Scott Stanford
Trenton, NJ
Activity
2020
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EVIDENCE FOR LAKE IROQUOIS BREAKOUT FLOODS IN THE HUDSON VALLEY AT 13.2 CAL KA FROM COREHOLES AT SANDY HOOK, NJ
94 D19. Quaternary Geology ITuesday, 27 October 20205:30 PM - 8:00 PMMeeting Rooms
2017
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PRE-WISCONSINAN GLACIATIONS OF NEW JERSEY
31 The Future of Pre-LGM Chronostratigraphy for the Pleistocene: The Glacial and Interglacial RecordMonday, 20 March 20178:00 AM - 12:00 PMConference Center A, Conference Level
2016
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REGIONAL AND LOCAL SOURCES OF RELATIVE SEA-LEVEL CHANGE AT SANDY HOOK, NJ
T263 Dynamics of Continental Margin Sedimentation (Posters)Tuesday, 27 September 20169:00 AM - 6:30 PMExhibit Hall E/F
2015
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GROUNDWATER SEEPAGE, LANDFORMS, AND LANDSCAPE EVOLUTION IN THE NEW JERSEY PINE BARRENS
325 Geomorphology: Channels and Channel Change at Short to Long Time ScalesWednesday, 4 November 20151:30 PM - 5:30 PMRoom 342
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WHY DOES SANDY HOOK HAVE THAT SINKING FEELING?
T197 Coastal Hazards from Minutes to MillenniaTuesday, 3 November 20158:00 AM - 12:00 PMRoom 307
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ONSHORE-OFFSHORE CORRELATION OF QUATERNARY INCISED VALLEYS AND TIDAL PALEOCHANNELS, CAPE MAY, NJ
T39 Continental Shelf and Estuarine Seafloor Mapping and Shallow Stratigraphy on the North American East Coast (Posters)Sunday, 1 November 20159:00 AM - 5:30 PMExhibit Hall