Titlebook: Glaciotectonic Landforms and Structures; James S. Aber,David G. Croot,Mark M. Fenton Book 1989 Springer Science+Business Media Dordrecht 1

insipid

Diapirs, Intrusions and Wedges,e from only a few cm to > 100 m (fig. 1-4) and may have vertical dimensions of several lOs of m. Intrusive structures rarely give rise to distinctive or noticeable landforms, but they may dominate the subsurface character of a glacial sequence (fig. 7-1).

Archipelago

Dynamism of Glaciotectonic Deformation,under the center of a thick ice sheet. Deformations may arise during advancing, maximal, or recessional phases of glaciation. All manner of material from well-consolidated bedrock to loose Quaternary sediment in both frozen and thawed conditions may be affected.

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978-94-015-6843-2Springer Science+Business Media Dordrecht 1989

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https://doi.org/10.1007/978-981-15-8143-4idges as, ‘a(chǎn) composite of great slices of up-thrust and commonly contorted sedimentary bedrock that is generally interlayered with and overlain by much glacial drift.’ The term . (= transverse-ridges of Clayton .. 1980) is used here for such ice-shoved ridges. Composite-ridges that include a substan

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