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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.
Aerial photo captured during an overflight of the Northeast Rift Zone eruption of Mauna Loa at approximately 5-6:30 p.m. HST on November 28, 2022. This photo is looking down on a section of the braided lava flow on the northeast flank.
Aerial photo captured during an overflight of the Northeast Rift Zone eruption of Mauna Loa at approximately 5-6:30 p.m. HST on November 28, 2022. This photo is looking down on a section of the braided lava flow on the northeast flank.
Aerial photo captured during an overflight of the Northeast Rift Zone eruption of Mauna Loa at approximately 5-6:30 p.m. HST on November 28, 2022. This photo is looking at the line of fissure vents erupting above 10,000 ft elevation on the Northeast Rift Zone of Mauna Loa.
Aerial photo captured during an overflight of the Northeast Rift Zone eruption of Mauna Loa at approximately 5-6:30 p.m. HST on November 28, 2022. This photo is looking at the line of fissure vents erupting above 10,000 ft elevation on the Northeast Rift Zone of Mauna Loa.
Aerial photo captured during an overflight of the Northeast Rift Zone eruption of Mauna Loa at approximately 5-6:30 p.m. HST on November 28, 2022.
Aerial photo captured during an overflight of the Northeast Rift Zone eruption of Mauna Loa at approximately 5-6:30 p.m. HST on November 28, 2022.
Aerial photograph taken during an overflight of the Northeast Rift Zone eruption of Mauna Loa at approximately 5-6:30 p.m. HST on November 28, 2022. Fissure vents above 10,000 ft on the Northeast Rift Zone generate lava fountains and lava flows to the northeast and parallel to the rift zone. Image courtesy of Civil Air Patrol.
Aerial photograph taken during an overflight of the Northeast Rift Zone eruption of Mauna Loa at approximately 5-6:30 p.m. HST on November 28, 2022. Fissure vents above 10,000 ft on the Northeast Rift Zone generate lava fountains and lava flows to the northeast and parallel to the rift zone. Image courtesy of Civil Air Patrol.
Aerial photo captured during an overflight of the Northeast Rift Zone eruption of Mauna Loa at approximately 5-6:30 p.m. HST on November 28, 2022. This photo shows the line of fissure vents erupting above 10,000 ft elevation on the Northeast Rift Zone of Mauna Loa. Image courtesy of Civil Air Patrol.
Aerial photo captured during an overflight of the Northeast Rift Zone eruption of Mauna Loa at approximately 5-6:30 p.m. HST on November 28, 2022. This photo shows the line of fissure vents erupting above 10,000 ft elevation on the Northeast Rift Zone of Mauna Loa. Image courtesy of Civil Air Patrol.
HVO field crews are at the summit of Mauna Loa to make observations and collect information about the eruption that began on November 27, 2022. The eruption began at the summit and migrated to the Northeast Rift Zone, where this photo was taken around 10:00 am local time (HST) on November 28, 2022.
HVO field crews are at the summit of Mauna Loa to make observations and collect information about the eruption that began on November 27, 2022. The eruption began at the summit and migrated to the Northeast Rift Zone, where this photo was taken around 10:00 am local time (HST) on November 28, 2022.
Mauna Loa eruption as viewed from Waikoloa at about 1:25am local time (HST). The eruption is occurring from the summit of the volcano, though lava has overflowed the caldera.
Mauna Loa eruption as viewed from Waikoloa at about 1:25am local time (HST). The eruption is occurring from the summit of the volcano, though lava has overflowed the caldera.
Hydrologic Unit and National Hydrography Dataset Plus Medium Resolution Spatial Scales Example
Hydrologic Unit and National Hydrography Dataset Plus Medium Resolution Spatial Scales Example
This map of the United States and its territories shows the areal extent and quality level of planned, in-progress, and existing publicly available lidar (IfSAR in Alaska) data identified by the United States Interagency Elevation Inventory (USIEI) that meet 3DEP base level specification planned to be under award by September 30, 2022. 3DEP base level spec
This map of the United States and its territories shows the areal extent and quality level of planned, in-progress, and existing publicly available lidar (IfSAR in Alaska) data identified by the United States Interagency Elevation Inventory (USIEI) that meet 3DEP base level specification planned to be under award by September 30, 2022. 3DEP base level spec
What are PFAS?
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.
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 marshes of Plum Island Estuary are among those predicted by scientists to submerge during the next century under conservative projections of sea-level rise.
The marshes of Plum Island Estuary are among those predicted by scientists to submerge during the next century under conservative projections of sea-level rise.
A photo of the west vent and active western portion of the lava lake within Halema‘uma‘u, at Kīlauea summit. The eastern side of the lava lake (out of view to the right), has a stagnant solidified crust on the surface. USGS photo taken by L. DeSmither on November 3, 2021.
A photo of the west vent and active western portion of the lava lake within Halema‘uma‘u, at Kīlauea summit. The eastern side of the lava lake (out of view to the right), has a stagnant solidified crust on the surface. USGS photo taken by L. DeSmither on November 3, 2021.
A telephoto image of the west vent in Halema‘uma‘u, taken from the northwest rim on November 3. Low roiling lava continues to erupt from the west vent, with occasional larger bursts of spatter. The spatter cone that has built up since the eruption began on September 29, contains ponded lava that supplies the lava lake through the tubed-over spillway.
A telephoto image of the west vent in Halema‘uma‘u, taken from the northwest rim on November 3. Low roiling lava continues to erupt from the west vent, with occasional larger bursts of spatter. The spatter cone that has built up since the eruption began on September 29, contains ponded lava that supplies the lava lake through the tubed-over spillway.
A telephoto image of the west vent in Halema‘uma‘u crater at the summit of Kīlauea. Ponded lava within the spatter cone supplies lava into the lava lake through the tubed-over spillway. The fast-moving lava stream is incandescent as it enters into the lava lake at the base of the cone.
A telephoto image of the west vent in Halema‘uma‘u crater at the summit of Kīlauea. Ponded lava within the spatter cone supplies lava into the lava lake through the tubed-over spillway. The fast-moving lava stream is incandescent as it enters into the lava lake at the base of the cone.
The vent in the western wall of Halema‘uma‘u continues to erupt at the summit of Kīlauea. Volcanic gas emissions, primarily from the west vent (right), remain elevated. Sulfur dioxide (SO2) emission rates were measured at around 3,600 tonnes per day on October 28, 2021. USGS photo taken on November 3, 2021, by L. DeSmither.
The vent in the western wall of Halema‘uma‘u continues to erupt at the summit of Kīlauea. Volcanic gas emissions, primarily from the west vent (right), remain elevated. Sulfur dioxide (SO2) emission rates were measured at around 3,600 tonnes per day on October 28, 2021. USGS photo taken on November 3, 2021, by L. DeSmither.
The extent of the active surface of the lava lake (orange) within Halema‘uma‘u crater, at the summit of Kīlauea, is clearly delineated as the sun sets on November 2, 2021. Photo taken at 5:56 p.m. HST from the west rim. USGS photo by J.M. Chang.
The extent of the active surface of the lava lake (orange) within Halema‘uma‘u crater, at the summit of Kīlauea, is clearly delineated as the sun sets on November 2, 2021. Photo taken at 5:56 p.m. HST from the west rim. USGS photo by J.M. Chang.
A telephoto image of the northeast margin of the lava lake within Halema‘uma‘u, at Kīlauea summit, on November 1, 2021. The lava lake has now risen high enough to start covering the lowest portion of the down-dropped block on the north side of Halema‘uma‘u.
A telephoto image of the northeast margin of the lava lake within Halema‘uma‘u, at Kīlauea summit, on November 1, 2021. The lava lake has now risen high enough to start covering the lowest portion of the down-dropped block on the north side of Halema‘uma‘u.