6 Quaternary and Environmental
Sunday, 19 March 2017
10:15 AM - 12:00 PM
Allegheny, 17th Floor
TWO LATE PLEISTOCENE FLOODS IN THE SCHENECTADY, NY, AREA AND THE DEMOTION OF THE DELMAR READVANCE
Paper number: 6-4
Program: Technical Sessions
Time: 11:15 AM – 11:35 AM
Authors
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Eric HansonClifton Park, NY
Abstract
Exposures of a second, near-surface diamict have been mapped along the Colonie Reservoir and in test borings drilled for a regional ground water study. The second, younger diamict can be traced from the Albany Airport to Round Lake. The younger flood eroded the Ballston-Round Lake-Drummond channels, scoured out the Round Lake and Saratoga Lake depressions, and deposited the Wilton subaqueous fan. It marks the transition from the Albany II to the Quaker Springs stages of Lake Albany, which occured approximately 11,900 14C years ago.
The trace of the Delmar ‘readvance’ marks a still-stand of the glacier.
Geological Society of America Abstracts with Programs. Vol. 49, No. 2
doi: 10.1130/abs/2017NE-291144
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