Jump to content

Borsu surface

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]
  1. ^ Lidmar-Bergströrm, Karna (1996). "Long term morphotectonic evolution in Sweden". Geomorphology. 16. Elsevier: 33–59.