EXPANSION OF ALPINE GLACIERS IN PACIFIC NORTH AMERICA IN THE FIRST MILLENNIUM A.D
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dc.contributor.author | Reyes A.V. | |
dc.contributor.author | Wiles G.C. | |
dc.contributor.author | Smith D.J. | |
dc.contributor.author | Allen S. | |
dc.contributor.author | Jackson S. | |
dc.contributor.author | Larocque S. | |
dc.contributor.author | Laxton S. | |
dc.contributor.author | Lewis D. | |
dc.contributor.author | Barclay D.J. | |
dc.contributor.author | Calkin P.E. | |
dc.contributor.author | Clague J.J. | |
dc.date.accessioned | 2024-12-07T09:08:09Z | |
dc.date.available | 2024-12-07T09:08:09Z | |
dc.date.issued | 2006 | |
dc.identifier | https://www.elibrary.ru/item.asp?id=14702816 | |
dc.identifier.citation | Geology, 2006, 34, 1, 57-60 | |
dc.identifier.issn | 0091-7613 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/46880 | |
dc.description.abstract | Radiocarbon ages and lichen-dated moraines from 17 glaciers in coastal and near-coastal British Columbia and Alaska document a widespread glacier advance during the first millennium A.D. Glaciers at several sites began advancing ca. A.D. 200-300 based on radiocarbon-dated overridden forests. The advance is centered on A.D. 400-700, when glaciers along an ~2000 km transect of the Pacific North American cordillera overrode forests, impounded lakes, and deposited moraines. The synchroneity of this glacier advance and inferred cooling over a large area suggest a regional climate forcing and, together with other proxy evidence for late Holocene environmental change during the Medieval Warm Period and Little Ice Age, provide support for milleannial-scale climate variability in the North Pacific region. © 2006 Geological Society of America. | |
dc.subject | ALASKA | |
dc.subject | BRITISH COLUMBIA | |
dc.subject | GLACIER | |
dc.subject | HOLOCENE | |
dc.subject | NEOGLACIATION | |
dc.subject | PALEOCLIMATE | |
dc.title | EXPANSION OF ALPINE GLACIERS IN PACIFIC NORTH AMERICA IN THE FIRST MILLENNIUM A.D | |
dc.type | Статья | |
dc.identifier.doi | 10.1130/G21902.1 | |
dc.subject.age | Cenozoic::Quaternary::Holocene | |
dc.subject.age | Кайнозой::Четвертичная::Голоцен |
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