| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6446878 | Quaternary Science Reviews | 2012 | 15 Pages |
Abstract
⺠This paper reports new evidence from the Monadhliath Mountains, Scotland. ⺠Deglaciation of the BIIS in the area occurred at ca 15.1 ka. ⺠The YD readvance (11.8-9.8 ka) was smaller due to a drier climate east from the Highlands ice cap. ⺠Our reconstruction confirms the steep SW to NE precipitation gradient across Scotland.
Keywords
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Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
D.M. Gheorghiu, D. Fabel, J.D. Hansom, S. Xu,