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Record #119378:
The formation of glacial flutes: assessment of models with evidence from Lyngsdalen, north Norway / John E. Gordon, W. Brian Whalley, Anne F. Gellatly, Diana M. Vere.
Title: | The formation of glacial flutes: assessment of models with evidence from Lyngsdalen, north Norway / John E. Gordon, W. Brian Whalley, Anne F. Gellatly, Diana M. Vere. |
Author(s): | Gordon, John E. Whalley, W. Brian. Gellatly, Anne F. Vere, Diana M. |
Date: | 1992. |
In: | Quaternary Science Reviews. (1992.), Vol. 11(7-8) (1992) |
Abstract: | In this region, flutes are associated with glaciers with cold-based margins. Three sets of variables were investigated: flutes themselves, and their shapes, dimensions and field relationships; physical properties of materials comprising them; and glacier properties, particularly basic thermal regime and ice--debris relationships at glacier margin. Proposes model in which flutes are primary features formed by deformation of basal ice around subglacial boulders or other obstacles. |
Notes: | Quaternary Science Reviews. Vol. 11(7-8) :709-731 (1992). |
Keywords: | 551.33 -- Glacial geology. 551.332.53 -- Moraines, ground and glacial flutes. 519.673 -- Modelling. .000(410) -- British author. E7 -- Glaciology: glacial geology and ice ages. (*58) -- Norway. (*584) -- Troms. |
SPRI record no.: | 119378 |
LDR 01547naa#a2200000#a#4500 001 SPRI-119378 005 20240419032619.0 007 ta 008 240419s1992####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-119378 040 ## ‡aUkCU-P‡beng‡eaacr 245 04 ‡aThe formation of glacial flutes :‡bassessment of models with evidence from Lyngsdalen, north Norway /‡cJohn E. Gordon, W. Brian Whalley, Anne F. Gellatly, Diana M. Vere. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1992. 300 ## ‡ap. 709-731 :‡bill., diags., maps. 500 ## ‡aQuaternary Science Reviews. Vol. 11(7-8) :709-731 (1992). 520 3# ‡aIn this region, flutes are associated with glaciers with cold-based margins. Three sets of variables were investigated: flutes themselves, and their shapes, dimensions and field relationships; physical properties of materials comprising them; and glacier properties, particularly basic thermal regime and ice--debris relationships at glacier margin. Proposes model in which flutes are primary features formed by deformation of basal ice around subglacial boulders or other obstacles. 650 07 ‡a551.33 -- Glacial geology.‡2udc 650 07 ‡a551.332.53 -- Moraines, ground and glacial flutes.‡2udc 650 07 ‡a519.673 -- Modelling.‡2udc 650 07 ‡a.000(410) -- British author.‡2udc 650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local 651 #7 ‡a(*58) -- Norway.‡2udc 651 #7 ‡a(*584) -- Troms.‡2udc 700 1# ‡aGordon, John E. 700 1# ‡aWhalley, W. Brian. 700 1# ‡aGellatly, Anne F. 700 1# ‡aVere, Diana M. 773 0# ‡7nnas ‡tQuaternary Science Reviews. ‡gVol. 11(7-8) (1992) ‡wSPRI-78722 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240419