Title Morphology and sediments of ice-damned lake after its outburst, West Greenland
Author Cesnulevicius, A.; Seiriene, V.; Kazakauskas, V.; Baltrunas, V.; Sinkunas, P.; Karmaza, B.
Author Affil Cesnulevicius, A., Vilnius Pedagogical University, Department of General Geography, Vilnius, Lithuania. Other: Institute of Geology and Geography, Lithuania
Source Geologija - Vilniaus Universitetas, Vol.65-66, p.42-52, . Publisher: Lietuvos Mokslu Akademijos Leidykla / Academia Publishers, Vilnius, Lithuania. ISSN: 1392- 110X
Publication Date 2009
Notes In English with Lithuanian and Russian summaries. 18 refs. GeoRef Acc. No: 297071
Index Terms algae; drainage; glacial deposits; glaciers; ice; lacustrine deposits; lakes; lake ice; mapping; measurement; melting; sediments; streams; terraces; Greenland--West Greenland; Arctic region; basins; clastic sediments; diatoms; discharge; glacial environment; glacial features; glaciolacustrine environment; Global Positioning System; Greenland; jokulhlaups; lacustrine environment; lake-level changes; microfossils; moraines; morphology; observations; Plantae; Russell Glacier; sand; West Greenland
Abstract Formation of glaciolacustrine basins during glacier recession is predetermined by abundance of supraglacial, inglacial and subglacial waters. Replenishment of glaciolacustrine basins is followed by their sudden drainage associated with glacier outbursts and melting of buried ice in the areas of end moraines, or capture of glaciofluvial streams. The outburst flood that appeared on August 31,2007 in the periphery of the Russell Glacier (West Greenland) caused a rapid drainage of an ice- dammed lake, which exposed a large part of the bottom and the slopes of the basin. The water level in the basin during the drainage subsided by 55 m, and in 11 hours of outburst flood 20 900 000 m3 of water escaped from the basin. The exposed bottom of the glaciolacustrine basin allowed evaluating the sediment complexes. The impact of glaciofluvial stream on the forms of relief was established as well.
URL http://hdl.handle.net/10.2478/v10056-009-0005-1
Publication Type journal article
Record ID 64002154