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Climatic geomorphology
Climatic geomorphology is the study of the role of climate in shaping landforms and the earth-surface processes.[1] An approach used in climatic geomorphology is to study relict landforms to infer ancient climates.[1] Being often concerned about past climates climatic geomorphology considered sometimes to be an aspect of historical geology.[2] Since landscape features in one region might have evolved under climates different from those of the present, studying climatically disparate regions might help understand present-day landscapes. For example, Julius Büdel studied both cold-climate processes in Svalbard and weathering processes in tropical India to understand the origin of the relief of Central Europe, which he argued was a palimpsest of landforms formed at different times and under different climates.[3]
- ^ a b Gutiérrez, Mateo; Gutiérrez, Francisco (2013). "Climatic Geomorphology". Treatise on Geomorphology. Vol. 13. pp. 115–131.
- ^ Gutiérrez, Mateo, ed. (2005). "Chapter 1 Climatic geomorphology". Developments in Earth Surface Processes. Vol. 8. pp. 3–32. doi:10.1016/S0928-2025(05)80051-3. ISBN 978-0-444-51794-4.
- ^ Migoń, Piotr (2006). "Büdel, J. 1982: Climatic geomorphology. Princeton: Princeton University Press. (Translation of Klima-geomorphologie, Berlin-Stuttgart: Gebrüder Borntraeger, 1977.)". Progress in Physical Geography. 30 (1): 99–103. doi:10.1191/0309133306pp473xx. S2CID 129512489.
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