Glac Geom

Acknowledgements, Chronological Table of reprinted articles and chapters, General Editor' s preface, lntroduction, 1 The channeled scablands of the Columbia Plateau, 2 Marginal drainage channels as indicators of the gradients of Quatemary ice caps, 3 Temperature observations in bergschrunds and their relationship to cirque erosion, 4 On the mechanism by which stones in till become oriented, 5 Ice-disintegration features in western Canada, 6 Ice melting under a thin layer of moraine, and the existence of ice cores in moraine ridges, 7 Mechanism for the formation of inner moraines found near the edge of cold ice caps and ice sheets, 8 The formation and shape of drumlins and their distribution and orientation in drumlin fields, 9 Moraines, sandar, kames and eskers near Breidamerkurj¶kull, lceland, 10 Bimodal distribution of rock and mineral fragments in basal tills, 11 The active push moraine of the Thompson Glacier: Axel Deiberg Island, Canadian Arctic Archipelago, 12 Modern Arctic glaciers as depositional models for former ice sheets, 13 Landscapes of glacial erosion in Greenland and their relationship to ice, topographic and bedrock conditions, 14 Nature of esker Sedimentation, 15 Proglacial ?uvial and lacustrine environments, 16 A framework for the investigation of medial moraine formation: Austerdalsbreen, Norway, and Bereudon Glacier, British Columbia, Canada, 17 A theoretical model of glacial abrasion, 18 A model for sedimentation by tidewater glaciers, 19 Sediment deformation beneath glaciers: rheology and geological consequences, 20 Till beneath ice stream B: 3. Till deformation: evidence and implications, 21 Drumlin fields, dispersal trains, and ice streams in Arctic Canada, 22 Structure and stability of the former subglacial drainage system of the Glacier de Tsanfteuron, Switzerland, 23 Constraints on the preservation of diamict facies (melt-out tills) at the margins of stagnant glaciers, 24 Potential effects of subglacial water-pressure fluctuations on quarrying, 25 A ploughing model for the origin of weak tills beneath ice streams: a qualitative treatment