Jay A. Stravers
Northern Illinois University
13 Papers
169 Citations
Jay A. Stravers is an academic researcher from Northern Illinois University. The author has contributed to research in topics: Glacial period & Fjord. The author has an hindex of 8, co-authored 12 publications. Previous affiliations of Jay A. Stravers include University of Colorado Boulder & Institute of Arctic and Alpine Research.
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Papers
Late glacial ice margins and deglacial chronology for southeastern Baffin Island and Hudson Strait, eastern Canadian Arctic
TL;DR: Radiocarbon dates from marine piston cores and from onshore raised marine stratigraphic sections in the Hudson Strait region were used to reconstruct deglacial isochrons for 9900, 9500, 8800, 8500,... as discussed by the authors.
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Abrupt early Holocene (9.9-9.6 ka) ice-stream advance at the mouth of Hudson Strait, Arctic Canada
TL;DR: Radiocarbon-dated glacial-geologic evidence documents an abrupt advance of the northern margin of the Labrador sector of the Laurentide Ice Sheet during the last deglaciation as discussed by the authors.
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Seismic facies changes along a nearly continuous 24 latitudinal transect :the fjords of chile and the northern antarctic peninsula
TL;DR: In this paper, high-resolution seismic reflection profiles and piston cores from bays, fjords, and straits of the inland passage of Chile and the northern Antarctic Peninsula region were used to examine changes in seismic facies along a nearly continuous 24 ° latitudinal transect that encompasses temperate, subpolar, and polar climatic regimes.
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Land-sea correlations and evolution of the Cambridge Fiord marine basin during the last deglaciation of Northern Baffin island
TL;DR: In this paper, a mean value of 2.34 × 106 m3/yer for deposits trapped in the inner fiord basins is given. But this is not the case for all the sediments in the upper fiord.
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Glacial debris flow deposits on the baffin island shelf : seismic facies architecture of till-tongue-like deposits
Jay A. Stravers,Ross D. Powell +1 more
TL;DR: In this paper, a 3D seismic facies modeling of late Foxe/Wisconsin glacial deposits in the Savage Basin provides important new data concerning the morphology and origin of acoustically unstratified seismic units on high-latitude continental shelves.
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