A GLACIAL LAKE OUTBURST FLOOD ASSOCIATED WITH RECENT MOUNTAIN GLACIER RETREAT, PATAGONIAN ANDES

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dc.contributor.author Harrison S.
dc.contributor.author Glasser N.
dc.contributor.author Winchester V.
dc.contributor.author Haresign E.
dc.contributor.author Warren C.
dc.contributor.author Jansson K.
dc.date.accessioned 2025-04-12T04:42:28Z
dc.date.available 2025-04-12T04:42:28Z
dc.date.issued 2006
dc.identifier https://elibrary.ru/item.asp?id=14631492
dc.identifier.citation The Holocene, 2006, 16, 4, 611-620
dc.identifier.issn 0959-6836
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/48922
dc.description.abstract Geomorphological mapping, sedimentology, lichenometry and dendrochronology were used to assess the nature and timing of glacier recession, moraine development and catastrophic mass movements in a tributary of the Leones valley, east of the Hielo Patagónico Norte, Chile. We show that during the 'Little Ice Age' Glaciar Calafate advanced downvalley to produce a terminal moraine. Recession of the glacier from this position occurred in the 1870s and produced a moraine dammed lake. In late 2000 a large rockfall into the lake breached the moraine and triggered a glacial lake outburst flood (GLOF) that entrained and subsequently deposited some 2 × 106 m3 of material. We interpret this event as a delayed paraglacial response to the retreat of Glaciar Calafate during the twentieth century. © 2006 Edward Arnold (Publishers) Ltd.
dc.subject 'LITTLE ICE AGE'
dc.subject GLACIAL LAKE OUTBURST FLOOD (GLOF)
dc.subject GLACIER
dc.subject MASS MOVEMENT
dc.subject PARAGLACIAL
dc.subject PATAGONIA
dc.title A GLACIAL LAKE OUTBURST FLOOD ASSOCIATED WITH RECENT MOUNTAIN GLACIER RETREAT, PATAGONIAN ANDES
dc.type Статья
dc.identifier.doi 10.1191/0959683606hl957rr


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