Peacock, J.D., Rose, J. (2017) Was the Younger Dryas (Loch Lomond Stadial) icefield on Rannoch Moor, western Scotland, deglaciated as early as c.12.5 cal ka BP?. Proceedings of the Geologists' Association, 128 (2) 173-179 doi:10.1016/j.pgeola.2017.02.002

Reference Type | Journal (article/letter/editorial) | ||
---|---|---|---|
Title | Was the Younger Dryas (Loch Lomond Stadial) icefield on Rannoch Moor, western Scotland, deglaciated as early as c.12.5 cal ka BP? | ||
Journal | Proceedings of the Geologists' Association | ||
Authors | Peacock, J.D. | Author | |
Rose, J. | Author | ||
Year | 2017 (April) | Volume | 128 |
Issue | 2 | ||
Publisher | Elsevier BV | ||
DOI | doi:10.1016/j.pgeola.2017.02.002Search in ResearchGate | ||
Generate Citation Formats | |||
Mindat Ref. ID | 295551 | Long-form Identifier | mindat:1:5:295551:7 |
GUID | 0 | ||
Full Reference | Peacock, J.D., Rose, J. (2017) Was the Younger Dryas (Loch Lomond Stadial) icefield on Rannoch Moor, western Scotland, deglaciated as early as c.12.5 cal ka BP?. Proceedings of the Geologists' Association, 128 (2) 173-179 doi:10.1016/j.pgeola.2017.02.002 | ||
Plain Text | Peacock, J.D., Rose, J. (2017) Was the Younger Dryas (Loch Lomond Stadial) icefield on Rannoch Moor, western Scotland, deglaciated as early as c.12.5 cal ka BP?. Proceedings of the Geologists' Association, 128 (2) 173-179 doi:10.1016/j.pgeola.2017.02.002 | ||
In | (2017, April) Proceedings of the Geologists' Association Vol. 128 (2) Elsevier BV |
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