GlacierHub highlights glacier and stream geochemistry research in the Dry Valleys

A new article on GlacierHub highlights research by MCM LTER collaborator, Sarah Fortner, on the geochemistry of meltwater of the Canada Glacier in the Taylor Valley of Antarctica. Dry Valley glaciers are unique in that their surface geochemistry is an important contributer to the chemistry of downstream ecosystems, such as Lake Hoare. Read more about this fascinating study here.

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