Continental Rises
Continental Rises is a deep-sea geomorphic feature that constitutes the gently sloping sedimentary accumulation zone at the base of the continental slope, distinguishing itself from adjacent continental margins and abyssal plains by its transitional position and thick, graded deposits derived from turbidity currents and contourite processes.
155
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12.2K
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365
Authors
168
Institutions
Publications per year
2017–2026
6
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155
Mountain belts and the new global tectonics
John Dewey, John Bird · Journal of Geophysical Research Atmospheres · 1970 · 1.6K citations
Sequences in the Cratonic Interior of North America
L. L. Sloss · Geological Society of America Bulletin · 1963 · 1.2K citations
Continental divide: Heidegger, Cassirer, Davos
Choice Reviews Online · 2010 · 424 citations
1–5 of 155
365
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Woods Hole Oceanographic Institution, United States
4 publications · 637 citations
4
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1–5 of 365
168

Lamont-Doherty Earth Observatory
Sparkill, United States
14 h-index
29 publications
3.6K citations
Columbia University
New York, United States
9 h-index
21 publications
2.8K citations
Woods Hole Oceanographic Institution
Falmouth, United States
9 h-index
18 publications
495 citations
National Institute of Oceanography and Applied Geophysics
Trieste, Italy
5 h-index
12 publications
447 citations
United States Geological Survey
Reston, United States
5 h-index
7 publications
1.1K citations
University of Rhode Island
Kingston, United States
4 h-index
6 publications
305 citations
Woodwell Climate Research Center
Falmouth, United States
4 h-index
16 publications
2.3K citations
University of Cambridge
Cambridge, United Kingdom
4 h-index
4 publications
1.8K citations
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14 publications · 2.7K citations
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15 publications · 1K citations
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14 publications · 494 citations
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JGR · 9 publications · 2.4K citations
9
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8 publications · 368 citations
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