Jump to content

Sub-Cambrian peneplain

From Wikipedia, the free encyclopedia

This is an old revision of this page, as edited by Lappspira (talk | contribs) at 22:11, 14 November 2016. The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

Extraordinary flat surfaces of the Sub-Cambrian peneplain around the shores of lake Vänern near Kinnekulle.

The sub-Cambrian peneplain is a geomorphic unit covering large swathes of Fennoscandia. It consists in a series of discontiguous low relief zones that are at some locations covered by a sedimentary rock cover dating to the Cambrian. Close to the cover rocks the exposed parts of the peneplain are extraordinarily flat.[1] The peneplain continues as an unconformity beneath the East European Platform.[2] In Norway the peneplain is apparently disrupted by vertical displacement along faults, following an NNE-SSW orientation.[3] Along the southern and central coast of Norrland in Sweden the peneplain is estimated to have been uplifted about 650 meters giving origin to a series of water gaps including those of Ångermanälven, Indalsälven and Ljusnan.[4]

The island Blå Jungfrun in the Baltic Sea is an ancient inselberg rising from the Sub-Cambrian peneplain. Being a inselberg formed in Precambrian time it was buried in sandstone after its formation and remained buried until erosion freed it in geologicaly recent times.[5]

See also

References

  1. ^ Lidmar-Bergström, Karna; Bonow, Johan M.; Japsen, Peter (2013). "Stratigraphic Landscape Analysis and geomorphological paradigms: Scandinavia as an example of Phanerozoic uplift and subsidence". Global and Planetary Change. 100: 153–171. {{cite journal}}: |access-date= requires |url= (help)
  2. ^ Det subkambriske peneplanet i Baltika
  3. ^ Jarsve, Erlend M.; Krøgli, Svein Olav; Etzelmüller, Bernd; Gabrielsen, Roy H. (2014). "Automatic identification of topographic surfaces related to the sub-Cambrian peneplain (SCP) in southern Norway—Surface generation algorithms and implications". Geomorphology. 211. Elsevier: 89–99. {{cite journal}}: |access-date= requires |url= (help)
  4. ^ Lidmar-Bergström, Karna; Olvmo, Mats (2015). Plains, steps, hilly relief and valleys in northern Sweden – review, interpretations and implications for conclusions on Phanerozoic tectonics (PDF) (Report). Geological Survey of Sweden. Retrieved June 29, 2016.
  5. ^ Lidmar-Bergström, Karna. "Inselberg". Nationalencyklopedin (in Swedish). Cydonia Development. Retrieved June 22, 2015.