Abstract
Morphometry consists of the measurement of form either from maps or in the field. It provides quantitative data that can then be analyzed to establish significant aspects of the morpology of the features investigated. As geomorphology is concerned with the understanding of the shape of features, morphometry provides essential material on which to base a valid analysis. From morphometric measurements it is possible to obtain the mean dimensions of specific features and to obtain a quantitative range within which they exist. The features in one area can be compared and contrasted with those in another area, providing often valuable clues as the the cause of differences in dimensions. In this contribution some examples of morphometric analysis on glacial geomorphology will be examined to illustrate the value of this method of study.
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© 1982 Donald R. Coates
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King, C.A.M. (1982). Morphometry in Glacial Geomorphology. In: Coates, D.R. (eds) Glacial Geomorphology. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-6491-7_5
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DOI: https://doi.org/10.1007/978-94-011-6491-7_5
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