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...

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Bibliographic Details
Main Authors: Gardner, Christopher B., Lyons, W. Berry
Format: Dataset
Language:unknown
Published: IEDA: US Antarctic Program Data Center 2019
Subjects:
Online Access:https://search.dataone.org/view/sha256:dab22c6ec8284978c2dc527bbeadc354a962da8dc4c754f82689ef4dc4cb4681