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Autor:
JESSICA A. BADGELEY, ERIN C. PETTIT, CHRISTINA G. CARR, SLAWEK TULACZYK, JILL A. MIKUCKI, W. BERRY LYONS
Publikováno v:
Journal of Glaciology, Vol 63, Pp 387-400 (2017)
Taylor Glacier hosts an active englacial hydrologic system that feeds Blood Falls, a supraglacial outflow of iron-rich subglacial brine at the terminus, despite mean annual air temperatures of −17°C and limited surface melt. Taylor Glacier is an o
Externí odkaz:
https://doaj.org/article/bd333f16254645f5a2ec94cda8d7d1f4
