The 2015 Chileno Valley glacial lake outburst flood, Patagonia
نویسندگان
چکیده
منابع مشابه
Paleohydraulics of the last outburst flood from glacial Lake Agassiz and the 8200 BP cold event
During the last deglaciation of North America, huge proglacial lakes formed along the southern margin of the Laurentide Ice Sheet. The largest of these was glacial Lake Agassiz, which formed about 11:7 C kyr and drained into Hudson Bay about 7:7 C kyr ð8:45 cal kyrÞ: Overflow from these lakes was variably directed to the Mississippi, St. Lawrence and Mackenzie drainage systems and it is thought...
متن کاملThe use of one- and two-dimensional hydraulic modelling to reconstruct a glacial outburst flood in a steep Alpine valley
In most cases authors are permitted to post their version of the article (e.g. in Word or Tex form) to their personal website or institutional repository. Authors requiring further information regarding Elsevier's archiving and manuscript policies are encouraged to visit: Summary The hydrologic characteristics of the 1943 outburst flood from the Glacier du Mont Miné, Switzerland, are herein rec...
متن کاملDigital landscapes of deglaciation: Identifying Late Quaternary glacial lake outburst
High resolution DEMs obtained from LiDAR topographic data have led to 9 improved landform inventories (e.g. landslides and fault scarps) and understanding of 10 geomorphic event frequency. Here we use airborne LiDAR mapping to investigate 11 meltwater pathways associated with the Tweed Valley palaeo ice-stream (UK). In particular 12 we focus on a gorge downstream of Palaeolake Milfield, previou...
متن کاملGlacial lake drainage in Patagonia (13-8 kyr) and response of the adjacent Pacific Ocean
Large freshwater lakes formed in North America and Europe during deglaciation following the Last Glacial Maximum. Rapid drainage of these lakes into the Oceans resulted in abrupt perturbations in climate, including the Younger Dryas and 8.2 kyr cooling events. In the mid-latitudes of the Southern Hemisphere major glacial lakes also formed and drained during deglaciation but little is known abou...
متن کاملReduced North Atlantic deep water coeval with the glacial Lake Agassiz freshwater outburst.
An outstanding climate anomaly 8200 years before the present (B.P.) in the North Atlantic is commonly postulated to be the result of weakened overturning circulation triggered by a freshwater outburst. New stable isotopic and sedimentological records from a northwest Atlantic sediment core reveal that the most prominent Holocene anomaly in bottom-water chemistry and flow speed in the deep limb ...
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ژورنال
عنوان ژورنال: Geomorphology
سال: 2019
ISSN: 0169-555X
DOI: 10.1016/j.geomorph.2019.01.015