From Wikipedia, the free encyclopedia
The Borsu surface (Swedish: Borsuytan) is an erosion surface found as valley benches in the northern Scandinavian Mountains. The surface was first identified by Walter Wråk who published his findings in Ymer in 1908.[1]
References
[edit]- ^ Lidmar-Bergströrm, Karna (1996). "Long term morphotectonic evolution in Sweden". Geomorphology. 16. Elsevier: 33–59.
Paleosurfaces | |||||||
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Sedimentary cover |
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Structures |
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Lesser igneous provinces | |||||||
Provinces and orogens |
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