Abstract
The range of genetic and climatic interpretations of Scottish ‘hummocky moraine’ is reviewed, and new data are presented from the Isle of Skye, western Scotland, which are used as the basis of a genetic classification. ‘Hummocky moraine’ on Skye is shown to consist of three principal sediment-landform associations: (1) recessional moraines; (2) chaotic ice-stagnation moraines; and (3) drumlins and fluted moraines. The recessional moraines consist of transverse moraine ridges and chains of mounds, and were formed by a combination of glaciotectonics and debris accumulation at active ice margins. Second, chaotic moraines consist of randomly-distributed hummocks, mounds and rim-ridges and record deposition in contact with inactive ice. Finally, drumlins and fluted moraines are longitudinally-oriented subglacial bedforms formed by a combination of lodgement and sediment deformation. Individual occurrences of ‘hummocky moraine’ may comprise one, two or all of these associations. The detailed study and differentiation of Scottish ‘hummocky moraine’ provides a valuable source of information on former glacier dynamics and landscape change.
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