<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/d526e2ce-c35d-470f-9d85-462132f51f01/8D2EF9F1-EEF2-4311-B0B4-39711C40CC77/" 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.abdn.ac.uk/~wpg008/asian_erosion2.html" href="http://www.abdn.ac.uk/~wpg008/asian_erosion2.html" style="font-size: 11px;">www.abdn.ac.uk</a></div><blockquote style="text-align: left; padding: 0px 8px; margin: 4px 0px 8px 0px; background: transparent; border: none;" cite="http://www.abdn.ac.uk/~wpg008/asian_erosion2.html"><div align="center"><img src="http://content8.clipmarks.com/blog_cache/www.abdn.ac.uk/img/C6EACFCD-FDB6-4C18-B427-46011266FC9B" alt="Indus Molasse, Ladakh" /></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.abdn.ac.uk/~wpg008/asian_erosion2.html"><FONT size="-1">Aerial view of the Eocene-Oligocene Indus Molasse Group within the Indus Suture Zone, Ladakh, India. This sequence is interpreted as the deposits of a paleo-Indus River and shows that the river started to flow soon after initial collision and uplift of southern Tibet (Clift et al., 2001).</FONT></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.abdn.ac.uk/~wpg008/asian_erosion2.html">If the process of marine sedimentation can be related to the modern mountains and drainage system then there is hope that ancient sediments can be used to reconstruct what the mountains looked like in the geologic past.</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.abdn.ac.uk/~wpg008/asian_erosion2.html">The marine sedimentary record can be used to reconstruct the erosion of the Himalayas and Tibet since the start of India-Asia collision. </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/8D2EF9F1-EEF2-4311-B0B4-39711C40CC77/blog/" title="blog or email this clip"><img src="http://content9.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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