Shed Brook Discontinuity and Little Falls Gravel: Evidence for the Erie interstade in central New York

Bulletin of the Geological Society of America

Volumn 109, Issue 6, 1997, Pages 652-665

  Ridge, John C ^a  

^a TUFTS UNIVERSITY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

CATCHMENTS; DEPOSITS; GRAVEL; LAKES; RIVER DIVERSION; STRATIGRAPHY;

CLIMATIC CHANGES; CONTINENTAL SHELVES; LACUSTRINE DEPOSITS; LAST DEGLACIATION; PALEOMAGNETIC DECLINATIONS; THERMOHALINE CIRCULATIONS; VARVE CHRONOLOGIES; WESTERN ATLANTIC; BRAIDED RIVER; FLUVIAL UNITS; NEW YORK;

LANDFORMS;

BRAIDED RIVER; CLIMATE CHANGE; CORRELATION; DISCONTINUITY; EROSION; GEOCHRONOLOGY; GRAVEL BED STREAM; IMPOUNDMENT; THERMOHALINE CIRCULATION; UNCONFORMITY; VARVE; WISCONSINAN; CHRONOLOGY; ERIE INTERSTADE; ICE RECESSION; INTERSTADE; INTERSTADIAL; LAKE DRAINAGE;

ATLANTIC OCEAN; ATLANTIC OCEAN (NORTH); HUDSON RIVER; HUDSON VALLEY; LITTLE FALLS; LONG ISLAND SOUND; MINNESOTA; MISSISSIPPI VALLEY; MOHAWK VALLEY; NEW ENGLAND; NEW JERSEY; NEW YORK [UNITED STATES]; ONTARIO [CANADA]; UNITED STATES; NEW YORK; USA;

EID: 0031439822     PISSN: 00167606     EISSN: None     Source Type: Journal    
DOI: 10.1130/0016-7606(1997)109<0652:SBDALF>2.3.CO;2     Document Type: Article

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