englacial


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Related to englacial: subglacial

en·gla·cial

 (ĕn-glā′shəl)
adj.
Located or occurring within a glacier.
American Heritage® Dictionary of the English Language, Fifth Edition. Copyright © 2016 by Houghton Mifflin Harcourt Publishing Company. Published by Houghton Mifflin Harcourt Publishing Company. All rights reserved.

englacial

(ɪnˈɡleɪsɪəl)
adj
(Physical Geography) embedded in, carried by, or running through a glacier: englacial drift; an englacial river.
enˈglacially adv
Collins English Dictionary – Complete and Unabridged, 12th Edition 2014 © HarperCollins Publishers 1991, 1994, 1998, 2000, 2003, 2006, 2007, 2009, 2011, 2014
References in periodicals archive ?
The englacial lake started to develop in the third June 2019 in the glacier of Nullah just before the jungle in Rogali valley at an elevation of 4500 meters above sea level.
The National Science Foundation sponsored the research, titled "An Englacial Hydrologie System of Brine Within a Cold Glacier: Blood Falls, McMurdo Dry Valleys, Antarctica," Journal of Glaciology, April 24,2017."
The heat from those eruptions would have melted massive amounts of ice to create englacial lakes--bodies of water that form within glaciers like liquid bubbles in a half-frozen ice cube.
The predominance of non-local lithologies suggest that the till is englacial or supraglacial (Dreimanis 1976), most likely deposited from stagnant or retreating ice.
The heat from those eruptions would have melted massive amounts of ice to form englacial lakes -- bodies of water that form within glaciers like liquid bubbles in a half-frozen ice cube.
The heat from those eruptions would have melted massive amounts of ice to form englacial lakes - bodies of water that form within glaciers like liquid bubbles in a half-frozen ice cube.
Matsuoka, "Pitfalls in radar diagnosis of ice-sheet bed conditions: lessons from englacial attenuation models," Geophysical Research Letters, vol.
We initiated mass balance, terminus and englacial temperature measurements on the Crusoe, Baby (Fig.
Exceptions to this trend are caused by the release of far-traveled carbonates from the englacial load of glaciers during formation of end moraines.
Eskers are the infillings of ice-walled stream channels, and may record deposition in subglacial, englacial or supraglacial drainage networks.