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Record #152225:
Assessment of requirements for cirque formation in northern Sweden / Peter Jansson, Cecilia Richardson, Stig Jonsson.
Title: | Assessment of requirements for cirque formation in northern Sweden / Peter Jansson, Cecilia Richardson, Stig Jonsson. |
Author(s): | Jansson, Peter. Richardson, Cecilia. Jonsson, Stig. |
Date: | 1999. |
In: | Annals of Glaciology. (1999.), Vol. 28 (1999) |
Abstract: | Studies climatic conditions for formation of cirque glaciers in Rassepautasjitjåkka massif in northern Sweden. Glacier has to be wet-based to lead to erosion of cirque, requiring warmer winters with increased precipitation, equivalent to more maritime influence in area than current climatic situation. Substantial glaciation in Scandinavia occurred at 12.6 Myr, so many cirque forms may have occurred much earlier than Quaternary. |
Notes: | Annals of Glaciology. Vol. 28 :16-22 (1999). Papers from the International Symposium on Glaciers and the Glaciated Landscape, 17--20 August 1998, Kiruna, Sweden, J. Kleman (Editor) |
Keywords: | 551.33 -- Glacial geology. 551.336 -- Ice ages. 551.32 -- Glaciology. 551.324 -- Land ice. 551.324.22 -- Glaciers. 551.331.52 -- Glaciated valleys. 551.77 -- Cenozoic. 551.79 -- Quaternary. 551.583 -- Climatic changes. E7 -- Glaciology: glacial geology and ice ages. (*57) -- Sweden. |
SPRI record no.: | 152225 |
LDR 01660naa#a2200000#a#4500 001 SPRI-152225 005 20240328104930.0 007 ta 008 240328s1999####xx#a##|##|###|0||#0|eng#d 035 ## ‡aSPRI-152225 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aJansson, Peter. 245 10 ‡aAssessment of requirements for cirque formation in northern Sweden /‡cPeter Jansson, Cecilia Richardson, Stig Jonsson. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1999. 300 ## ‡ap. 16-22 :‡bill., diags. 500 ## ‡aAnnals of Glaciology. Vol. 28 :16-22 (1999). 500 ## ‡aPapers from the International Symposium on Glaciers and the Glaciated Landscape, 17--20 August 1998, Kiruna, Sweden, J. Kleman (Editor) 520 3# ‡aStudies climatic conditions for formation of cirque glaciers in Rassepautasjitjåkka massif in northern Sweden. Glacier has to be wet-based to lead to erosion of cirque, requiring warmer winters with increased precipitation, equivalent to more maritime influence in area than current climatic situation. Substantial glaciation in Scandinavia occurred at 12.6 Myr, so many cirque forms may have occurred much earlier than Quaternary. 650 07 ‡a551.33 -- Glacial geology.‡2udc 650 07 ‡a551.336 -- Ice ages.‡2udc 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.324 -- Land ice.‡2udc 650 07 ‡a551.324.22 -- Glaciers.‡2udc 650 07 ‡a551.331.52 -- Glaciated valleys.‡2udc 650 07 ‡a551.77 -- Cenozoic.‡2udc 650 07 ‡a551.79 -- Quaternary.‡2udc 650 07 ‡a551.583 -- Climatic changes.‡2udc 650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local 651 #7 ‡a(*57) -- Sweden.‡2udc 700 1# ‡aRichardson, Cecilia. 700 1# ‡aJonsson, Stig. 773 0# ‡7nnas ‡tAnnals of Glaciology. ‡gVol. 28 (1999) ‡wSPRI-60773 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240328