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

dc.contributor.authorHarrison S.
dc.contributor.authorGlasser N.
dc.contributor.authorWinchester V.
dc.contributor.authorHaresign E.
dc.contributor.authorWarren C.
dc.contributor.authorJansson K.
dc.date.accessioned2025-04-12T04:42:28Z
dc.date.available2025-04-12T04:42:28Z
dc.date.issued2006
dc.description.abstractGeomorphological 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.identifierhttps://elibrary.ru/item.asp?id=14631492
dc.identifier.citationThe Holocene, 2006, 16, 4, 611-620
dc.identifier.doi10.1191/0959683606hl957rr
dc.identifier.issn0959-6836
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/48922
dc.subject'LITTLE ICE AGE'
dc.subjectGLACIAL LAKE OUTBURST FLOOD (GLOF)
dc.subjectGLACIER
dc.subjectMASS MOVEMENT
dc.subjectPARAGLACIAL
dc.subjectPATAGONIA
dc.titleA GLACIAL LAKE OUTBURST FLOOD ASSOCIATED WITH RECENT MOUNTAIN GLACIER RETREAT, PATAGONIAN ANDES
dc.typeСтатья

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