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43:— have higher potential to be preserved than small and irregular surfaces and are thus the most studied kind of paleosurfaces. Irregular paleosurfaces, albeit usually smaller than flat ones, occur across the globe, one example being the
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is valued by geologists allowing for a broader range of surface types to be considered. However, when paleosurfaces are viewed by geomorphologists the
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or deconstructive processes are considered. This is because geomorphologists are primarily concerned with erosional and
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Widdowson, M. (1997). "The geomorphological and geological importance of palaeosurfaces". In
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Traditionally geologist and geomorphologist view paleosurfaces differently. Geologists look into the
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it is argued that they become paleosurfaces once they are detached from the
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in that they represent geological and geomorphological events.
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