Water, wind, and time

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	Water, wind, and time
amgumen
5-11-2008 8:37 PM
639 views
amgumen says:
This clip is sequential to Alanocu's one http://clipmarks.com/clipmark/C54E068A-A304-475D-9600-3200C5AE1506/
3 Comments |
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5-12-2008 9:45 AM
michellezm
Now that's just plain fascinating. Tks.
5-12-2008 9:46 AM
skwirlinator
Water and wind yes but time did nothing at all
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<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/150fcdeb-8aa0-478e-8ccc-bf1a9dd6e4a9/E15ECB04-2EC9-4A98-AEBC-43156E5B476C/" 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.britannica.com/eb/subject?idxStructId=289113" href="http://www.britannica.com/eb/subject?idxStructId=289113" style="font-size: 11px;">www.britannica.com</a></div><blockquote style="text-align: left; padding: 0px 8px; margin: 4px 0px 8px 0px; background: transparent; border: none;" cite="http://www.britannica.com/eb/subject?idxStructId=289113"><DIV class="featcopy">(from German Insel, “island,” and Berg, “mountain”), isolated hill that stands above well-developed plains and appears not unlike an island rising from the sea. The early German explorers of southern Africa were impressed by such features, and they dubbed the domed or castlelike highlands inselbergs. Spectacular examples include Ayers Rock and the Olga Rocks in central Australia.</DIV></blockquote><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://content9.clipmarks.com/images/clip-icon.gif" 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.britannica.com/eb/art-1254/Three-phase-block-diagram-of-pedimentation-of-an-upland-in" href="http://www.britannica.com/eb/art-1254/Three-phase-block-diagram-of-pedimentation-of-an-upland-in" style="font-size: 11px;">www.britannica.com</a></div><blockquote style="text-align: left; padding: 0px 8px; margin: 4px 0px 8px 0px; background: transparent; border: none;" cite="http://www.britannica.com/eb/art-1254/Three-phase-block-diagram-of-pedimentation-of-an-upland-in"><div align="center"><img src="http://content6.clipmarks.com/blog_cache/www.britannica.com/img/7A1E3200-2830-430D-935F-5B414EA79AED" alt="Art:Figure 3: Three-phase block diagram of pedimentation of an upland in a desert. The process of “scarp” retreat and planation is accomplished by sheet wash on non-vegetated surfaces, but it cannot begin until a local base level of erosion–deposition is established. Streams dissecting the upland cannot cut below the level created where deposition of alluvium begins as runoff dissipates. The long-term locus of that deposition established the datum for lateral stream-bank and valley-wall recessio" /></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.britannica.com/eb/art-1254/Three-phase-block-diagram-of-pedimentation-of-an-upland-in"> Three-phase block diagram of pedimentation of an upland in a desert. The process of “scarp” retreat and planation is accomplished by sheet wash on non-vegetated surfaces, but it cannot begin until a local base level of erosion–deposition is established. Streams dissecting the upland cannot cut below the level created where deposition of alluvium begins as runoff dissipates. The long-term locus of that deposition established the datum for lateral stream-bank and valley-wall recession at higher elevations.</blockquote><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://content7.clipmarks.com/images/clip-icon.gif" 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://flickr.com/photos/rowteight/153178276/sizes/l/" href="http://flickr.com/photos/rowteight/153178276/sizes/l/" style="font-size: 11px;">flickr.com</a></div><blockquote style="text-align: left; padding: 0px 8px; margin: 4px 0px 8px 0px; 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padding: 0px 8px; margin: 4px 0px 8px 0px; background: transparent; border: none;" cite="http://flickr.com/photos/rbcav2003/2295245676/sizes/l/in/set-72157603992066464/"><div align="center"><img src="http://content8.clipmarks.com/blog_cache/flickr.com/img/8E7B729E-BE23-4F74-AE1C-1AF2A0575F57" alt="" /></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/E15ECB04-2EC9-4A98-AEBC-43156E5B476C/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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