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Geopedology pp 251–264Cite as

Use of Soil Maps and Surveys to Interpret Soil-Landform Assemblages and Soil-Landscape Evolution

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Abstract

Soils form in unconsolidated parent materials, which make them a key link to the geologic system that originally deposited the parent material. In young soils, i.e. those that post-date the last glaciation, parent materials can often be easily identified as to type and depositional system. In a GIS, soil map units can then be geospatially tied to parent materials, enabling the user to create maps of surficial geology. We suggest that maps of this kind have a wide variety of applications in the Earth Sciences, and to that end provide five examples from temperate climate soil-landscapes.

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Correspondence to R. J. Schaetzl .

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Schaetzl, R.J., Miller, B.A. (2016). Use of Soil Maps and Surveys to Interpret Soil-Landform Assemblages and Soil-Landscape Evolution. In: Zinck, J.A., Metternicht, G., Bocco, G., Del Valle, H.F. (eds) Geopedology. Springer, Cham. https://doi.org/10.1007/978-3-319-19159-1_15

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