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pile-up had been pushed bodi-
          ly fifty, sixty and even seventy
          kilometres over its neighbour.
          Erosion subsequently exposed
          the different layers. The top of
          the Matterhorn is a fragment of
          Africa!

          But why did the African conti-
          nent move? North America
          and Greenland had begun
          to drift away from Northern
          Europe creating the embryo-
          nic Atlantic Ocean. Millions
          of years later, the great land
          mass lying in the southern
          hemisphere -- Gondwanaland
          -- began to break up. South
          America, Australia, Antarctica
          and India began to split away
          from Africa. India ultimately
          crashed into the bottom of Asia
          to form the Himalayas. Thus re-
          leased from this burden, Africa
          began to drift inexorably nor-
          thward, narrowing the former
          ocean and crushing everything
          that lay in its path. As this plate
          pushed northward with irre-
          sistible force, the shape of the
          landscape changed many times.      Finally, about  25  million years   see today, peaks must have rea-
          The ocean became a shallow sea,    ago, there was no where to go but   ched 10,000 even 12,000 metres—
          islands appeared, the sea was cut off,   upward and the young Alps began   erosion has carried most of it away.
          dried out leaving salt beds, was re-  to emerge. The powerful process
          placed by fresh-water lakes, but the   continued unabated until an ex-  It should not be imagined that the
          sea broke through again—this cycle   traordinarily high mountain range   collision of continents took place
          repeated itself over and over again.   was formed. On the basis of what we   any faster than it is happening to-
                                                                                           day—a few millimetres
                                                                                           per year. But we do
                                                                                           know that at one stage
                                                                                           the uplift was extre-
                                                                                            mely intense—layers of
                                                                                            rock tipped up at such
                                                                                           steep angles that they
                                                                                           collapsed into multiple
                                                                                           folds under the effect of
                                                                                           gravity and deep beds
                                                                                           of broken rock, gravel,
                                                                                           sand and mud washed
                                                                                           down by torrents from
                                                                                           vast heights. Under
                                                                                            Lausanne there are  4.5
                                                                                           kilometres of sediment.
                                                                                           In short, the geology of
                                                                                           the Alps is total chaos.
                                                                                           The granite core of
                                                                                           Mont Blanc that may
                                                                                           have once lain twenty-
                                                                                           five kilometres under-
                                                                                           ground lies exposed
                                                                                            nearly five kilometres
                                                                                           above sea level.


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