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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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