Hormones and pharmaceuticals, widely used for treatment of humans, domestic animals, and livestock, have the potential to enter the environment, including groundwater. In 2009, nearly 70% of Americans took at least one prescription drug, and more than half took 2 or more.
Images
Explore our planet through photography and imagery, including climate change and water all the way back to the 1800s when the USGS was surveying the country by horse and buggy.
Hormones and pharmaceuticals, widely used for treatment of humans, domestic animals, and livestock, have the potential to enter the environment, including groundwater. In 2009, nearly 70% of Americans took at least one prescription drug, and more than half took 2 or more.
School Branch at Maloney Road near Brownsburg IN - dry stream
School Branch at Maloney Road near Brownsburg IN - dry streamSchool Branch at Maloney Road near Brownsburg IN - dry stream
School Branch at Maloney Road near Brownsburg IN - dry stream
School Branch at Maloney Road near Brownsburg IN - dry streamSchool Branch at Maloney Road near Brownsburg IN - dry stream
School Branch at Maloney Road near Brownsburg IN - equipment
School Branch at Maloney Road near Brownsburg IN - equipmentSchool Branch at Maloney Road near Brownsburg IN - equipment
School Branch at Maloney Road near Brownsburg IN - equipment
School Branch at Maloney Road near Brownsburg IN - equipmentSchool Branch at Maloney Road near Brownsburg IN - equipment
School Branch at Maloney Road near Brownsburg IN - measurement
School Branch at Maloney Road near Brownsburg IN - measurementSchool Branch at Maloney Road near Brownsburg IN - measurement
School Branch at Maloney Road near Brownsburg IN - measurement
School Branch at Maloney Road near Brownsburg IN - measurementSchool Branch at Maloney Road near Brownsburg IN - measurement
School Branch at Maloney Road near Brownsburg IN - measuring stream
School Branch at Maloney Road near Brownsburg IN - measuring streamSchool Branch at Maloney Road near Brownsburg IN - measuring stream width
School Branch at Maloney Road near Brownsburg IN - measuring stream
School Branch at Maloney Road near Brownsburg IN - measuring streamSchool Branch at Maloney Road near Brownsburg IN - measuring stream width
School Branch at Maloney Road near Brownsburg IN - no flow
School Branch at Maloney Road near Brownsburg IN - no flowSchool Branch at Maloney Road near Brownsburg IN - no flow
School Branch at Maloney Road near Brownsburg IN - no flow
School Branch at Maloney Road near Brownsburg IN - no flowSchool Branch at Maloney Road near Brownsburg IN - no flow
School Branch at Maloney Road near Brownsburg IN - stream measurement
School Branch at Maloney Road near Brownsburg IN - stream measurementSchool Branch at Maloney Road near Brownsburg IN - stream measurement
School Branch at Maloney Road near Brownsburg IN - stream measurement
School Branch at Maloney Road near Brownsburg IN - stream measurementSchool Branch at Maloney Road near Brownsburg IN - stream measurement
Serapeum, a Roman Marketplace in Pozzuoli, Italy, records deformation of Campi Flegrei caldera over two millennia.
Serapeum, a Roman Marketplace in Pozzuoli, Italy, records deformation of Campi Flegrei caldera over two millennia.
USGS researchers deploying a prototype DTS fiber optic cable
USGS researchers deploying a prototype DTS fiber optic cableNortheast Region Photo Contest Winner | October 2018 | USGS at Work
USGS researchers deploying a prototype DTS fiber optic cable array in the Delaware River
USGS researchers deploying a prototype DTS fiber optic cable
USGS researchers deploying a prototype DTS fiber optic cableNortheast Region Photo Contest Winner | October 2018 | USGS at Work
USGS researchers deploying a prototype DTS fiber optic cable array in the Delaware River
Gravel bar on the north fork of the Agashashok River, Alaska
Gravel bar on the north fork of the Agashashok River, AlaskaA gravel bar on the north fork of the Agashashok River, Alaska. This work is part of the Hydro-Ecology of Arctic Thawing (HEAT): Hydrology project that takes place in the Arctic Network Parks because they lie in a region that is rapidly warming.
Gravel bar on the north fork of the Agashashok River, Alaska
Gravel bar on the north fork of the Agashashok River, AlaskaA gravel bar on the north fork of the Agashashok River, Alaska. This work is part of the Hydro-Ecology of Arctic Thawing (HEAT): Hydrology project that takes place in the Arctic Network Parks because they lie in a region that is rapidly warming.
Kankakee River at Davis, IN - camera on gage
USGS hydrologic technicians train Kootenai Tribe of Idaho staff
USGS hydrologic technicians train Kootenai Tribe of Idaho staffUSGS hydrologic technicians Keith Hein and Pete Elliott explain site selection and operation of USGS streamgages to staff members of the Kootenai Tribe of Idaho's Fish and Wildlife Department at streamgage station 12310100, Kootenai River at Tribal Hatchery near Bonners Ferry, Idaho.
USGS hydrologic technicians train Kootenai Tribe of Idaho staff
USGS hydrologic technicians train Kootenai Tribe of Idaho staffUSGS hydrologic technicians Keith Hein and Pete Elliott explain site selection and operation of USGS streamgages to staff members of the Kootenai Tribe of Idaho's Fish and Wildlife Department at streamgage station 12310100, Kootenai River at Tribal Hatchery near Bonners Ferry, Idaho.
View into Halema‘uma‘u from the west rim of Kīlauea's summit ca
View into Halema‘uma‘u from the west rim of Kīlauea's summit caView into Halema‘uma‘u from the west rim of Kīlauea's summit caldera. USGS photo: J. Kauahikaua, 03 March 2019
View into Halema‘uma‘u from the west rim of Kīlauea's summit ca
View into Halema‘uma‘u from the west rim of Kīlauea's summit caView into Halema‘uma‘u from the west rim of Kīlauea's summit caldera. USGS photo: J. Kauahikaua, 03 March 2019
Aerial view due south of the Mono Lake-Long Valley volcanic region. Inset map shows locations of latest Pleistocene–Holocene silicic magmatic centers relative to Long Valley caldera. Rhyolites of the Mono–Inyo chain are shown in pink, and the dacitic–rhyodacitic Mammoth Mountain dome complex is shown in blue. U.S.
Aerial view due south of the Mono Lake-Long Valley volcanic region. Inset map shows locations of latest Pleistocene–Holocene silicic magmatic centers relative to Long Valley caldera. Rhyolites of the Mono–Inyo chain are shown in pink, and the dacitic–rhyodacitic Mammoth Mountain dome complex is shown in blue. U.S.
Huckleberry Ridge Tuff deposit exposed on Mt. Everts, Yellowstone National Park
Huckleberry Ridge Tuff deposit exposed on Mt. Everts, Yellowstone National ParkHuckleberry Ridge Tuff deposit exposed on Mt. Everts, near the northern boundary of Yellowstone National Park. The deposit was created by ash falling from the plume early in the eruption sequence, 2.08 million years ago. Photo by Madison Myers, Montana State University.
Huckleberry Ridge Tuff deposit exposed on Mt. Everts, Yellowstone National Park
Huckleberry Ridge Tuff deposit exposed on Mt. Everts, Yellowstone National ParkHuckleberry Ridge Tuff deposit exposed on Mt. Everts, near the northern boundary of Yellowstone National Park. The deposit was created by ash falling from the plume early in the eruption sequence, 2.08 million years ago. Photo by Madison Myers, Montana State University.
Lindsay Carlson swabbing hunter harvested ducks in western Alaska
Lindsay Carlson swabbing hunter harvested ducks in western AlaskaLindsay Carlson swabbing hunter-harvested ducks in western Alaska as part of USGS research to investigate the persistence of avian influenza viruses in North American wetlands. USGS scientists and colleagues found that influenza A viruses may remain infectious in surface waters of northern wetlands for more than seven months.
Lindsay Carlson swabbing hunter harvested ducks in western Alaska
Lindsay Carlson swabbing hunter harvested ducks in western AlaskaLindsay Carlson swabbing hunter-harvested ducks in western Alaska as part of USGS research to investigate the persistence of avian influenza viruses in North American wetlands. USGS scientists and colleagues found that influenza A viruses may remain infectious in surface waters of northern wetlands for more than seven months.
An egret walks in the surf of Dauphin Island beach
An egret walks in the surf of Dauphin Island beachAn egret walks in the shallow surf of an undeveloped beach on Dauphin Island, Alabama, with buildings viewed in the background from a different area on the island.
An egret walks in the surf of Dauphin Island beach
An egret walks in the surf of Dauphin Island beachAn egret walks in the shallow surf of an undeveloped beach on Dauphin Island, Alabama, with buildings viewed in the background from a different area on the island.
Collecting larval fish for the Dragonfly Mercury Project
Collecting larval fish for the Dragonfly Mercury ProjectBetween 2009 and 2018, scientists conducted a national scale assessment of mercury accumulation in the National Park System using dragonfly larvae as biosentinels (species that accumulate a pollutant in their tissues as an index of exposure to other organisms without significant adverse effects to the biosentinel) through a citizen science network called the Dragonf
Collecting larval fish for the Dragonfly Mercury Project
Collecting larval fish for the Dragonfly Mercury ProjectBetween 2009 and 2018, scientists conducted a national scale assessment of mercury accumulation in the National Park System using dragonfly larvae as biosentinels (species that accumulate a pollutant in their tissues as an index of exposure to other organisms without significant adverse effects to the biosentinel) through a citizen science network called the Dragonf
Photograph of the entrance to Grand Traverse Bay Harbor
Photograph of the entrance to Grand Traverse Bay HarborPhotograph of the entrance to Grand Traverse Bay Harbor, located 8 kilometers downdrift of the spoils pile. Migration of the dark-colored stamp sands (moving from left to right) has buried the original beach, overtopped the wall, and partially blocked the channel.
Photograph of the entrance to Grand Traverse Bay Harbor
Photograph of the entrance to Grand Traverse Bay HarborPhotograph of the entrance to Grand Traverse Bay Harbor, located 8 kilometers downdrift of the spoils pile. Migration of the dark-colored stamp sands (moving from left to right) has buried the original beach, overtopped the wall, and partially blocked the channel.
Photograph of the R/V Rafael alongside dock near the survey site
Photograph of the R/V Rafael alongside dock near the survey sitePhotograph of the R/V Rafael alongside dock near the survey site on Lake Superior.
Photograph of the R/V Rafael alongside dock near the survey site
Photograph of the R/V Rafael alongside dock near the survey sitePhotograph of the R/V Rafael alongside dock near the survey site on Lake Superior.
Photograph showing a high scarp cut into the large pile of stamp sands
Photograph showing a high scarp cut into the large pile of stamp sandsPhotograph showing a high scarp cut into the large pile of stamp sands at the town of Gay, Michigan. Nearly a century of erosion by waves and currents has transported millions of cubic yards of mine tailings along the coast and spread them across the adjacent lake floor.
Photograph showing a high scarp cut into the large pile of stamp sands
Photograph showing a high scarp cut into the large pile of stamp sandsPhotograph showing a high scarp cut into the large pile of stamp sands at the town of Gay, Michigan. Nearly a century of erosion by waves and currents has transported millions of cubic yards of mine tailings along the coast and spread them across the adjacent lake floor.