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Record #93737:
Ice-shoved hills of Saskatchewan compared with Mississippi Delta mudlumps - implications for glaciotectonic models / James S. Aber.
Title: | Ice-shoved hills of Saskatchewan compared with Mississippi Delta mudlumps - implications for glaciotectonic models / James S. Aber. |
Author(s): | Aber, James S. |
Date: | 1988. |
Publisher: | Rotterdam: A.A. Balkema |
In: | Glaciotectonics; forms and processes. Proceedings of various meetings of the Glaciotectonics Work Group : Field Meeting, Møn, Denmark (1986)/INQUA Congress, Ottawa, Canada (1987)/Field Meeting, Norfolk, UK (1988). (1988.), |
Abstract: | Glaciotectonic models for genesis of Dirt Hills and Cactus Hills of southern Saskatchwan, and other ice-shoved hills, fall into two groups: models in which glacier thrusts permanently frozen strata, and models in which permafrost is not prerequisite. Mudlumps of delta are deforming in style and magnitude similar to ice-shoved ridges, and may be regarded as modern non-glacial analogs to large ice-shoved hills of Pleistocene age. Both situations share several traits: only significant difference is nature of advancing load, i.e. glacier ice or delta sand. |
Notes: | In: Glaciotectonics; forms and processes. Proceedings of various meetings of the Glaciotectonics Work Group : Field Meeting, Møn, Denmark (1986)/INQUA Congress, Ottawa, Canada (1987)/Field Meeting, Norfolk, UK (1988) / David G. Croot, ed. |
Keywords: | 551.333.3 -- Glacial drift, deformation structures in. E7 -- Glaciology: glacial geology and ice ages. E7 -- Glaciology: glacial geology and ice ages. (*41) -- Canada. (*427) -- Saskatchewan. |
SPRI record no.: | 93737 |
LDR 01858naa#a2200000#a#4500 001 SPRI-93737 005 20231209030344.0 007 ta 008 231209s1988####ne#ab##|#####|0||#0#eng#d 035 ## ‡aSPRI-93737 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aAber, James S. 245 10 ‡aIce-shoved hills of Saskatchewan compared with Mississippi Delta mudlumps - implications for glaciotectonic models /‡cJames S. Aber. 260 ## ‡aRotterdam :‡bA.A. Balkema,‡c1988. 300 ## ‡ap. 1-9 :‡bdiags., maps. 500 ## ‡aIn: Glaciotectonics; forms and processes. Proceedings of various meetings of the Glaciotectonics Work Group : Field Meeting, Møn, Denmark (1986)/INQUA Congress, Ottawa, Canada (1987)/Field Meeting, Norfolk, UK (1988) / David G. Croot, ed. 520 3# ‡aGlaciotectonic models for genesis of Dirt Hills and Cactus Hills of southern Saskatchwan, and other ice-shoved hills, fall into two groups: models in which glacier thrusts permanently frozen strata, and models in which permafrost is not prerequisite. Mudlumps of delta are deforming in style and magnitude similar to ice-shoved ridges, and may be regarded as modern non-glacial analogs to large ice-shoved hills of Pleistocene age. Both situations share several traits: only significant difference is nature of advancing load, i.e. glacier ice or delta sand. 650 07 ‡a551.333.3 -- Glacial drift, deformation structures in.‡2udc 650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local 650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local 651 #7 ‡a(*41) -- Canada.‡2udc 651 #7 ‡a(*427) -- Saskatchewan.‡2udc 773 0# ‡7nnam ‡aDavid G. Croot, ed. ‡tGlaciotectonics; forms and processes. Proceedings of various meetings of the Glaciotectonics Work Group : Field Meeting, Møn, Denmark (1986)/INQUA Congress, Ottawa, Canada (1987)/Field Meeting, Norfolk, UK (1988). ‡dRotterdam : A.A. Balkema, 1988. ‡wSPRI-93736 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20231209