An englacial hydrologic system of brine within a cold glacier: Blood Falls, McMurdo Dry Valleys, Antarctica
ABSTRACT 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 outlet glacier of the East Antarctic ice shee...
| Published in: | Journal of Glaciology |
|---|---|
| Main Authors: | , , , , , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Cambridge University Press (CUP)
2017
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| Subjects: | |
| Online Access: | http://dx.doi.org/10.1017/jog.2017.16 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143017000168 |