Bennett, Matthew R., Boulton, Geoffrey S. (1993) A reinterpretation of Scottish ‘hummocky moraine’ and its significance for the deglaciation of the Scottish Highlands during the Younger Dryas or Loch Lomond Stadial. Geological Magazine, 130 (3) 301-318 doi:10.1017/s0016756800019993
| Reference Type | Journal (article/letter/editorial) | ||
|---|---|---|---|
| Title | A reinterpretation of Scottish ‘hummocky moraine’ and its significance for the deglaciation of the Scottish Highlands during the Younger Dryas or Loch Lomond Stadial | ||
| Journal | Geological Magazine | ||
| Authors | Bennett, Matthew R. | Author | |
| Boulton, Geoffrey S. | Author | ||
| Year | 1993 (May) | Volume | 130 |
| Issue | 3 | ||
| Publisher | Cambridge University Press (CUP) | ||
| DOI | doi:10.1017/s0016756800019993Search in ResearchGate | ||
| Generate Citation Formats | |||
| Mindat Ref. ID | 255760 | Long-form Identifier | mindat:1:5:255760:5 |
| GUID | 0 | ||
| Full Reference | Bennett, Matthew R., Boulton, Geoffrey S. (1993) A reinterpretation of Scottish ‘hummocky moraine’ and its significance for the deglaciation of the Scottish Highlands during the Younger Dryas or Loch Lomond Stadial. Geological Magazine, 130 (3) 301-318 doi:10.1017/s0016756800019993 | ||
| Plain Text | Bennett, Matthew R., Boulton, Geoffrey S. (1993) A reinterpretation of Scottish ‘hummocky moraine’ and its significance for the deglaciation of the Scottish Highlands during the Younger Dryas or Loch Lomond Stadial. Geological Magazine, 130 (3) 301-318 doi:10.1017/s0016756800019993 | ||
| In | (1993, May) Geological Magazine Vol. 130 (3) Cambridge University Press (CUP) | ||
| Abstract/Notes | AbstractThe aim of this paper is to demonstrate that much of the ‘hummocky moraine’ present within the northern part of the LochLomond Readvance ice cap formerly situated in the North West Scottish Highlands may be interpreted as suites of ice-front moraines deposited during active decay. These landforms can be used to reconstruct ice cap decay, whichleads to important insights into the shrinking form of the ice cap and associated environmental conditions. Evidence has been collected from 10803 airphotographs and from detailed field survey. It is presented at three spatial scales. | ||
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