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Sediment Cores

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USGS Law of the Sea

The USGS Law of the Sea project helps to determine the outer limits of the extended continental shelf (ECS) of the United States. The ECS is that portion of the continental shelf beyond 200 nautical miles. It is an important maritime zone that holds many resources and vital habitats for marine life. Its size may exceed one million square kilometers, encompassing areas in the Arctic, Atlantic...
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USGS Law of the Sea

The USGS Law of the Sea project helps to determine the outer limits of the extended continental shelf (ECS) of the United States. The ECS is that portion of the continental shelf beyond 200 nautical miles. It is an important maritime zone that holds many resources and vital habitats for marine life. Its size may exceed one million square kilometers, encompassing areas in the Arctic, Atlantic...
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Cascadia Subduction Zone Marine Geohazards

Societal Issue: Uncertainty related to rupture extent, slip distribution, and recurrence of past subduction megathrust earthquakes in the Pacific Northwest (northern CA, OR, WA, and southern BC) leads to ambiguity in earthquake and tsunami hazard assessments and hinders our ability to prepare for future events.
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Cascadia Subduction Zone Marine Geohazards

Societal Issue: Uncertainty related to rupture extent, slip distribution, and recurrence of past subduction megathrust earthquakes in the Pacific Northwest (northern CA, OR, WA, and southern BC) leads to ambiguity in earthquake and tsunami hazard assessments and hinders our ability to prepare for future events.
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PCMSC MarFac Field Equipment and Capabilities

Learn about the USGS Pacific Coastal and Marine Science Center Marine Facility’s vast array of field equipment, sampling devices, and mapping systems, and our capabilities. Our engineers, designers, mechanics, and technicians have also designed and developed some of the specialized field equipment we use in field operations in the nearshore, in the deep sea, and on land.
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PCMSC MarFac Field Equipment and Capabilities

Learn about the USGS Pacific Coastal and Marine Science Center Marine Facility’s vast array of field equipment, sampling devices, and mapping systems, and our capabilities. Our engineers, designers, mechanics, and technicians have also designed and developed some of the specialized field equipment we use in field operations in the nearshore, in the deep sea, and on land.
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Drag and sediment transport: conditions at the bottom boundary

Research on bed sediment grain size, bedform morphology, vegetation characteristics, and sediment resuspension and transport.
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Tsunami Hazards, Modeling, and the Sedimentary Record

Basic research to develop the geologic record of paleotsunamis and improve the ability to interpret that record is needed to mitigate tsunami risk in the U.S.
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Piston coring rig

The USGS Pacific Coastal and Marine Science Center’s Marine Facility recently acquired this floating coring rig that features a motorized piston coring unit and is capable of collecting 20-meter sediment cores in calm waters.
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Piston coring rig

The USGS Pacific Coastal and Marine Science Center’s Marine Facility recently acquired this floating coring rig that features a motorized piston coring unit and is capable of collecting 20-meter sediment cores in calm waters.
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VibeCore DW

The VibeCore DW is a small, portable, 24v DC vibracorer
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VibeCore DW

The VibeCore DW is a small, portable, 24v DC vibracorer
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Rossfelder vibracorer

USGS uses the vibracorer is best in locations where the seafloor, lakebed, bay-floor, or river-bottom sediment is unconsolidated and waterlogged.
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Rossfelder vibracorer

USGS uses the vibracorer is best in locations where the seafloor, lakebed, bay-floor, or river-bottom sediment is unconsolidated and waterlogged.
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Jumbo piston corer

Piston corers are generally used in areas with soft sediment, such as clay.
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GOMEX box corer

PCMSC uses the GOMEX box corer for collecting soft, deep-water sediment samples.
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GOMEX box corer

PCMSC uses the GOMEX box corer for collecting soft, deep-water sediment samples.
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Preliminary Analysis of Sedimentary Deposits from the July 17, 1998 Papua New Guinea Tsunami

Preliminary analysis of sedimentary deposits from the tsunami caused by the July 17, 1998 Papua New Guinea earthquake.
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