The Geochemistry of englacial brine from Taylor Glacier, Antarctica.

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 IceMole. We an...

Full description

Bibliographic Details
Main Authors: B Gardner, Christopher, Lyons, W. Berry Lyons
Format: Dataset
Language:English
Published: U.S. Antarctic Program (USAP) Data Center 2019
Subjects:
Online Access:https://dx.doi.org/10.15784/601179
http://www.usap-dc.org/view/dataset/601179