The Geochemistry of englacial brine from Taylor Glacier, Antarctica.

Abstract: Blood Falls is a hypersaline, iron‐rich discharge at the terminus of the Taylor Glacier in the McMurdo Dry Valleys, Antarctica. In November 2014, brine in a conduit within the glacier was penetrated and sampled using clean‐entry techniques and a thermoelectric melting probe called the IceM...

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Bibliographic Details
Main Authors: B Gardner, Christopher, Lyons, W. Berry Lyons
Format: Dataset
Language:unknown
Published: IEDA: US Antarctic Program Data Center 2019
Subjects:
Subglacial Brine
Chemistry:Ice
Glaciology
Antarctica
Glaciers/Ice Sheet
Cryosphere
Geochemistry
US Antarctic Program Data Center (USAP-DC)
Antarctic
Blood Falls
McMurdo Dry Valleys
Taylor Glacier
Antarc*
Ice Sheet
Online Access:http://get.iedadata.org/metadata/iso/601179

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