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Images

Pacific Coastal and Marine Science Center images.

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A remotely operated vehicle collecting rock samples from the Eastern Galapágos Spreading Center
Collecting rock samples from the Eastern Galapágos Spreading Center
Collecting rock samples from the Eastern Galapágos Spreading Center
Collecting rock samples from the Eastern Galapágos Spreading Center

Collecting rock samples from the Eastern Galapágos Spreading Center, during the expedition Ultra-Fine Scale Seafloor Mapping in October-November 2023.

Hydrothermal chimneys at the Eastern Galapágos Spreading Center
Hydrothermal chimneys at the Eastern Galapágos Spreading Center
Hydrothermal chimneys at the Eastern Galapágos Spreading Center
Hydrothermal chimneys at the Eastern Galapágos Spreading Center

Hydrothermal chimneys at the Eastern Galapágos Spreading Center, from the expedition Ultra-Fine Scale Seafloor Mapping in October-November 2023.

Tubeworms found at the Eastern Galapágos Spreading Center
Tubeworms found at the Eastern Galapágos Spreading Center
Tubeworms found at the Eastern Galapágos Spreading Center
Tubeworms found at the Eastern Galapágos Spreading Center

Tubeworms found at the Eastern Galapágos Spreading Center, from the expedition Ultra Fine-Scale Seafloor Mapping, in October-November 2023.

Diagram showing seismic profile and sediment core collected at Hosgri fault
Diagram showing seismic profile and sediment core collected at Hosgri fault
Diagram showing seismic profile and sediment core collected at Hosgri fault
Diagram showing seismic profile and sediment core collected at Hosgri fault

Compressed high-intensity radar pulse (chirp) profile HFC-9 located south of the Cross-Hosgri slope (CHS). Profile crosses the midshelf region and images the extensive transgressive surface of erosion unconformity (blue) also seen below the CHS. The seafloor is delineated in red.

Compressed high-intensity radar pulse (chirp) profile HFC-9 located south of the Cross-Hosgri slope (CHS). Profile crosses the midshelf region and images the extensive transgressive surface of erosion unconformity (blue) also seen below the CHS. The seafloor is delineated in red.

Figure showing cross-sections of the southern Cascadia margin, showing the subsurface structure of the outer arc high
Cross-sections of the southern Cascadia margin, showing the subsurface structure of the outer arc high
Cross-sections of the southern Cascadia margin, showing the subsurface structure of the outer arc high
Figure showing outputs of a metamodel to downscale total water levels in open beaches
Figure showing outputs of a metamodel to downscale total water levels in open beaches
Figure showing outputs of a metamodel to downscale total water levels in open beaches
Figure showing outputs of a metamodel to downscale total water levels in open beaches

A figure showing metamodel outputs to downscale total water levels in open beaches, from the PCMSC Science Seminar presented by Manuel Zornoza-Aguado.

Composite satellite images showing different sea-level rise and flooding scenarios for Lower Nooksack River
Lower Nooksack River flood projections
Lower Nooksack River flood projections
Lower Nooksack River flood projections

National Agricultural Imagery Program (NAIP) composite images showing water depth after 1.6 feet (ft) (0.5 meter [m]) and 3.3 feet (1.0 m) of sea-level rise (SLR) for 50 percent, 10 percent, and 4 percent annual exceedance probability (AEP) stream floods, which are expected in coming decades and which will increasingly affect groundwater, drainage issues, and freque

National Agricultural Imagery Program (NAIP) composite images showing water depth after 1.6 feet (ft) (0.5 meter [m]) and 3.3 feet (1.0 m) of sea-level rise (SLR) for 50 percent, 10 percent, and 4 percent annual exceedance probability (AEP) stream floods, which are expected in coming decades and which will increasingly affect groundwater, drainage issues, and freque

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