-F13E-49B6-9264-0351F07F2F7E/</link><description>&lt;b&gt;clipped by:&lt;/b&gt; &lt;a href="http://clipmarks.com/clipper/Aribeth/"&gt;Aribeth&lt;/a&gt;&lt;br&gt;&lt;b&gt;clipper's remarks:&lt;/b&gt;  Welcome to the Earth as Art Gallery.Here you can view our planet through the beautiful images taken by the Landsat-7 satellite - and most recently, the Terra Satellite's Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER). This gallery of images uses the visceral avenue of art to convey the thrilling perspective of the Earth that satellites provide to the viewer. &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://earthasart.gsfc.nasa.gov/image_index.html" title="http://earthasart.gsfc.nasa.gov/image_index.html"&gt;earthasart.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/Aribeth/512/21DA0B43-62E7-432D-B480-F065C7F4B312.jpg" alt="Earth As Art: View the Earth 
through the eyes of the Landsat-7 satellite" /&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://earthasart.gsfc.nasa.gov/akpatok.html" title="http://earthasart.gsfc.nasa.gov/akpatok.html"&gt;earthasart.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;

Akpatok 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;northern Quebec, Canada&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/Aribeth/512/D4BEF3D8-FAC5-4751-B341-B8C410847CBC.jpg" alt="An icy looking lung shaped 
plateu" /&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://earthasart.gsfc.nasa.gov/aleutian.html" title="http://earthasart.gsfc.nasa.gov/aleutian.html"&gt;earthasart.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;

Aleutian Clouds&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/Aribeth/512/39C1C6E2-4C90-4429-88B8-9B8CF824C913.jpg" alt="Cloud formations colored green, blue, and orange" /&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://earthasart.gsfc.nasa.gov/alluvial.html" title="http://earthasart.gsfc.nasa.gov/alluvial.html"&gt;earthasart.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;

Alluvial Fan, China&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/Aribeth/512/D25FAB64-1B82-4464-97AD-D8F7C362BD04.jpg" alt="Alluvial Fan, China" /&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://earthasart.gsfc.nasa.gov/bogda.html" title="http://earthasart.gsfc.nasa.gov/bogda.html"&gt;earthasart.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;

Bogda Mountains&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/Aribeth/512/87EE3A24-3D6F-4D75-8478-A8382802B496.jpg" alt="Bogda Mountains" /&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://earthasart.gsfc.nasa.gov/bolivian.html" title="http://earthasart.gsfc.nasa.gov/bolivian.html"&gt;earthasart.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;

Bolivian Deforestation&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/Aribeth/512/49C85691-A49B-4290-80B1-68B20030CC4E.jpg" alt="Patchwork squares 
 showing clearings in the forest" /&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://earthasart.gsfc.nasa.gov/cancun.html" title="http://earthasart.gsfc.nasa.gov/cancun.html"&gt;earthasart.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;

Cancun&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;Mexico's Yucatan Peninsula&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/Aribeth/512/8A8F8B1F-B6B2-430B-B1F8-1108C651EE0F.jpg" alt="Cancun" /&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://earthasart.gsfc.nasa.gov/campeche.html" title="http://earthasart.gsfc.nasa.gov/campeche.html"&gt;earthasart.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;

Campeche&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;Mexico's Yucatan Peninsula&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/Aribeth/512/7E54E76F-7882-4B98-8884-741A5EA6DE52.jpg" alt="Campeche" /&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://earthasart.gsfc.nasa.gov/chile.html" title="http://earthasart.gsfc.nasa.gov/chile.html"&gt;earthasart.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;

Chilean Volcanoes&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/Aribeth/512/FCA1C58D-468D-4ECE-8714-1D1F38052B48.jpg" alt="Volcanoes scattered around mountainous area." /&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://earthasart.gsfc.nasa.gov/colima.html" title="http://earthasart.gsfc.nasa.gov/colima.html"&gt;earthasart.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;

Colima 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;Mexico&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/Aribeth/512/B6399715-C9B1-41FC-8F9B-2D2FC2BAA784.jpg" alt="Colima Volcano" /&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://earthasart.gsfc.nasa.gov/netherland.html" title="http://earthasart.gsfc.nasa.gov/netherland.html"&gt;earthasart.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;

Delta Region, Netherlands&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/Aribeth/512/70B4DC28-1038-491A-8B1E-5A65D4F7956A.jpg" alt="Delta Region, Netherlands" /&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://earthasart.gsfc.nasa.gov/demini.html" title="http://earthasart.gsfc.nasa.gov/demini.html"&gt;earthasart.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;

Demini River&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;Brazil&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/Aribeth/512/541AD3C7-B543-407B-829D-27F51E8B9E60.jpg" alt="Marsh and Rivers" /&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://earthasart.gsfc.nasa.gov/desolat.html" title="http://earthasart.gsfc.nasa.gov/desolat.html"&gt;earthasart.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;

Desolation Canyon&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;American West&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/Aribeth/512/BEBECD55-5D82-4608-A66D-C0519ED01C6E.jpg" alt="Desolation Canyon" /&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://earthasart.gsfc.nasa.gov/everglades.html" title="http://earthasart.gsfc.nasa.gov/everglades.html"&gt;earthasart.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;

Florida Everglades&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/Aribeth/512/CE437CE1-05E0-4ADD-9020-44CF7302ACEF.jpg" alt="Image shows Everglades." /&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://earthasart.gsfc.nasa.gov/ghadamis.html" title="http://earthasart.gsfc.nasa.gov/ghadamis.html"&gt;earthasart.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;

Ghadamis River&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;Libya&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/Aribeth/512/274884F6-62EF-447F-8A5A-BF492FD273EC.jpg" alt="Scar looks like veins or fern plants." /&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://earthasart.gsfc.nasa.gov/salt.html" title="http://earthasart.gsfc.nasa.gov/salt.html"&gt;earthasart.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;

Great Salt Desert&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/Aribeth/512/6506D31A-CC4B-4131-852D-C122491051FB.jpg" alt="Great Salt Desert" /&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://earthasart.gsfc.nasa.gov/scar.html" title="http://earthasart.gsfc.nasa.gov/scar.html"&gt;earthasart.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;

Great Sandy Scars&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;Western Australia&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/Aribeth/512/FB388E12-A19D-4F1C-812E-18C0A352FF16.jpg" alt="The desert looks like sheets of rock that have a mottled
color." /&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://earthasart.gsfc.nasa.gov/guinea.html" title="http://earthasart.gsfc.nasa.gov/guinea.html"&gt;earthasart.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;

Guinea-Bissau&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/Aribeth/512/6B93FD7F-C519-4235-A03D-21334CA7CCB2.jpg" alt="Blue water, cracked and creviced shoreline." /&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://earthasart.gsfc.nasa.gov/himalayas.html" title="http://earthasart.gsfc.nasa.gov/himalayas.html"&gt;earthasart.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;

The Himalayas&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/Aribeth/512/30C50FCE-5394-4994-A7E4-69E4479272B1.jpg" alt="The Himalayas" /&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://earthasart.gsfc.nasa.gov/icefall.html" title="http://earthasart.gsfc.nasa.gov/icefall.html"&gt;earthasart.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;

Icefall, Lambert Glacier, Antarctica&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/Aribeth/512/B6D396C6-6F4D-473E-813D-964EC5EF158F.jpg" alt="Grooves worn on the surface of a blue glacier" /&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://earthasart.gsfc.nasa.gov/jordan.html" title="http://earthasart.gsfc.nasa.gov/jordan.html"&gt;earthasart.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;

Jordan&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/Aribeth/512/32A16737-9B44-49E5-AA52-3300800C6C2A.jpg" alt="Jordan" /&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://earthasart.gsfc.nasa.gov/carnegie.html" title="http://earthasart.gsfc.nasa.gov/carnegie.html"&gt;earthasart.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;

Lake Carnegie&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/Aribeth/512/343FBEB2-D59D-4847-8097-73A597F1EF7A.jpg" alt="The desert looks like sheets of rock that have a mottled
color." /&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://earthasart.gsfc.nasa.gov/malaspina.html" title="http://earthasart.gsfc.nasa.gov/malaspina.html"&gt;earthasart.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;

Malaspina Glacier&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;Alaska&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/Aribeth/512/60D8EBF9-6A65-42DD-8870-790C830FD52E.jpg" alt="A large glacier - blue with ripples spreading out." /&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://earthasart.gsfc.nasa.gov/etna.html" title="http://earthasart.gsfc.nasa.gov/etna.html"&gt;earthasart.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;

Mt. Etna&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;Sicily&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/Aribeth/512/344CDBAD-6E89-4CB6-B4E6-E34A391A1B6A.jpg" alt="Mt. Etna" /&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://earthasart.gsfc.nasa.gov/namib.html" title="http://earthasart.gsfc.nasa.gov/namib.html"&gt;earthasart.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;

Namib Desert, Namibia&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/Aribeth/512/DF930EE7-BE6E-4620-B851-92177924E3BB.jpg" alt="Rippling Sand Dunes with scar running horizontally down middle of 
image." /&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://earthasart.gsfc.nasa.gov/bahamas.html" title="http://earthasart.gsfc.nasa.gov/bahamas.html"&gt;earthasart.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;

Ocean Sand, Bahamas&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/Aribeth/512/E93DF95B-144F-4880-BC00-C451C08E359E.jpg" alt="Image shows ocean sand at the Bahamas." /&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://earthasart.gsfc.nasa.gov/syrian.html" title="http://earthasart.gsfc.nasa.gov/syrian.html"&gt;earthasart.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;

Syrian Desert&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/Aribeth/512/7D6C90D2-51EB-4469-BC3E-E934BAA77473.jpg" alt="Syrian Desert" /&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://earthasart.gsfc.nasa.gov/vatna.html" title="http://earthasart.gsfc.nasa.gov/vatna.html"&gt;earthasart.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;

Vatnajökull Glacier Ice Cap&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;Iceland's 
                Skaftafell National Park&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/Aribeth/512/C9BB621C-099D-4CAB-9F27-6457021EC9EA.jpg" alt="Vatnajökull Glacier Ice Cap" /&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://earthasart.gsfc.nasa.gov/index.htm" title="http://earthasart.gsfc.nasa.gov/index.htm"&gt;earthasart.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;AREA coords="217,91,307,91,346,140,360,216,284,237,216,145" shape="poly" title="Africa" alt="Africa" href="http://earthasart.gsfc.nasa.gov/africa.html"&gt;&lt;/AREA&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/Aribeth/512/5EDA63EF-3B5D-4094-B9D5-CA4CEF7272D3.gif" alt="USGS &amp; NASA logos" /&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/pics/" rel="tag"&gt;pics&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/images/" rel="tag"&gt;images&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/photo/" rel="tag"&gt;photo&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/photos/" rel="tag"&gt;photos&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/gallery/" rel="tag"&gt;gallery&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/beautiful/" rel="tag"&gt;beautiful&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/satellite/" rel="tag"&gt;satellite&lt;/a&gt;&lt;/div&gt;</description><clipSource>http://earthasart.gsfc.nasa.gov/image_index.html</clipSource><pubDate>Wed, 05 Dec 2007 18:19:57 GMT</pubDate></item><item><title>Unreal Landscapes of the Bolivian Salt Lake</title><link>http://clipmarks.com/clipmark/930FB1B2-19ED-4615-9D91-774DB8BB4F98/</link><description>&lt;b&gt;clipped by:&lt;/b&gt; &lt;a href="http://clipmarks.com/clipper/abramsv/"&gt;abramsv&lt;/a&gt;&lt;br&gt;&lt;b&gt;clipper's remarks:&lt;/b&gt;  The Bolivia's Salar de Uyuni is perhaps one of the most spectacular landscapes in the world. A magnificent area with an impressive Salt Desert (the world's largest), active volcanoes, tall cacti islands and geyser flats, it exists like an alien mirage, something completely out-of-this-world... &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://thrillingwonder.blogspot.com/2006/11/fantastic-landscapes-of-bolivian-salt_27.html" title="http://thrillingwonder.blogspot.com/2006/11/fantastic-landscapes-of-bolivian-salt_27.html"&gt;thrillingwonder.blogspot.com&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;H3 class="post-title"&gt;
                      	 &lt;A title="external%20%0D%0A%0D%0Alink" href="http://thrillingwonder.blogspot.com/2006/11/fantastic-landscapes-of-bolivian-salt_27.html"&gt;
                      	 Fantastic Landscapes of the Bolivian Salt Lake
	                       &lt;/A&gt;
                          &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;B&gt;Salar de Uyuni - Bolivian Salt Lake and islands&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;&lt;DIV&gt;The Bolivia's Salar de Uyuni is perhaps one of the most spectacular landscapes in the world. A magnificent area with an impressive Salt Desert (the world's largest), active volcanos, tall cacti islands and geyser flats, it exists like an alien mirage,  something completely out-of-this-world...&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/abramsv/512/5D2C35B8-6AAB-47F0-8B34-AD88C092F053.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/abramsv/512/B7D3C172-EE93-4305-9481-9D6186E110A7.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;I&gt;"...We finally reached the salt flats. Imagine being surrounded by endless white salt covered by a few inches of water. Without any reference points the sky meets the salt and creates an odd illusion that objects in the flats are flying. I had never seen anything like it... The truck drove through the salt flats and stopped at an island full of cacti. We had lunch on a table made of a large salt tablet and eventually stopped at a hotel made completely of salt."&lt;/I&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/abramsv/512/767B75AF-1FA8-4C0E-A911-D0A3EEECFC74.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/abramsv/512/78D9799A-2720-403E-9350-E326BF511E0D.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/abramsv/512/DE817D10-73DE-417A-892E-3D07563766CA.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/abramsv/512/592E100A-A66A-4CB4-BD98-850D8CB1A16D.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/abramsv/512/068C89B6-F6DE-4F78-9C36-A043575C0A89.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/abramsv/512/12BA6986-C05A-47E4-9B62-B850A434FC00.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/travel/" rel="tag"&gt;travel&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/photography/" rel="tag"&gt;photography&lt;/a&gt;&lt;/div&gt;</description><clipSource>http://thrillingwonder.blogspot.com/2006/11/fantastic-landscapes-of-bolivian-salt_27.html</clipSource><pubDate>Tue, 28 Nov 2006 05:54:48 GMT</pubDate></item><item><title>Surprising Activity Discovered at Yellowstone Supervolcano</title><link>http://clipmarks.com/clipmark/6E636D67-6302-4D24-A9CB-EC28A40E2252/</link><description>&lt;b&gt;clipped by:&lt;/b&gt; &lt;a href="http://clipmarks.com/clipper/invictus/"&gt;invictus&lt;/a&gt;&lt;br&gt;&lt;b&gt;clipper's remarks:&lt;/b&gt;  &lt;blockquote&gt;What the researchers think is happening, on a short-term basis at least, is that the bulging Yellowstone hotspot north of the Tetons is pushing against the north edge of Jackson Hole and jamming it against the mountains. (This is also causing the southwest part of the Yellowstone plateau, under the hotspot, to slide downhill at a rate of one-sixth of an inch each year.).&lt;/blockquote&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/forcesofnature/070307_yellowstone_shape.html" title="http://www.livescience.com/forcesofnature/070307_yellowstone_shape.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 class="style1"&gt;Supervolcanoes can sleep for centuries or millennia before
producing incredibly massive eruptions that can drop ash across an entire
continent. One of the largest &lt;A href="http://www.livescience.com/forcesofnature/050308_super_volcano.html"&gt;supervolcanoes&lt;/A&gt;
in the world lies beneath &lt;A href="http://www.livescience.com/php/video/player.php?video_id=yellowstone_quest"&gt;Yellowstone
National Park&lt;/A&gt;, which spans parts of Wyoming, Montana and Idaho. &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 class="style1"&gt;Though the Yellowstone system is active and expected to
eventually blow its top, scientists don’t think it will &lt;A href="http://www.livescience.com/forcesofnature/050308_super_volcano.html"&gt;erupt&lt;/A&gt;
any time soon. &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 class="style1"&gt;Yet &lt;A href="http://cms.space.com/livescience/storage/article/Yellowstone%20Volcano%20Grows%20as%20Geysers%20Reawaken"&gt;significant
activity continues&lt;/A&gt; beneath the surface. And the activity has been
increasing lately, scientists have discovered. In addition, the nearby &lt;A href="http://www.livescience.com/php/multimedia/imagedisplay/img_display.php?pic=070306_jackson_hole_02.jpg∩=Wyoming%27s+Teton+Range+looms+behind+a+Global+Positioning+System+%28GPS%29+antenna+in+Jackson+Hole.+Credit:+Jamie+Farrell%2C+University+of+Utah."&gt;Teton
Range&lt;/A&gt;, in a total surprise, is getting shorter.&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 class="style1"&gt;The findings, reported this month in the &lt;EM&gt;&lt;SPAN&gt;Journal of Geophysical Research—Solid Earth&lt;/SPAN&gt;&lt;/EM&gt;,
suggest that a slow and gradual movement caused by a giant hotspot of molten
rock beneath a &lt;A href="http://www.livescience.com/volcanoes/"&gt;volcano&lt;/A&gt; can
shape a landscape more than sudden ground movements caused by the volcano’s
frequent earthquakes.  &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/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/yellowstone/" rel="tag"&gt;yellowstone&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/eruption/" rel="tag"&gt;eruption&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/caldera/" rel="tag"&gt;caldera&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/fault+lines/" rel="tag"&gt;fault lines&lt;/a&gt;&lt;/div&gt;</description><clipSource>http://www.livescience.com/forcesofnature/070307_yellowstone_shape.html</clipSource><pubDate>Thu, 15 Mar 2007 22:41:43 GMT</pubDate></item><item><title>Ancient Chaiten Volcano Erupts after 10,000 Years</title><link>http://clipmarks.com/clipmark/5034DD8B-BE84-400F-B662-5EBC28B3EC4C/</link><description>&lt;b&gt;clipped by:&lt;/b&gt; &lt;a href="http://clipmarks.com/clipper/BobbyDelray/"&gt;BobbyDelray&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/story/_a/eruption-leaves-chilean-town-deserted/20080502193109990001?icid=1615988631x1201521334x1200303489" title="http://news.aol.com/story/_a/eruption-leaves-chilean-town-deserted/20080502193109990001?icid=1615988631x1201521334x1200303489"&gt;news.aol.com&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/BobbyDelray/512/032EE46D-F85E-4DC6-8562-DFF6E56FC942.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;The Chaiten volcano spewed light ash on a nearly deserted village Saturday, two days after its first eruption in thousands of years&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;Just six miles away, the volcano belched fat smoke plumes that at times rose as high as 12 miles into the air, the government's Emergency Bureau said.&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;Winds carried the ash to other towns in the region and across the Andes mountains to Argentina, where two airlines suspended flights due to poor visibility.&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 Chaiten volcano has "probably been dormant for about 9,000 or 10,000 years but that's not unusual," said Charles Stern, a professor of volcanology at the University of Colorado who specializes in Andes volcanoes.&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;"This could be the end of our town," &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;"We have worked an entire life here and now all we could do was to put a few things in a bag and depart, leaving everything behind."&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.aol.com/story/_a/eruption-leaves-chilean-town-deserted/20080502193109990001?icid=1615988631x1201521334x1200303489</clipSource><pubDate>Sun, 04 May 2008 03:28:22 GMT</pubDate></item><item><title>Mass extinctions? Blame it on the ocean</title><link>http://clipmarks.com/clipmark/603B44A7-DAA4-4595-874A-FF6B7F78969C/</link><description>&lt;b&gt;clipped by:&lt;/b&gt; &lt;a href="http://clipmarks.com/clipper/invictus/"&gt;invictus&lt;/a&gt;&lt;br&gt;&lt;b&gt;clipper's remarks:&lt;/b&gt;  &lt;blockquote&gt;In the course of hundreds of millions of years the world's oceans have expanded and contracted in response to the shifting of the Earth's tectonic plates and to changes in climate. There were periods of the planet's history when vast areas of the continents were flooded by shallow seas such as the shark and mosasaur infested seaway that neatly split North America during the age of the dinosaurs.&lt;br/&gt;&lt;br/&gt;As those epicontinental seas drained, animals like mosasaurs and giant sharks went extinct, and conditions on the marine shelves where life exhibited its greatest diversity in the form of things like clams and snails changed as well. &lt;/blockquote&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.nsf.gov/news/news_summ.jsp?cntn_id=111722&amp;org=NSF" title="http://www.nsf.gov/news/news_summ.jsp?cntn_id=111722&amp;org=NSF"&gt;www.nsf.gov&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;STRONG&gt;Ebb and flow of the sea is the primary cause of the world's mass extinctions over the past 500 million years&lt;/STRONG&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/invictus/512/FE753C9C-3EA9-4FA1-BEFF-A83FD6734889.jpg" alt="Fossils of crinoids, commonly known as sea lilies, from Ontario, Canada." /&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;If you are curious about Earth's periodic mass extinction events such as the sudden demise of the dinosaurs 65 million years ago, you might consider crashing asteroids and sky-darkening super volcanoes as culprits.&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;But a new study, published June 15, 2008, in the journal &lt;EM&gt;Nature&lt;/EM&gt;, suggests that it is the ocean, and in particular the epic ebbs and flows of sea level and sediment over the course of geologic time, that is the primary cause of the world's periodic mass extinctions over the past 500 million years.&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;I&gt;View  &lt;A href="http://nsfgov.httpsvc.vitalstreamcdn.com/nsfgov_vitalstream_com/fossil.swf"&gt;a video interview&lt;/A&gt; with geoscientist Shanan Peters.&lt;/I&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/mass+extinctions/" rel="tag"&gt;mass extinctions&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/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.nsf.gov/news/news_summ.jsp?cntn_id=111722&amp;org=NSF</clipSource><pubDate>Thu, 19 Jun 2008 16:19:31 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>The Physics of Interstellar Travel - by Dr. Michio Kaku</title><link>http://clipmarks.com/clipmark/599925F9-9769-4CA5-9401-C6AEB5712E38/</link><description>&lt;b&gt;clipped by:&lt;/b&gt; &lt;a href="http://clipmarks.com/clipper/Djiezes/"&gt;Djiezes&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.mkaku.org/article_intertravel.htm" title="http://www.mkaku.org/article_intertravel.htm"&gt;www.mkaku.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 class="style9"&gt;The Physics of Interstellar Travel &lt;A name="top"&gt;&lt;/A&gt;&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 id="article-tag"&gt;&lt;EM&gt;To one day, reach the stars.&lt;/EM&gt;&lt;BR /&gt;
        &lt;STRONG&gt;By Michio Kaku&lt;/STRONG&gt;&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 first realistic attempt to analyze extra-terrestrial civilizations from the point of view of the laws of physics and the laws of thermodynamics was by Russian astrophysicist Nicolai Kardashev. He based his ranking of possible civilizations on the basis of total energy output which could be quantified and used as a guide to explore the dynamics of advanced civilizations:&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;Type I: this civilization harnesses the energy output of an entire planet.&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;Type II: this civilization harnesses the energy output of a star, and generates about 10 billion times the energy output of a Type I civilization. &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;Type III: this civilization harnesses the energy output of a galaxy, or about 10 billion time the energy output of a Type II civilization.&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;Type 0:&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;UL&gt;
      &lt;LI&gt;Chemical rockets 
      &lt;/LI&gt;&lt;LI&gt;Ionic engines 
      &lt;/LI&gt;&lt;LI&gt;Fission power 
      &lt;/LI&gt;&lt;LI&gt;EM propulsion (rail guns)&lt;/LI&gt;
    &lt;/UL&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;Type I&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;UL&gt;
      &lt;LI&gt;Ram-jet fusion engines 
      &lt;/LI&gt;&lt;LI&gt;Photonic drive&lt;/LI&gt;
    &lt;/UL&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;Type II&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;UL&gt;
      &lt;LI&gt;Antimatter drive 
      &lt;/LI&gt;&lt;LI&gt;Von Neumann nano probes&lt;/LI&gt;
    &lt;/UL&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;Type III&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;UL&gt;
      &lt;LI&gt;Planck energy propulsion&lt;/LI&gt;
    &lt;/UL&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;A Type I civilization would be able to manipulate truly planetary energies. They might, for example, control or modify their weather. They would have the power to manipulate planetary phenomena, such as hurricanes, which can release the energy of hundreds of hydrogen bombs. Perhaps volcanoes or even earthquakes may be altered by such a civilization.&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/physics/" rel="tag"&gt;physics&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/sf/" rel="tag"&gt;sf&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/scifi/" rel="tag"&gt;scifi&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/michio+kaku/" rel="tag"&gt;michio kaku&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/kaku/" rel="tag"&gt;kaku&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/article/" rel="tag"&gt;article&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/essay/" rel="tag"&gt;essay&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/space/" rel="tag"&gt;space&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/space+travel/" rel="tag"&gt;space travel&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/civilizations/" rel="tag"&gt;civilizations&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/kardashev/" rel="tag"&gt;kardashev&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/energy/" rel="tag"&gt;energy&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/travel/" rel="tag"&gt;travel&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/et/" rel="tag"&gt;et&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/type/" rel="tag"&gt;type&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/types/" rel="tag"&gt;types&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/literature/" rel="tag"&gt;literature&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/interstellar/" rel="tag"&gt;interstellar&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/astronomy/" rel="tag"&gt;astronomy&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/light/" rel="tag"&gt;light&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/speed/" rel="tag"&gt;speed&lt;/a&gt;&lt;/div&gt;</description><clipSource>http://www.mkaku.org/article_intertravel.htm</clipSource><pubDate>Fri, 06 Oct 2006 15:00:10 GMT</pubDate></item><item><title>Earth: A Borderline Planet for Life?</title><link>http://clipmarks.com/clipmark/5EF3B4CB-134D-4844-8BDE-CC1E92406448/</link><description>&lt;b&gt;clipped by:&lt;/b&gt; &lt;a href="http://clipmarks.com/clipper/wildcat/"&gt;wildcat&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://physorg.com/news119108915.html" title="http://physorg.com/news119108915.html"&gt;physorg.com&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/wildcat/512/87A2C0BF-F315-43C2-AEDA-A7374C2F3EB7.jpg" alt="A super-Earth like the one in this artists conception can grow twice as large as Earth with up to 10 times the mass. Super-Earths are likely to be more life-friendly than our world because they would be more geologically active. Credit: David A. Agui ..." /&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;  

Our planet is changing before our eyes, and as a result, many species are living on the edge. Yet Earth has been on the edge of habitability from the beginning. New work by astronomers at the Harvard-Smithsonian Center for Astrophysics shows that if Earth had been slightly smaller and less massive, it would not have plate tectonics - the forces that move continents and build mountains. And without plate tectonics, life might never have gained a foothold on our 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;&lt;DIV&gt;Plate tectonics are crucial to a planet's habitability because they enable complex chemistry and recycle substances like carbon dioxide, which acts as a thermostat and keeps Earth balmy. Carbon dioxide that was locked into rocks is released when those rocks melt, returning to the atmosphere from volcanoes and oceanic ridges. 
&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;"There are not only more potentially habitable planets, but MANY more," stated Sasselov, who is director of the Harvard Origins of Life Initiative. 
&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/planet+earth/" rel="tag"&gt;planet earth&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/habitability/" rel="tag"&gt;habitability&lt;/a&gt;&lt;/div&gt;</description><clipSource>http://physorg.com/news119108915.html</clipSource><pubDate>Thu, 10 Jan 2008 10:27:46 GMT</pubDate></item></channel></rss>