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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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Plummer, Charles, David McGeary, and Diane Carlson. Physical Geology. 10th ed. Boston: McGraw-Hill, 2004.
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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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③ 1码＝3英尺＝0.914米。——译注
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④ load of stream和stream load除译作河流的含沙量之外，后者也常作为河流中泥沙砾石的统称。——译注
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⑤ 在中、英文冰川地貌学中有些名词使用较为混乱。据美国地质学词典的解释，新、老冰川区由冰川和冰缘水流形成的堆积物统称为冰川堆积物（glacial deposit 或 drift）；在冰川区内由冰川旁或下部直接形成的无分选、不分层、大小混杂的堆积物专称为冰碛（物）（till或moraine，其中moraine又兼指由它构成的冰碛丘岗地貌; till 有时又指主要由砾石和黏土组成的泥砾［boulder clay］）。在冰川外缘的水流堆积下形成有相当分选和成层的堆积物，专称为“冰水堆积物”（fluvial glacial deposit）。——译注
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