Assessment of Per- and Polyfluoroalkyl Substances (PFAS) in West Virginia Public Source-Water Supplies
Assessment of Per- and Polyfluoroalkyl Substances (PFAS) in West Virginia Public Source-Water SuppliesWhat are PFAS?
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What are PFAS?
The Landsat archive at EROS contains an unparalleled 50 years of Earth observation data. But with earlier technologies, some Landsat scenes were collected and stored only by international ground receiving stations rather than in the central archive at EROS.
The Landsat archive at EROS contains an unparalleled 50 years of Earth observation data. But with earlier technologies, some Landsat scenes were collected and stored only by international ground receiving stations rather than in the central archive at EROS.
Government officials and scientists had high hopes for Landsat when the first experimental satellite launched July 23, 1972. Those hopes were soon realized when imagery came back depicting features never before seen. Since then, an archive of imagery surpassing 10 million scenes has amassed at EROS, collected from eight different Landsat satellites.
Government officials and scientists had high hopes for Landsat when the first experimental satellite launched July 23, 1972. Those hopes were soon realized when imagery came back depicting features never before seen. Since then, an archive of imagery surpassing 10 million scenes has amassed at EROS, collected from eight different Landsat satellites.
Aerial image of storm waves along a Florida coastline
El aumento de riesgos por inundaciones a lo largo de nuestras costas está causado por el cambio climático, el desarrollo urbano y la pérdida de hábitat.
El aumento de riesgos por inundaciones a lo largo de nuestras costas está causado por el cambio climático, el desarrollo urbano y la pérdida de hábitat.
Coral reefs are important for supporting biodiversity, fisheries, tourism, and coastal protection, but are in decline worldwide, primarily due to extreme heat waves and subsequent coral bleaching, in addition to other stressors.
Coral reefs are important for supporting biodiversity, fisheries, tourism, and coastal protection, but are in decline worldwide, primarily due to extreme heat waves and subsequent coral bleaching, in addition to other stressors.
The complex, three-dimensional reefs built by corals over hundreds to thousands of years provide invaluable ecosystem services to society—contributing billions of dollars per year to the global economy through shoreline protection, tourism, and habitat for biodiversity and fisheries.
The complex, three-dimensional reefs built by corals over hundreds to thousands of years provide invaluable ecosystem services to society—contributing billions of dollars per year to the global economy through shoreline protection, tourism, and habitat for biodiversity and fisheries.
Damage to Yellowstone National Park north entrance road due to June 2022 flooding
Mike Poland, scientist-in-charge of the Yellowstone Volcano Observatory, describes activity at Yellowstone volcano in this monthly update for July 1, 2022.
Mike Poland, scientist-in-charge of the Yellowstone Volcano Observatory, describes activity at Yellowstone volcano in this monthly update for July 1, 2022.
Keeping Tabs on the Volcanoes of the Last Frontier
An Update from the Alaska Volcano Observatory
By Michelle Coombs, USGS Research Geologist
Scientist-in-Charge, Alaska Volcano Observatory
Keeping Tabs on the Volcanoes of the Last Frontier
An Update from the Alaska Volcano Observatory
By Michelle Coombs, USGS Research Geologist
Scientist-in-Charge, Alaska Volcano Observatory
Dr. Christopher G. Smith pumps water from a submarine groundwater well on the seafloor through tubing to the R/V Halimeda and uses an instrument called a YSI to measure salinity and ensure the wells are working properly and producing groundwater.
Dr. Christopher G. Smith pumps water from a submarine groundwater well on the seafloor through tubing to the R/V Halimeda and uses an instrument called a YSI to measure salinity and ensure the wells are working properly and producing groundwater.
Dr. Christopher G. Smith pumps water from a submarine groundwater well on the seafloor through tubing to the R/V Halimeda and uses an instrument called a YSI to measure salinity and ensure the wells are working properly and producing groundwater.
Dr. Christopher G. Smith pumps water from a submarine groundwater well on the seafloor through tubing to the R/V Halimeda and uses an instrument called a YSI to measure salinity and ensure the wells are working properly and producing groundwater.
Dr. Christopher G. Smith pumps water from a submarine groundwater well on the seafloor through tubing to the R/V Halimeda and uses an instrument called a YSI to measure salinity and ensure the wells are working properly and producing groundwater.
Dr. Christopher G. Smith pumps water from a submarine groundwater well on the seafloor through tubing to the R/V Halimeda and uses an instrument called a YSI to measure salinity and ensure the wells are working properly and producing groundwater.
A team from the USGS St. Petersburg Coastal and Marine Science Center heads out into the Gulf of Mexico to check on a set of recently installed groundwater wells. These types of wells allow scientists to monitor submarine groundwater through time and quantify the flux of groundwater from Florida’s aquifer into the coastal waters of the west Florida Shelf.
A team from the USGS St. Petersburg Coastal and Marine Science Center heads out into the Gulf of Mexico to check on a set of recently installed groundwater wells. These types of wells allow scientists to monitor submarine groundwater through time and quantify the flux of groundwater from Florida’s aquifer into the coastal waters of the west Florida Shelf.
We don't need a scientist to tell us that city streets catch and hold heat. Anyone who's walked barefoot from a parking lot to a beach can tell you that. What scientists can help us understand, particularly scientists who work with spaceborne, remotely sensed data, is just how big a difference there is between cities and the countryside.
We don't need a scientist to tell us that city streets catch and hold heat. Anyone who's walked barefoot from a parking lot to a beach can tell you that. What scientists can help us understand, particularly scientists who work with spaceborne, remotely sensed data, is just how big a difference there is between cities and the countryside.
This video acts as a “visual abstract” for a recent publication analyzing the stormwater management practices in Clarksburg, MD. The video features interviews with the team of USGS scientists as well as a water specialist from Montgomery County.
This video acts as a “visual abstract” for a recent publication analyzing the stormwater management practices in Clarksburg, MD. The video features interviews with the team of USGS scientists as well as a water specialist from Montgomery County.
Illustration of Landsat satellite generations over 50 years
50 years of teamwork. 50 years of innovation. 50 years of resilience. In 1966, Secretary of the Interior Stewart Udall announced his vision to create a program aimed at gathering facts about the natural resources of the Earth from Earth orbiting satellites. It was a bold proclamation. It was also an idea that worked and continues to work 50 years on.
50 years of teamwork. 50 years of innovation. 50 years of resilience. In 1966, Secretary of the Interior Stewart Udall announced his vision to create a program aimed at gathering facts about the natural resources of the Earth from Earth orbiting satellites. It was a bold proclamation. It was also an idea that worked and continues to work 50 years on.
Restored staghorn coral (Acropora cervicornis) at Looe Key reef in the lower Florida Keys outplanted by Mote Marine Laboratory's coral restoration program.
Restored staghorn coral (Acropora cervicornis) at Looe Key reef in the lower Florida Keys outplanted by Mote Marine Laboratory's coral restoration program.
The lava lake in Halema‘uma‘u, at the summit of Kīlauea, remains active. On Wednesday, June 15, a small collapse of a portion of the lake rim created a dusty plume and lake agitation, including waves that traveled across the lake surface.
The lava lake in Halema‘uma‘u, at the summit of Kīlauea, remains active. On Wednesday, June 15, a small collapse of a portion of the lake rim created a dusty plume and lake agitation, including waves that traveled across the lake surface.
Over the last few weeks, Woods Hole scientists have been mapping the seafloor of Nantucket Sound as part of a long-term partnership with the State of Massachusetts.
Over the last few weeks, Woods Hole scientists have been mapping the seafloor of Nantucket Sound as part of a long-term partnership with the State of Massachusetts.
Color video preview image
This timelapse sequence shows the evolution of the lava lake and rise of the crater floor in Halema‘uma‘u, at the summit of Kīlauea Volcano, since the eruption start in September 2021. Much of the the crater floor rise is driven by lava supplied beneath the surface crust. The camera is located on the west rim of the summit caldera, looking east.
This timelapse sequence shows the evolution of the lava lake and rise of the crater floor in Halema‘uma‘u, at the summit of Kīlauea Volcano, since the eruption start in September 2021. Much of the the crater floor rise is driven by lava supplied beneath the surface crust. The camera is located on the west rim of the summit caldera, looking east.
Between January 14-15, 2022, volcanic eruptions destroyed much of Hunga Tonga-Hunga Ha'apai, an uninhabited island in the Tonga archipelago in the southern Pacific Ocean. A plume of ash rising 36 miles into the atmosphere blanketed the neighboring Tongan islands.
Between January 14-15, 2022, volcanic eruptions destroyed much of Hunga Tonga-Hunga Ha'apai, an uninhabited island in the Tonga archipelago in the southern Pacific Ocean. A plume of ash rising 36 miles into the atmosphere blanketed the neighboring Tongan islands.
Seafloor features such as sulfide mounds and chimneys are prominent evidence of hydrothermal activity. These features, whether active or dormant, are just the tip of the iceberg, so to speak; much of the “plumbing” of hydrothermal systems exists beneath the seafloor surface.
Seafloor features such as sulfide mounds and chimneys are prominent evidence of hydrothermal activity. These features, whether active or dormant, are just the tip of the iceberg, so to speak; much of the “plumbing” of hydrothermal systems exists beneath the seafloor surface.