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你所居住地区的地貌特征是由哪些作用形成的？
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延伸阅读
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Ahnert, Frank. Introduction to Geomorphology. London: EdwardArnold, 1998.
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Benn, DouglasI. Glaciers and Glaciation. London: Edward Arnold, 1998.
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Bland, Will J., and David Rolls. Weathering: An Introduction to Basic Principles. London: Edward Arnold, 1998.
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Briggs, David, et al. , eds. Fundamentals of the Physical Environment. 2d ed. NewYork: Routledge, 1997.
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Chorley, Richard J. Water, Earth, and Man. London: Methuen, 1969.
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Easterbrook, Don J. Surface Processes and Landforms. 2d ed. Upper Saddle River, N. J.: Prentice Hall, 1998.
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Evans, David J. A., and Hugh M. French, eds. Periglacial Geomorphology. NewYork: Routledge, 2004.
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Goudie, Andrew. The Changing Earth: Rates of Geom-orphological Processes. Oxford, England: Blackwell, 1995.
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Haslett, Simon. Coastal Systems. NewYork: Routledge, 2001.
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Huggett, Richard J. Fundamentals of Geomorphology. NewYork: Routledge, 2002.
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Knighton, David. Fluvial Forms and Processes. Rev. ed. London; Arnold, 1998.
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Kump, Lee, James Kasting, and Robert Crane. The Earth System. 2d ed. Upper Saddle River, N. J. : Prentice Hall, 2003.
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Livingstone, Ian, and Andrew Warren. Aeolian Geomorphology: An Introduction. Upper Saddle River, N. J. : Prentice Hall, 1996.
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Montgomery, Carla W. Environmental Geology. 6th ed. Boston: McGraw-Hill, 2003.
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Ollier, Cliff, and Colin Pain. The Origin of Mountains. NewYork: Routledge, 2000.
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Plummer, Charles, David McGeary, and Diane Carlson. Physical Geology. 10th ed. Boston: McGraw-Hill, 2004.
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Progressin Physical Geography. London: Edward Arnold. Various issues.
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Spencer, Edgar W. Earth Science. Boston: McGraw-Hill, 2003.
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Strahler, Alan, and Arthur Strahler. Physical Geography: Science and Systems of the Human Environment. 2d ed. NewYork: John Wiley & Sons, 2001.
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Trenhaile, Alan S. Coastal Dynamics and Landforms. Oxford: Oxford University Press, 1997.
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@万维网上和地理学有关的网站极其丰富。与本章主题有关的网站请见与本书有关的在线学习中心的“Web Links”部分。网址：www.mhhe.com/getis11e.
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① landscape在地理学中有两层意思：一是广义的景观，一是地貌学方面比较狭义的地景。—译注
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② 里氏震级之间是对数关系，整个数量级中的每一个增量意味着增大10倍。所以，一个4级地震的影响要为一个3级地震的10倍。地震对于人类的实际影响不仅随着地震的强烈程度而变化，而且还随着一些次生影响而变化，例如海啸、滑坡，地震影响区的人口密度和建筑物质量等。矩震级为地震的大小提供了最可靠的估算。
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