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48    INTRODUCING LANDFORMS AND LANDSCAPES


              the humid tropics. Third, Ollier questions the accepted  FURTHER READING
              chronology of mountain building, which sees Tibet, the
              highlands of western North America, and the Andes  Berner, E. K. and Berner, R. A. (1987) The Global Water
              beginning to rise about 40 million years ago, favouring  Cycle: Geochemistry and Environment. Englewood Cliffs,
              instead rise over the last few million years.  N.J.: Prentice Hall.
                                                        Old but still worth reading.

              SUMMARY                                   Berner, R. A. and Berner, E. K. (1995) Global Environ-
                                                        ment: Water and Geochemical Cycles. Upper Saddle River,
                                                        N.J.: Prentice Hall.
              Three grand cycles of matter affect Earth surface  A later incarnation of the previous book.
              processes – the water cycle (evaporation, condensation,
              precipitation, and runoff), the rock cycle (uplift, weath-  Ruddiman, W. F. (ed.) (1997) Tectonic Uplift and
              ering, erosion, deposition, and lithification), and the  Climatic Change. New York: Plenum Press.
              biogeochemical cycles. Denudation encompasses weath-  A detailed account of the connections between tectonics,
              ering and erosion. Erosive agents – ice, water, and wind –  weathering, and climate.
              pick up weathered debris, transport it, and deposit it.  Westbroek, P. (1991) Life as a Geological Force: Dynam-
              Climate partly determines denudation (weathering and  ics of the Earth. New York: W. W. Norton.
              erosion). In addition, geological and topographic fac-  A leisurely and winning introduction to geological and
              tors affect mechanical denudation. Climate, rock type,  biogeochemical cycles from the perspective of Earth
              topographic factors, and organisms influence chemical  history.
              denudation. Climate, topography, and plate tectonic
              process interact in complex ways. Uplift changes cli-
              mates, climatic changes may increase erosion, erosion
              mayaffecttheflowofcrustalrocksandsoinfluenceuplift.
              Erosion of mountains may affect the carbon dioxide
              balance of the atmosphere and promote climatic change.


              ESSAY QUESTIONS

              1  To what extent are the Earth’s grand
                 ‘cycles’ interconnected?
              2  How important are substrates in
                 explaining land form?
              3  Assess the relative importance of the
                 factors that influence denudation
                 rates.
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