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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

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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.
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651 #7 ‡a(*41) -- Canada.‡2udc
651 #7 ‡a(*427) -- Saskatchewan.‡2udc
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