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Sample text

They are also draped in some locations by recessional push moraines. , 1999b; Evans and Twigg, 2000, 2002). Due to the sparsity of supraglacial and englacial debris over large areas of temperate glacier snouts, hummocky moraine, defined as the product of melt-out of debris-mantled glaciers (Benn and Evans, 1998), is often sparsely developed over deglaciated forelands. g. Dawson, 1979; Levson and Rutter, 1989a, b; Evans and Twigg, 2000, 2002; Fig. 6). However, such features are rarely reported, being difficult to identify among the stronger imprints of other landform-sediment accumulations.

G. g. Bednarski, 1998). 6 Main photograph: Holocene ice-contact delta being proglacially thrust by the advancing margin of Hook Glacier, Makinson Inlet, southwest Ellesmere Island. Inset top photograph: view across thrust blocks of delta showing contorted bedding of fine-grained bottomsets and gravelly foresets. Inset bottom photograph: detail of topset gravels in state of partial entrainment by apron overriding of the thrust-block moraine.

9 The relationship between water pressure cycles on sliding and deformation (stickslip cycles) postulated by Boulton et al. (2001a) based upon data collected from Breiaamerkurjökull. 10 A) Lodged and striated boulder and lee-side fluting on the foreland of Skalafellsjökull, Iceland. B) Explanation of a fluting forming in the lee of a lodged boulder (from Benn, 1994). near the outer limits of the Little Ice Age advance contain complex interbedded sequences of tills and stratified sediments. Often underlying the surface tills are stratified sediments deposited initially in ice-contact fans, braided streams and localized proglacial lakes (Howarth, 1968; Boulton, 1987; Benn and Evans, 1996; Evans, 2000; Evans and Twigg, 2002; Fig.

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