D
David C. Mosher
Researcher at Bedford Institute of Oceanography
Publications - 145
Citations - 3727
David C. Mosher is an academic researcher from Bedford Institute of Oceanography. The author has contributed to research in topics: Continental margin & Continental shelf. The author has an hindex of 28, co-authored 142 publications receiving 3385 citations. Previous affiliations of David C. Mosher include Durham University & Geological Survey of Canada.
Papers
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Journal ArticleDOI
The International Bathymetric Chart of the Arctic Ocean (IBCAO) Version 3.0
Martin Jakobsson,Larry A. Mayer,Bernard Coakley,Julian A. Dowdeswell,Steve Forbes,Boris Fridman,Hanne Hodnesdal,Riko Noormets,Richard Pedersen,Michele Rebesco,Hans Werner Schenke,Yulia Zarayskaya,Daniela Accettella,Andy Armstrong,Robert M Anderson,Paul Bienhoff,Angelo Camerlenghi,I. Church,Margo H. Edwards,James V. Gardner,John K. Hall,Benjamin Hell,Ole Hestvik,Yngve Kristoffersen,Christian Marcussen,Rezwan Mohammad,David C. Mosher,Son V. Nghiem,Maria T. Pedrosa,Paola Travaglini,Pauline Weatherall +30 more
TL;DR: The International Bathymetric Chart of the Arctic Ocean (IBCAO) released its first gridded bathymetric compilation in 1999 as discussed by the authors, which has since supported a wide range of Arc...
Book ChapterDOI
Submarine Mass Movements and Their Consequences
Yasuhiro Yamada,Kiichiro Kawamura,Ken Ikehara,Yujiro Ogawa,Roger Urgeles,David C. Mosher,Jason D. Chaytor,Michael Strasser,Michael Strasser +8 more
TL;DR: Weimer et al. as discussed by the authors showed that 30% of the World's population lives within 60 km of the coast, and the hazard posed by submarine landslides is expected to grow as global sea level rises.
Journal ArticleDOI
Near-surface geology and sediment-failure geohazards of the central Scotian Slope
TL;DR: The central Scotian slope is characterized by a relatively smooth seafloor, but with numerous 1080m (33260ft)-high escarpments representing slide failure scars as discussed by the authors.
Journal ArticleDOI
Late Quaternary sediment, sediment mass flow processes and slope stability on the Scotian Slope, Canada
TL;DR: In this paper, the authors show that a large portion of the near surface sediment (<20 m) in the area has undergone erosion, rotational slumping and internal deformation, and the most plausible explanation for large scale slope failures in this region are ground accelerations related to earthquake shock.
Journal ArticleDOI
Erosion and deposition of fine‐grained sediments from the Bay of Fundy
Carl L. Amos,David C. Mosher +1 more
TL;DR: In this article, the authors evaluated the sedimentation character of fine-grained cohesive sediment from two field studies and a flume experiment with undisturbed sediment from the Bay of Fundy.