Submarine landslide tsunamis: how extreme and how likely?
A number of examples are presented to substantiate that submarine landslides have
occurred along most continental margins and along several volcano flanks. Their properties …
occurred along most continental margins and along several volcano flanks. Their properties …
Morphometry of mass-transport deposits as a predictive tool
L Moscardelli, L Wood - Bulletin, 2016 - pubs.geoscienceworld.org
Mass-transport deposits (MTDs) are gravity-induced units that represent an important
component of modern and ancient deep-water stratigraphic successions. MTDs have been …
component of modern and ancient deep-water stratigraphic successions. MTDs have been …
Circum-Arctic Lithosphere Evolution (CALE) Transect C: displacement of the Arctic Alaska–Chukotka microplate towards the Pacific during opening of the Amerasia …
This paper synthesizes the framework and geological evolution of the Arctic Alaska–
Chukotka microplate (AACM), from its origin as part of the continental platform fringing …
Chukotka microplate (AACM), from its origin as part of the continental platform fringing …
Size‐fractionated compositions of marine suspended particles in the Western Arctic Ocean: Lateral and vertical sources
We present full water depth sections of size‐fractionated (1–51 μm;> 51 μm) concentrations
of suspended particulate matter and major particle phase composition (particulate organic …
of suspended particulate matter and major particle phase composition (particulate organic …
Tsunami hazard assessment of Canada
LJ Leonard, GC Rogers, S Mazzotti - Natural Hazards, 2014 - Springer
We present a preliminary probabilistic tsunami hazard assessment of Canadian coastlines
from local and far-field, earthquake, and large submarine landslide sources. Analyses …
from local and far-field, earthquake, and large submarine landslide sources. Analyses …
True volumes of slope failure estimated from a Quaternary mass‐transport deposit in the northern South China Sea
Submarine slope failure can mobilize large amounts of seafloor sediment, as shown in
varied offshore locations around the world. Submarine landslide volumes are usually …
varied offshore locations around the world. Submarine landslide volumes are usually …
Basalts From the Chukchi Borderland: 40Ar/39Ar Ages and Geochemistry of Submarine Intraplate Lavas Dredged From the Western Arctic Ocean
SB Mukasa, A Andronikov, K Brumley… - Journal of …, 2020 - Wiley Online Library
Submarine volcanism in the western Arctic Ocean, known as Amerasia Basin, is attributed to
a mantle plume based on geophysics and meager geochemical evidence. Basaltic samples …
a mantle plume based on geophysics and meager geochemical evidence. Basaltic samples …
[HTML][HTML] A 100-km wide slump along the upper slope of the Canadian Arctic was likely preconditioned for failure by brackish pore water flushing
CK Paull, SR Dallimore, DW Caress, R Gwiazda… - Marine Geology, 2021 - Elsevier
Exploration of the continental slope of the Canadian Beaufort Sea has revealed a
remarkable coalescence of slide scars with headwalls between 130 and 1100 m water …
remarkable coalescence of slide scars with headwalls between 130 and 1100 m water …
Canada Basin revealed
DC Mosher, J Shimeld, D Hutchinson… - OTC Arctic Technology …, 2012 - onepetro.org
Abstract More than 15,000 line-km of new regional seismic reflection and refractiondata in
the western Arctic Ocean provide insights into the tectonic andsedimentologic history of …
the western Arctic Ocean provide insights into the tectonic andsedimentologic history of …
A submarine landslide complex affecting the Jan Mayen Ridge, Norwegian–Greenland Sea: slide-scar morphology and processes of sediment evacuation
JS Laberg, K Kawamura, H Amundsen, N Baeten… - Geo-Marine Letters, 2014 - Springer
Swath-bathymetry data and 2D multichannel seismics reveal for the first time an up to~ 60
km wide amphitheater-shaped slide scar on the eastern flank of the Jan Mayen Ridge, a …
km wide amphitheater-shaped slide scar on the eastern flank of the Jan Mayen Ridge, a …