Geologists examining the Ross Sea Drift sediments exposed in Commonwealth Stream, New Harbour, Taylor Valley. Layers of silt and gravel were deposited in an ancient lake that formed when Taylor Valley was dammed by Ross Sea Ice between 12,000 and 30,000
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DepictsDuncan Ritchie
Dougal TownsendChristian OhneiserProgrammeK105 Southern Victoria Land geological mappingSeason2008-2009LocationCommonwealth Stream
Dougal TownsendChristian OhneiserProgrammeK105 Southern Victoria Land geological mappingSeason2008-2009LocationCommonwealth StreamReference
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Geologists examining the Ross Sea Drift sediments exposed in Commonwealth Stream, New Harbour, Taylor Valley. Layers of silt and gravel were deposited in an ancient lake that formed when Taylor Valley was dammed by Ross Sea Ice between 12,000 and 30,000 . Antarctica NZ, accessed 13/12/2024, https://adam.antarcticanz.govt.nz/nodes/view/32601