A low, oblique aerial view of the west vent in Halema‘uma‘u at Kīlauea's summit (upper right) taken during an overflight on May 13. The area of active lava has slowly been decreasing in recent weeks, but not all of the lava lake surface has stagnated. Portions of the lake surface continue to resurface via a process called foundering.
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.
A low, oblique aerial view of the west vent in Halema‘uma‘u at Kīlauea's summit (upper right) taken during an overflight on May 13. The area of active lava has slowly been decreasing in recent weeks, but not all of the lava lake surface has stagnated. Portions of the lake surface continue to resurface via a process called foundering.
Connecting powerline rights-of-way vegetation management to improve pollinator habitat. A USGS RAMPS technician samples pollinating insects along the Salt River Project powerline that crosses through Apache-Sitgreaves and Tonto National Forests.
Connecting powerline rights-of-way vegetation management to improve pollinator habitat. A USGS RAMPS technician samples pollinating insects along the Salt River Project powerline that crosses through Apache-Sitgreaves and Tonto National Forests.
Halema‘uma‘u eruption activity on May 12, 2021 — Kīlauea summit
Halema‘uma‘u eruption activity on May 12, 2021 — Kīlauea summitA close up view of the western portion of the lava lake within Halema‘uma‘u, at Kīlauea summit. A weak gas plume is emitted from the western fissure vent (left), with the most recent sulfur dioxide emission rate measured at 150 tonnes per day on May 11. USGS photograph taken by D. Downs on May 12, 2021 from the west rim of Halema‘uma‘u.
Halema‘uma‘u eruption activity on May 12, 2021 — Kīlauea summit
Halema‘uma‘u eruption activity on May 12, 2021 — Kīlauea summitA close up view of the western portion of the lava lake within Halema‘uma‘u, at Kīlauea summit. A weak gas plume is emitted from the western fissure vent (left), with the most recent sulfur dioxide emission rate measured at 150 tonnes per day on May 11. USGS photograph taken by D. Downs on May 12, 2021 from the west rim of Halema‘uma‘u.
Halema‘uma‘u eruption activity on May 12, 2021 — Kīlauea summit
Halema‘uma‘u eruption activity on May 12, 2021 — Kīlauea summitA wide view of Halema‘uma‘u from the western crater rim, at the summit of Kīlauea. The west vent (lower left) continues to supply lava into the lake through a submerged inlet. Much of the western active lava lake surface has crusted over in the last few weeks as the effusion rate remains low. USGS photograph taken by D. Downs on May 12, 2021.
Halema‘uma‘u eruption activity on May 12, 2021 — Kīlauea summit
Halema‘uma‘u eruption activity on May 12, 2021 — Kīlauea summitA wide view of Halema‘uma‘u from the western crater rim, at the summit of Kīlauea. The west vent (lower left) continues to supply lava into the lake through a submerged inlet. Much of the western active lava lake surface has crusted over in the last few weeks as the effusion rate remains low. USGS photograph taken by D. Downs on May 12, 2021.
Puerto Rico study area and Hurricane María path and data
Puerto Rico study area and Hurricane María path and data(Left) Map of Puerto Rico showing study area location (red box), the oceanographic buoys (orange triangles), and the track of María with eye timing and locations (black dots) in 6-hour increments and the wind radii of 64-knot winds (gray circular outlines).
Puerto Rico study area and Hurricane María path and data
Puerto Rico study area and Hurricane María path and data(Left) Map of Puerto Rico showing study area location (red box), the oceanographic buoys (orange triangles), and the track of María with eye timing and locations (black dots) in 6-hour increments and the wind radii of 64-knot winds (gray circular outlines).
During the annual Mauna Loa GPS campaign, 33 campaign stations are occupied with GPS instruments for days to weeks. The stations are spread across the flanks of the volcano and provide a synoptic picture of deformation on the volcano over the past year.
During the annual Mauna Loa GPS campaign, 33 campaign stations are occupied with GPS instruments for days to weeks. The stations are spread across the flanks of the volcano and provide a synoptic picture of deformation on the volcano over the past year.
Another GPS survey benchmark being occupied on Mauna Loa's north flank, with clear views of Mauna Kea in the background. The metal disk on the ground beneath the tripod is the benchmark, which is cemented to the lava flow surface.
Another GPS survey benchmark being occupied on Mauna Loa's north flank, with clear views of Mauna Kea in the background. The metal disk on the ground beneath the tripod is the benchmark, which is cemented to the lava flow surface.
Global Positioning System (GPS) survey of Mauna Loa recently completed
Global Positioning System (GPS) survey of Mauna Loa recently completedRecently, HVO geophysicists completed the annual high-precision Global Positioning System (GPS) survey of Mauna Loa. The annual survey supplements HVO's continuous GPS monitoring stations and provides information on vertical and horizontal deformation of the ground surface.
Global Positioning System (GPS) survey of Mauna Loa recently completed
Global Positioning System (GPS) survey of Mauna Loa recently completedRecently, HVO geophysicists completed the annual high-precision Global Positioning System (GPS) survey of Mauna Loa. The annual survey supplements HVO's continuous GPS monitoring stations and provides information on vertical and horizontal deformation of the ground surface.
On the west side of Mauna Loa summit, a campaign GPS (center-right) measures its location for a period of 2–3 days. This site has been occupied every year by helicopter since 1994. Mauna Kea, Hualālai and Haleakalā can be seen in the distance. USGS photo taken by S.
On the west side of Mauna Loa summit, a campaign GPS (center-right) measures its location for a period of 2–3 days. This site has been occupied every year by helicopter since 1994. Mauna Kea, Hualālai and Haleakalā can be seen in the distance. USGS photo taken by S.
The Region 1, May 2021 "Honorable Mention #1" Winner (by Chelsea Delsack)
The Region 1, May 2021 "Honorable Mention #1" Winner (by Chelsea Delsack)
Scientists aboard research vessel conduct water-quality mapping
Scientists aboard research vessel conduct water-quality mappingScientists aboard R/V Aiken conduct water-quality mapping in support of wastewater-derived nutrients project
Scientists aboard research vessel conduct water-quality mapping
Scientists aboard research vessel conduct water-quality mappingScientists aboard R/V Aiken conduct water-quality mapping in support of wastewater-derived nutrients project
Upstream view from 03108000 - Raccoon Creek at Moffatts Mill, PA
Upstream view from 03108000 - Raccoon Creek at Moffatts Mill, PAThe Region 1, May 2021 "Where We Work" Winner (by Ian Lynch)
Upstream view from 03108000 - Raccoon Creek at Moffatts Mill, PA
Upstream view from 03108000 - Raccoon Creek at Moffatts Mill, PAThe Region 1, May 2021 "Where We Work" Winner (by Ian Lynch)
The lava lake in Halema‘uma‘u crater, at the summit of Kīlauea, remains active, as seen in this view looking northwest. The active surface lava area continues to decrease in size, and activity is weaker, with only occasional localized surface foundering.
The lava lake in Halema‘uma‘u crater, at the summit of Kīlauea, remains active, as seen in this view looking northwest. The active surface lava area continues to decrease in size, and activity is weaker, with only occasional localized surface foundering.
This map of Halema‘uma‘u at the summit of Kīlauea shows 20 m (66 ft) contour lines (dark gray) that mark locations of equal elevation above sea level (asl). The map shows that the lava lake has filled 229 m (751 ft) of the crater, to an elevation of 746 m (2448 ft) asl since the eruption began on December 20, 2020.
This map of Halema‘uma‘u at the summit of Kīlauea shows 20 m (66 ft) contour lines (dark gray) that mark locations of equal elevation above sea level (asl). The map shows that the lava lake has filled 229 m (751 ft) of the crater, to an elevation of 746 m (2448 ft) asl since the eruption began on December 20, 2020.
An Acoustic Doppler Current Profiler (ADCP) on the deck of the R/V Sallenger ready to be deployed in the water. The ADCP now sits on the bottom of the ocean off Madeira beach, Florida in 5m water depth.
An Acoustic Doppler Current Profiler (ADCP) on the deck of the R/V Sallenger ready to be deployed in the water. The ADCP now sits on the bottom of the ocean off Madeira beach, Florida in 5m water depth.
Close-up view of active western portion of Halema‘uma‘u lava lake
Close-up view of active western portion of Halema‘uma‘u lava lakeThis close-up view of the active western portion of the Halema‘uma‘u lava lake at the summit of Kīlauea was captured on Thursday, May 6 through the lens of a laser rangefinder used by HVO scientists to measure distances to features within the crater.
Close-up view of active western portion of Halema‘uma‘u lava lake
Close-up view of active western portion of Halema‘uma‘u lava lakeThis close-up view of the active western portion of the Halema‘uma‘u lava lake at the summit of Kīlauea was captured on Thursday, May 6 through the lens of a laser rangefinder used by HVO scientists to measure distances to features within the crater.
Scientific divers BJ Reynolds and Hunter Wilcox prepare to lower an Acoustic Doppler Current Profiler (ADCP) into the water. The ADCP now sits on the bottom of the ocean off Madeira beach, Florida in 5m water depth.
Scientific divers BJ Reynolds and Hunter Wilcox prepare to lower an Acoustic Doppler Current Profiler (ADCP) into the water. The ADCP now sits on the bottom of the ocean off Madeira beach, Florida in 5m water depth.
View of the active surface lava in the western portion of Halema‘uma‘u, at the summit of Kīlauea Volcano. The west vent (upper left) continues to erupt lava into the lava lake through an inlet near the base of the cone.
View of the active surface lava in the western portion of Halema‘uma‘u, at the summit of Kīlauea Volcano. The west vent (upper left) continues to erupt lava into the lava lake through an inlet near the base of the cone.
Lava continues to flow from the western vent (bottom left) into the lava lake at Halema‘uma‘u Crater at the summit of Kīlauea Volcano, Island of Hawai‘i. A portion of the active surface of the lava lake can be seen here with orange, incandescent lava between the west vent and the main island. This photograph was taken on Wednesday, March 5, 2021, at 12:37 p.m.
Lava continues to flow from the western vent (bottom left) into the lava lake at Halema‘uma‘u Crater at the summit of Kīlauea Volcano, Island of Hawai‘i. A portion of the active surface of the lava lake can be seen here with orange, incandescent lava between the west vent and the main island. This photograph was taken on Wednesday, March 5, 2021, at 12:37 p.m.
Hillshade of lidar acquired within the Pinto Mountain Fault Zone
Hillshade of lidar acquired within the Pinto Mountain Fault ZoneThe image shown displays a portion of the lidar data collected by the USGS for the SAFSOC Project. Our goal is to study and map surficial processes and landforms related to tectonism, specifically the San Andreas Fault system.
Hillshade of lidar acquired within the Pinto Mountain Fault Zone
Hillshade of lidar acquired within the Pinto Mountain Fault ZoneThe image shown displays a portion of the lidar data collected by the USGS for the SAFSOC Project. Our goal is to study and map surficial processes and landforms related to tectonism, specifically the San Andreas Fault system.
Multi-parameter probes, temperature and dissolved oxygen sensors
Multi-parameter probes, temperature and dissolved oxygen sensors(A) Examples of the multi-parameter water-quality probes used for continuous fixed-station monitoring, moving boat surveys, and vertical water-quality profiles. (B) Example of smaller temperature and dissolved oxygen sensors with and without a wiper unit.
Multi-parameter probes, temperature and dissolved oxygen sensors
Multi-parameter probes, temperature and dissolved oxygen sensors(A) Examples of the multi-parameter water-quality probes used for continuous fixed-station monitoring, moving boat surveys, and vertical water-quality profiles. (B) Example of smaller temperature and dissolved oxygen sensors with and without a wiper unit.