<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/f62060b7-7bdd-4895-9d7e-b8e1d2240b93/652CB940-E380-46CA-A2CF-C89D15107340/" 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://geology.com/nasa/greenland-glaciers/" href="http://geology.com/nasa/greenland-glaciers/" style="font-size: 11px;">geology.com</a></div><blockquote style="text-align: left; padding: 0px 8px; margin: 4px 0px 8px 0px; background: transparent; border: none;" cite="http://geology.com/nasa/greenland-glaciers/"><div align="center"><img src="http://content6.clipmarks.com/blog_cache/geology.com/img/26CB984C-0B95-4999-9A20-820FD0A0944C" alt="Greenland Glaciers" /></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://geology.com/nasa/greenland-glaciers/"><table background="undefined" bgcolor=""><tr><TD>This satellite image shows several small glaciers spilling into a mostly dry valley in western Greenland. The image was captured on August 29, 2009. The Advanced Land Imager on NASA’s Earth Observing-1 satellite acquired this natural-color image. This image shows most of the valley and the image below is a close-up of two glacier snouts. Image credit NASA / Earth Observatory.</TD></tr></table></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://geology.com/nasa/greenland-glaciers/"><div align="center"><img src="http://content7.clipmarks.com/blog_cache/geology.com/img/4F5C436F-D723-4C67-BCDA-2554289A7BD7" alt="Greenland Glaciers" /></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://geology.com/nasa/greenland-glaciers/"><table background="undefined" bgcolor=""><tr><TD>This close-up image allows a clear view of both snouts’ rough surfaces. While ice at the bottom of a glacier generally flows smoothly, the ice overhead is often brittle. As a result, the glacier’s movement causes ruptures on the ice surface, which can be exacerbated by surface melting. <SPAN class="jargon">Foehn winds</SPAN>—warm, dry, down-slope winds—may contribute to glacier melt, and also keep the underlying valley mostly dry. The shallow, blue-green water in the valley bottom is likely laced with rock flour left over from earlier glacial grinding of Greenland’s rocks. Image credit NASA / Earth Observatory.</TD></tr></table></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/652CB940-E380-46CA-A2CF-C89D15107340/blog/" title="blog or email this clip"><img src="http://content8.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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