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CHAPTER 6 • From Greenhouse to Icehouse: The Last 50 Million Years  109


        amounts of plateau construction may have occurred      Prediction 2: Unusual Physical Weathering The
        on Africa near 100 Myr ago as the giant continent of  second test of the uplift weathering hypothesis is
        Pangaea broke up. As a result, it is hard to argue that  whether or not today’s high topography is causing
        the present plateau exceeds features that may have  higher rates of physical weathering and rock fragmenta-
        existed during earlier intervals.                   tion than occurred in the past. The concentrations of
                                                            suspended particles carried southward and eastward
                                                            from the Himalaya and Tibet by Asian rivers are larger
          IN SUMMARY, the existence of the massive Tibetan
          Plateau makes modern topography unusual,          than any on Earth (Figure 6-15). The youthful topogra-
          consistent with the uplift weathering hypothesis.  phy of the eastern Andes drained by the Amazon River is
          Regions of high youthful terrain also exist along  another region of high particle concentrations. These
          subducting plate margins and elsewhere, but they  measurements clearly indicate intense physical weather-
          may be similar to features that existed in the past.  ing at the present time in the two regions with highest
                                                            terrain.







                                           BOX 6-1 CLIMATE DEBATE

                                                    CONTINUED









                                                    Rockies








                                                                                  High plains
                                  Basin and range

                         Sierra
                                                                 Rockies
                                                 Colorado
                                                 Plateau












         Topography in the American West A broad bulge of high topography reaches from the Sierra in
         the far western United States to the Rocky Mountains and High Plains farther east, with the
         Colorado Plateau and Basin and Range lying in between. Low-elevation regions a few hundred
         meters above sea level are shown in green, with progressively higher elevations in yellow, brown,
         pale orange, and white. (Courtesy of Peter Schloss, National Geophysical Data Center, Boulder, CO.)
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