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Pacific Coastal and Marine Science Center images.

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Map with flood extent data on it
CoSMoS flood extent map
CoSMoS flood extent map
CoSMoS flood extent map

Example CoSMoS flood extent map products for the Humboldt County region, showing a 100-year storm across three sea-level rise scenarios.

Example CoSMoS flood extent map products for the Humboldt County region, showing a 100-year storm across three sea-level rise scenarios.

Six figures showing modeled shoreline change projections at Cape Lookout National Seashore
Modeled shoreline change projections at Cape Lookout National Seashore
Modeled shoreline change projections at Cape Lookout National Seashore
Modeled shoreline change projections at Cape Lookout National Seashore

Modeled shoreline change projections overlayed onto maps of some key areas of Cape Lookout National Seashore. Note that the reference shoreline position from 1990 is not shown. Panel (A) shows the shoreline near the historic Portsmouth Village, at the northern extent of the islands, including a ferry terminal.

Modeled shoreline change projections overlayed onto maps of some key areas of Cape Lookout National Seashore. Note that the reference shoreline position from 1990 is not shown. Panel (A) shows the shoreline near the historic Portsmouth Village, at the northern extent of the islands, including a ferry terminal.

Schematic deposit model showing formation of hydrothermal minerals along faults
Schematic deposit model showing formation of hydrothermal minerals along faults
Schematic deposit model showing formation of hydrothermal minerals along faults
Schematic deposit model showing formation of hydrothermal minerals along faults

Schematic deposit model showing formation of hydrothermal Fe- and Mn-oxide deposits at depth along faults during the Neogene (∼8.5–4.8 Ma) from ascending hydrothermal fluids driven by frictional heating and other fault-related processes; the deposits may have experienced minor uplift along faults during the Neogene and Quaternary, and variably exposed as seaflo

Schematic deposit model showing formation of hydrothermal Fe- and Mn-oxide deposits at depth along faults during the Neogene (∼8.5–4.8 Ma) from ascending hydrothermal fluids driven by frictional heating and other fault-related processes; the deposits may have experienced minor uplift along faults during the Neogene and Quaternary, and variably exposed as seaflo

Regional location map and bathymetry of the Arctic Ocean
Regional location map and bathymetry of the Arctic Ocean
Regional location map and bathymetry of the Arctic Ocean
Regional location map and bathymetry of the Arctic Ocean

Regional location map and bathymetry of the Arctic Ocean with the study area delineated by the black rectangle (Base map, IASC, 2004).

Image collage of four photos of various deep-ocean substrate types upon collection
Photos of various deep-ocean substrate types upon collection
Photos of various deep-ocean substrate types upon collection
Photos of various deep-ocean substrate types upon collection

Photos of each substrate type upon collection. (A) Basalt; (B) Ferromanganese (FeMn) crust; (C) Sedimentary; and (D) Phosphorite rock.

Cascadia sparker data with ghosts removed, with annotation identifying geologic contacts, offset layers, and a submarine land
Cascadia sparker data with ghosts removed, with annotation identifying geologic contacts, offset layers, and a submarine landslide deposit
Cascadia sparker data with ghosts removed, with annotation identifying geologic contacts, offset layers, and a submarine landslide deposit
Example annotated orthoimagery of woody debris along the Elwha River
Example annotated orthoimagery of woody debris along the Elwha River
Example annotated orthoimagery of woody debris along the Elwha River
Example annotated orthoimagery of woody debris along the Elwha River

Example annotated images (left column) and resulting label images (right column) made using the software program Doodler (Buscombe et al., 2021). Spacing between ticks is 200 pixels.

Multi-paneled graph of orthoimagery shows example model output of woody debris along Elwha River
Elwha River woody debris example model output
Elwha River woody debris example model output
Elwha River woody debris example model output

Example model outputs for the first (2012-04-07) and last (2017-09-22) aerial survey from a selection of bars in the middle reach (MR) and lower reach (LR) of the Elwha River.

Example model outputs for the first (2012-04-07) and last (2017-09-22) aerial survey from a selection of bars in the middle reach (MR) and lower reach (LR) of the Elwha River.

Four-panel image showing example aerial orthoimagery of wood along Elwha River
Example aerial orthoimagery of wood along Elwha River
Example aerial orthoimagery of wood along Elwha River
Example aerial orthoimagery of wood along Elwha River

Example aerial orthoimagery at a typical location (located in the middle reach of the Elwha River), showing the variation in color and brightness, as well as the nature of the channel, wood deposition, and bar growth.

Example aerial orthoimagery at a typical location (located in the middle reach of the Elwha River), showing the variation in color and brightness, as well as the nature of the channel, wood deposition, and bar growth.

Sub seafloor structure of landslide in Santa Barbara Channel, CA
Sub seafloor structure of landslide in Santa Barbara Channel, CA
Sub seafloor structure of landslide in Santa Barbara Channel, CA
Sub seafloor structure of landslide in Santa Barbara Channel, CA

Example imagery revealing the sub-seafloor structure below a submarine landslide in the Santa Barbara Channel, offshore California. The base of the slide is traced in blue, and the near vertical black lines highlight shallow faults cutting through a zone of uplift located below the slide headscarp.   

Example imagery revealing the sub-seafloor structure below a submarine landslide in the Santa Barbara Channel, offshore California. The base of the slide is traced in blue, and the near vertical black lines highlight shallow faults cutting through a zone of uplift located below the slide headscarp.   

Diagram shows the paths that sound travels away from the sparker source
Diagram showing paths that sound travels away from the sparker source
Diagram showing paths that sound travels away from the sparker source
Diagram showing paths that sound travels away from the sparker source

Diagram shows the paths that the sound travels away from the sparker source (black oval). The ghost reflections are shown in green and orange. PP= Primary Pulse, BP = Bubble Pulse. From the study Practical approaches to maximizing the resolution of sparker seismic reflection data.

Animated GIF of fault zone outcrop from late Miocene–Pliocene period, Western Macedonia, Greece
Animated GIF of fault zone outcrop from late Miocene–Pliocene period, Western Macedonia, Greece
Animated GIF of fault zone outcrop from late Miocene–Pliocene period, Western Macedonia, Greece
Animated GIF of fault zone outcrop from late Miocene–Pliocene period, Western Macedonia, Greece

Animated GIF of fault zone outcrop from late Miocene–Pliocene period, Western Macedonia, Greece. Subsequent images are overlays that are offset with colors inverted, to simulate ghost reflections found in sparker seismic data.

Cover of Coastal Science Navigator Companion Guide. Image shows boat on water.
Companion Guide Cover
Companion Guide Cover
Companion Guide Cover

Cover of the Coastal Science Navigator Companion Guide. The guide introduces some of the many coastal change hazards-related products available through the USGS. In it, we showcase the products included in the Coastal Science Navigator’s initial publication in July 2023.

Cover of the Coastal Science Navigator Companion Guide. The guide introduces some of the many coastal change hazards-related products available through the USGS. In it, we showcase the products included in the Coastal Science Navigator’s initial publication in July 2023.

Personnel from Oregon State University launch a personal water craft into the surf zone during bathymetric surveys
Launching a personal water craft into the surf zone during bathymetric surveys
Launching a personal water craft into the surf zone during bathymetric surveys
Launching a personal water craft into the surf zone during bathymetric surveys

Personnel from Oregon State University launch a personal water craft into the surf zone during bathymetric surveys along the Washington coast.

Diana McCandles collecting topographic data on an all-terrain vehicle
Collecting topographic data on an all-terrain vehicle
Collecting topographic data on an all-terrain vehicle
Collecting topographic data on an all-terrain vehicle

Diana McCandless, an environmental specialist with the Washington State Department of Ecology, collecting topographic data on an all-terrain vehicle.

Diana McCandless, an environmental specialist with the Washington State Department of Ecology, collecting topographic data on an all-terrain vehicle.

USGS Oceanographer Andrew Stevens performing a topographic survey at the base of an eroding dune
Topographic survey at the base of an eroding dune
Topographic survey at the base of an eroding dune
Topographic survey at the base of an eroding dune

USGS Oceanographer Andrew Stevens performing a topographic survey at the base of an eroding dune.

Paige Hovenga, former Graduate Research Assistant at Oregon State University, participating in a dawn topographic survey
Topographic beach survey at dawn
Topographic beach survey at dawn
Topographic beach survey at dawn

Paige Hovenga, former Graduate Research Assistant at Oregon State University, participating in a dawn topographic survey.

Paige Hovenga, former Graduate Research Assistant at Oregon State University, participating in a dawn topographic survey.

Kai Parker, USGS Oceanographer, navigates the surf zone on a personal watercraft during a bathymetric survey
Navigating the surf zone on a personal watercraft during a bathymetric survey
Navigating the surf zone on a personal watercraft during a bathymetric survey
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