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The International Bathymetric Chart of the Arctic Ocean (IBCAO) Version 3.0
The International Bathymetric Chart of the Arctic Ocean (IBCAO) released its first gridded bathymetric compilation in 1999. The IBCAO bathymetric portrayals have since supported a wide range of ArcExpand
Late Quaternary deglaciation and sea-level history of eastern Juan de Fuca Strait, Cascadia
Abstract Eastern Juan de Fuca Strait of southwestern British Columbia/northwestern Washington State is near the western and southern terminus of Late Wisconsinan glaciation in North America.Expand
Active tectonics of the Devils Mountain fault and related structures, northern Puget Lowland and eastern Strait of Juan de Fuca region, Pacific Northwest
Information from marine high-resolution and conventional seismic-reflection surveys, acromagnetic mapping, coastal exposures of Pleistocene strata, and lithologic logs of water wells is used toExpand
A Middle–Late Triassic (Ladinian–Rhaetian) carbon and oxygen isotope record from the Tethyan Ocean
Abstract We obtained bulk-sediment δ18O and δ13C data from biostratigraphically-constrained Tethyan marine sections at Aghia Marina (Greece), Guri Zi (Albania), and Brumano and Italcementi QuarryExpand
Late Quaternary stratigraphy and seafloor geology of eastern Juan de Fuca Strait, British Columbia and Washington
Abstract A combination of shallow sediment cores and high-resolution seismic-reflection data were used to identify and map four main surficial geologic units in eastern Juan de Fuca Strait. TheseExpand
The Chronology and Recurrence of Submarine Mass Movements on the Continental Slope Off Southeastern Canada
High-resolution seismic reflection profiles, multibeam bathymetry, piston cores, and biostratigraphy from petroleum wells are used to date submarine mass movements on the continental slope offExpand
Submarine Mass Movements and Their Consequences
Submarine mass movements represent major offshore geohazards due to their destructive and tsunami-generation potential. This potential poses a threat to human life as well as to coastal, near shoreExpand
Near-surface geology and sediment-failure geohazards of the central Scotian Slope
The central Scotian Slope demonstrates a complex seafloor morphology superimposed on a regional gradient of 24 across the margin. The west-central Scotian Slope is characterized by a relativelyExpand
Drilling probes past carbon cycle perturbations on the Demerara Rise
Ocean Drilling Program (ODP) Leg 207 recently cored sediments on the Demerara Rise at ∼9°N in the tropical Atlantic and successfully recovered continuous records of the Paleocene/Eocene ThermalExpand
Late Quaternary sediment, sediment mass flow processes and slope stability on the Scotian Slope, Canada
The study area, just to the west of the Verrill Canyon on the Scotian Slope, eastern Canada, exhibits both large and small scale sediment mass movement features. Study of high resolution seismicExpand
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