The characteristics of glacial till reflect the erosional, transportational and depositional history of the constituent sediment. Glacial till is a heterogeneous mixture of rock fragments ranging in size from clay to boulders and is deposited directly from glacial ice without water transport. (Strahler A. H. & Strahler A. N. 1976). Ice sheets deposited in the Pleistocene period may be more than 30 m deep and inevitably the constituents of glacial till will reflect the retreats, advances and stationary phases of the ice which have taken place during the history of a glacier since its formation.I shall outline the various forms of glacial till, giving consideration to the type of prevailing climatic conditions which give rise to their formation and deposition to illustrate how the constituent sediment does provide evidence for glacial activity over time.As glaciers are so effective at erosion and transport, large quantities of debris is also associated with them. According to its location with respect to the glacier, such debris transported as ice mass may be divided into three main......

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