Borsu surface
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
- ^ Lidmar-Bergströrm, Karna (1996). "Long term morphotectonic evolution in Sweden". Geomorphology. 16. Elsevier: 33–59.
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Geology of Fennoscandia
- Borsu surface
- Hardangervidda
- Muddus plains
- Paleic surface
- Ostrobothnian Plain
- South Småland peneplain
- 300 m peneplain
- 200 m peneplain
- Strandflat
- Sub-Cambrian peneplain
- Sub-Mesozoic hilly relief
| Moraines |
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| Sedimentary rock |
| Faults and shear zones |
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| Large impact craters | |
| Morphostrucures |
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