Official websites use .gov
A .gov website belongs to an official government organization in the United States.
Secure .gov websites use HTTPS
A lock () or https:// means you’ve safely connected to the .gov website. Share sensitive information only on official, secure websites.
Pacific Coastal and Marine Science Center images.
Figure 4: Results of geomorphic change analysis in the reservoir delta of Jenkinson Lake for 3 time intervals after the Caldor Fire: (a) October–November 2021; (b) 2021–2022, (c) 2022–2023. Refer to text for explanation of time steps. Color legend indicates vertical change detected from DEM differencing.
Figure 4: Results of geomorphic change analysis in the reservoir delta of Jenkinson Lake for 3 time intervals after the Caldor Fire: (a) October–November 2021; (b) 2021–2022, (c) 2022–2023. Refer to text for explanation of time steps. Color legend indicates vertical change detected from DEM differencing.
Western ends of each site showing the overall accretion using QGIS. See legend for color corresponding dates. The first continuous shoreline for each respective year was used for the visualization. (a) Rockaway Peninsula, (b) Long Beach, (c) Jones Beach Island.
Western ends of each site showing the overall accretion using QGIS. See legend for color corresponding dates. The first continuous shoreline for each respective year was used for the visualization. (a) Rockaway Peninsula, (b) Long Beach, (c) Jones Beach Island.
The Long Island study area, including (a,b) the overall location of Long Island with respect to New York and the greater U.S.
The Long Island study area, including (a,b) the overall location of Long Island with respect to New York and the greater U.S.
Scientists and technicians from the Woods Hole Coastal and Marine Science Center (WHCMSC) in Woods Hole, Massachusetts traveled to the Pacific Coastal and Marine Science Center (PCMSC) in Santa Cruz, California to learn about their seafloor imaging and sampling instrument—the Benthic Observation camera Sled, or BOBSled.
Scientists and technicians from the Woods Hole Coastal and Marine Science Center (WHCMSC) in Woods Hole, Massachusetts traveled to the Pacific Coastal and Marine Science Center (PCMSC) in Santa Cruz, California to learn about their seafloor imaging and sampling instrument—the Benthic Observation camera Sled, or BOBSled.
Image of Santa Cruz wharf during Dec 23 2024 storm taken from a CoastCam atop the Dream Inn hotel.
Image of Santa Cruz wharf during Dec 23 2024 storm taken from a CoastCam atop the Dream Inn hotel.
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.
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.
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 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 with the study area delineated by the black rectangle (Base map, IASC, 2004).
Regional location map and bathymetry of the Arctic Ocean with the study area delineated by the black rectangle (Base map, IASC, 2004).
Photos of each substrate type upon collection. (A) Basalt; (B) Ferromanganese (FeMn) crust; (C) Sedimentary; and (D) Phosphorite rock.
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 landslide deposit.
Cascadia sparker data with ghosts removed, with annotation identifying geologic contacts, offset layers, and a submarine landslide deposit.
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.
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.
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.
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.
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.
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. Subsequent images are overlays that are offset with colors inverted, to simulate ghost reflections found in sparker seismic data.
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.
Diagram of system designed to record signature of outgoing sparker source, from the study Practical approaches to maximizing the resolution of sparker seismic reflection data.
Diagram of system designed to record signature of outgoing sparker source, from the study Practical approaches to maximizing the resolution of sparker seismic reflection data.
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.
Example sparker data from Cascadia Subduction Zone showing multiple ghost reflections that reduce the overall resolution of the image.
Example sparker data from Cascadia Subduction Zone showing multiple ghost reflections that reduce the overall resolution of the image.
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.