<div style="margin: 12px 0px; font-family: arial; color: #333333; background: #ffffff; border: solid 4px #e5e5e5; width: 100%; clear: left;"><div class="CM_CTB_Content_Wrap" style="margin: 0px; padding: 0px;background-color: #ffffff;"><div style="border-bottom: solid 1px #dcdcdc; white-space: nowrap; margin-bottom: 8px; background-color: #eeeeee ;background-image: url(http://clipmarks.com/images/source-bg.gif); background-repeat: repeat-x; height: 24px; line-height: 24px; vertical-align: middle; padding-bottom: 4px; color: #666666; font-size: 10px;" ><a href="http://clipmarks.com/clip-to-blog/" title="see clips that are hot right now"><img src="http://content.clipmarks.com/blog_embed/af7a4465-f472-42d8-b144-c0bea62052d6/05D7C15A-B59F-4CAE-8920-48FD192F1CAD/" alt="" width="19" height="19" border="0" style="vertical-align: middle; margin: 0px 4px; display: inline; border: none; float:none;" /></a>clipped from <a title="http://www.fys.uio.no/pgp/index.php?option=com_content&task=view&id=321&Itemid=230&limit=1&limitstart=1" href="http://www.fys.uio.no/pgp/index.php?option=com_content&task=view&id=321&Itemid=230&limit=1&limitstart=1" style="font-size: 11px;">www.fys.uio.no</a></div><blockquote style="text-align: left; padding: 0px 8px; margin: 4px 0px 8px 0px; background: transparent; border: none;" cite="http://www.fys.uio.no/pgp/index.php?option=com_content&task=view&id=321&Itemid=230&limit=1&limitstart=1"><div align="center"><img src="http://content6.clipmarks.com/blog_cache/www.fys.uio.no/img/BBD38E38-CEF3-45B7-902B-6409BF3144AA" alt="Image" /></div></blockquote><div style="height: 2px; font-size: 2px; background: #dcdcdc; border-bottom: solid 1px #f5f5f5; margin: 2px 4px;"></div><blockquote style="text-align: left; padding: 0px 8px; margin: 4px 0px 8px 0px; background: transparent; border: none;" cite="http://www.fys.uio.no/pgp/index.php?option=com_content&task=view&id=321&Itemid=230&limit=1&limitstart=1"><DIV align="left" class="mosimage_caption">Methane gas eruption. Photo: S. Planke</DIV></blockquote><div style="height: 2px; font-size: 2px; background: #dcdcdc; border-bottom: solid 1px #f5f5f5; margin: 2px 4px;"></div><blockquote style="text-align: left; padding: 0px 8px; margin: 4px 0px 8px 0px; background: transparent; border: none;" cite="http://www.fys.uio.no/pgp/index.php?option=com_content&task=view&id=321&Itemid=230&limit=1&limitstart=1"><P> Natural mud volcanoes are found in many sedimentary basins world-wide. The most spectacular mud volcanoes are present in Azerbaijan. But they are also present on-shore in places like Pakistan, Trinidad and Indonesia. Offshore mud volcanoes are likely even more numerous, and are common in places like the Mediterranean, the Black Sea and the Barents Sea. </P></blockquote><div style="height: 2px; font-size: 2px; background: #dcdcdc; border-bottom: solid 1px #f5f5f5; margin: 2px 4px;"></div><blockquote style="text-align: left; padding: 0px 8px; margin: 4px 0px 8px 0px; background: transparent; border: none;" cite="http://www.fys.uio.no/pgp/index.php?option=com_content&task=view&id=321&Itemid=230&limit=1&limitstart=1"><div align="center"><img src="http://content8.clipmarks.com/blog_cache/www.fys.uio.no/img/B6A1A46A-04B0-40A4-9131-241382B2D833" alt="Image" /></div></blockquote><div style="height: 2px; font-size: 2px; background: #dcdcdc; border-bottom: solid 1px #f5f5f5; margin: 2px 4px;"></div><blockquote style="text-align: left; padding: 0px 8px; margin: 4px 0px 8px 0px; background: transparent; border: none;" cite="http://www.fys.uio.no/pgp/index.php?option=com_content&task=view&id=321&Itemid=230&limit=1&limitstart=1"><div align="center"><img src="http://content9.clipmarks.com/blog_cache/www.fys.uio.no/img/D0944421-E464-4A43-A025-EE91B3941F57" alt="Image" /></div></blockquote><div style="height: 2px; font-size: 2px; background: #dcdcdc; border-bottom: solid 1px #f5f5f5; margin: 2px 4px;"></div><blockquote style="text-align: left; padding: 0px 8px; margin: 4px 0px 8px 0px; background: transparent; border: none;" cite="http://www.fys.uio.no/pgp/index.php?option=com_content&task=view&id=321&Itemid=230&limit=1&limitstart=1"><DIV align="left" class="mosimage_caption">Burning methane seep. Lokbatan. Photo: S. Planke</DIV></blockquote><div style="height: 2px; font-size: 2px; background: #dcdcdc; border-bottom: solid 1px #f5f5f5; margin: 2px 4px;"></div><blockquote style="text-align: left; padding: 0px 8px; margin: 4px 0px 8px 0px; background: transparent; border: none;" cite="http://www.fys.uio.no/pgp/index.php?option=com_content&task=view&id=321&Itemid=230&limit=1&limitstart=1"><STRONG>1. Active mud volcanoes in Azerbaijan </STRONG></blockquote><div style="height: 2px; font-size: 2px; background: #dcdcdc; border-bottom: solid 1px #f5f5f5; margin: 2px 4px;"></div><blockquote style="text-align: left; padding: 0px 8px; margin: 4px 0px 8px 0px; background: transparent; border: none;" cite="http://www.fys.uio.no/pgp/index.php?option=com_content&task=view&id=321&Itemid=230&limit=1&limitstart=1"><STRONG>2. Active mud volcanoes in the Barents Sea</STRONG></blockquote><div style="height: 2px; font-size: 2px; background: #dcdcdc; border-bottom: solid 1px #f5f5f5; margin: 2px 4px;"></div><blockquote style="text-align: left; padding: 0px 8px; margin: 4px 0px 8px 0px; background: transparent; border: none;" cite="http://www.fys.uio.no/pgp/index.php?option=com_content&task=view&id=321&Itemid=230&limit=1&limitstart=1"><STRONG>3. Fossil mud volcanoes in the Norwegian Sea and S. Africa</STRONG></blockquote><div style="height: 2px; font-size: 2px; background: #dcdcdc; border-bottom: solid 1px #f5f5f5; margin: 2px 4px;"></div><blockquote style="text-align: left; padding: 0px 8px; margin: 4px 0px 8px 0px; background: transparent; border: none;" cite="http://www.fys.uio.no/pgp/index.php?option=com_content&task=view&id=321&Itemid=230&limit=1&limitstart=1"><div align="center"><img src="http://content6.clipmarks.com/blog_cache/www.fys.uio.no/img/8ABF48D2-EE7C-482D-89EE-136455B1473A" alt="Image" /></div></blockquote><div style="height: 2px; font-size: 2px; background: #dcdcdc; border-bottom: solid 1px #f5f5f5; margin: 2px 4px;"></div><blockquote style="text-align: left; padding: 0px 8px; margin: 4px 0px 8px 0px; background: transparent; border: none;" cite="http://www.fys.uio.no/pgp/index.php?option=com_content&task=view&id=321&Itemid=230&limit=1&limitstart=1"><DIV align="left" class="mosimage_caption">Mud flow, Azerbaijan. Photo: S. Planke</DIV></blockquote></div><div style="margin: 0px 6px 6px 4px;"><table style="font-size: 11px;border-spacing: 0px;padding: 0px;" cellpadding="0" cellspacing="0" width="100%"><tr><td style="background:transparent;border-width:0px;padding:0px;">&nbsp;</td><td align="right" style="background:transparent;border-width:0px;padding:0px;width:107px" width="107"><a href="http://clipmarks.com/share/05D7C15A-B59F-4CAE-8920-48FD192F1CAD/blog/" title="blog or email this clip"><img src="http://content7.clipmarks.com/images/c2b-foot.png" border="0" alt="blog it" width="107" height="17" style="border-width:0px;padding:0px;margin:0px;" /></a></td></tr></table></div></div>

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