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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