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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.

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Aerial view of ocean entry
Kīlauea Volcano — Kapoho Ocean Entry
Kīlauea Volcano — Kapoho Ocean Entry
Kīlauea Volcano — Kapoho Ocean Entry

An aerial view of the Kapoho ocean entry, as of 6:30 a.m. HST today, shows the extent of the lava delta, now about 200 acres in size, that has formed over the past six days (lava first entered the ocean on the night of June 3).

An aerial view of the Kapoho ocean entry, as of 6:30 a.m. HST today, shows the extent of the lava delta, now about 200 acres in size, that has formed over the past six days (lava first entered the ocean on the night of June 3).

R/V Petrel leaving the dock in Beach Haven, NJ to begin the geophysical survey in May 2018.
R/V Petrel leaving the dock in Beach Haven, NJ
R/V Petrel leaving the dock in Beach Haven, NJ
R/V Petrel leaving the dock in Beach Haven, NJ

) R/V Petrel leaving the dock in Beach Haven, NJ to begin the geophysical survey in May 2018.

Scientists setting up a weatherport for shelter on St. Matthew Island, Alaska
Setting up a weatherport on St. Matthew Island, Alaska
Setting up a weatherport on St. Matthew Island, Alaska
Setting up a weatherport on St. Matthew Island, Alaska

Scientists setting up a weatherport for shelter while conducting research on St. Matthew Island Alaska.

Scientists setting up a weatherport for shelter while conducting research on St. Matthew Island Alaska.

Kīlauea lower East Rift Zone lava flows and fissures, June 8, 12:00...
Kīlauea LERZ lava flows and fissures, June 8, 12:00 p.m.
Kīlauea LERZ lava flows and fissures, June 8, 12:00 p.m.
Kīlauea LERZ lava flows and fissures, June 8, 12:00 p.m.

Map as of 12:00 p.m. (noon) HST, June 8, 2018. Given the dynamic nature of Kīlauea's lower East Rift Zone eruption, with changing vent locations, fissures starting and stopping, and varying rates of lava effusion, map details shown here are accurate as of the date/time noted. Shaded purple areas indicate lava flows erupted in 1840, 1955, 1960, and 2014-2015.

Map as of 12:00 p.m. (noon) HST, June 8, 2018. Given the dynamic nature of Kīlauea's lower East Rift Zone eruption, with changing vent locations, fissures starting and stopping, and varying rates of lava effusion, map details shown here are accurate as of the date/time noted. Shaded purple areas indicate lava flows erupted in 1840, 1955, 1960, and 2014-2015.

Plumes from ocean entry
Kīlauea Volcano — Kapoho Bay and Vacationland
Kīlauea Volcano — Kapoho Bay and Vacationland
Kīlauea Volcano — Kapoho Bay and Vacationland

HVO's early morning helicopter overflight of Kīlauea's lower East Rift Zone showed that lava continues to flow into the ocean in the vicinity of Kapoho Bay and Vacationland.

HVO's early morning helicopter overflight of Kīlauea's lower East Rift Zone showed that lava continues to flow into the ocean in the vicinity of Kapoho Bay and Vacationland.

Lava fountaining at night time
Kīlauea Volcano — Lava Fountaining (Fissure 8)
Kīlauea Volcano — Lava Fountaining (Fissure 8)
Kīlauea Volcano — Lava Fountaining (Fissure 8)

Around 3:00 a.m. HST today (June 8), lava fountains erupting from fissure 8 on Kīlauea Volcano's Lower East Rift Zone were reaching heights of 180–220 feet.

Around 3:00 a.m. HST today (June 8), lava fountains erupting from fissure 8 on Kīlauea Volcano's Lower East Rift Zone were reaching heights of 180–220 feet.

Outgassing rising from the summit
Kīlauea Volcano — Summit Outgassing
Kīlauea Volcano — Summit Outgassing
Kīlauea Volcano — Summit Outgassing

Outgassing from Halema‘uma‘u produced twin pillars that rose in the still morning air and merged into a towering cap above the summit of Kīlauea just after sunrise.

Outgassing from Halema‘uma‘u produced twin pillars that rose in the still morning air and merged into a towering cap above the summit of Kīlauea just after sunrise.

Plume coming from a crater
Kīlauea Volcano — Summit Pluming
Kīlauea Volcano — Summit Pluming
Kīlauea Volcano — Summit Pluming

Dramatic changes at Halema‘uma‘u could be seen through gases rising from the crater during HVO's overflight of the summit this morning at 10 a.m. HST. The view here looks to the southwest, with the former overlook parking lot barely visible to the left of the gas plume.

Dramatic changes at Halema‘uma‘u could be seen through gases rising from the crater during HVO's overflight of the summit this morning at 10 a.m. HST. The view here looks to the southwest, with the former overlook parking lot barely visible to the left of the gas plume.

Measuring streamflow in Belle Fource River below Hulett, WY
Measuring streamflow in Belle Fource River below Hulett, WY
Measuring streamflow in Belle Fource River below Hulett, WY
Measuring streamflow in Belle Fource River below Hulett, WY

Measuring streamflow in Belle Fource River below Hulett, WY

Chuck Worley (USGS) monitoring the real-time sonar data aboard the R/V Petrel during the geophysical survey in May 2018.
Monitoring real-time sonar data
Monitoring real-time sonar data
Monitoring real-time sonar data

Chuck Worley (USGS) monitoring the real-time sonar data aboard the R/V Petrel during the geophysical survey in May 2018.

Chuck Worley (USGS) monitoring the real-time sonar data aboard the R/V Petrel during the geophysical survey in May 2018.

Water Sampling Locations Rapid Creek and Canyon Lake
Water Sampling Locations Rapid Creek and Canyon Lake
Water Sampling Locations Rapid Creek and Canyon Lake
Water Sampling Locations Rapid Creek and Canyon Lake

Water-quality sampling locations on Rapid Creek and Canyon Lake in Rapid City, SD.

Water-quality sampling locations on Rapid Creek and Canyon Lake in Rapid City, SD.

Another explosion at the summit of Kīlauea...
Another explosion at the summit of Kīlauea
Another explosion at the summit of Kīlauea
Another explosion at the summit of Kīlauea

On June 6, at 4:07 p.m. HST, an explosion within Halema‘uma‘u sent an ash and gas plume to a height of about 10,000 feet above sea level. The explosion released energy equivalent to that of a magnitude-5.6 earthquake; a result of the explosion-related energy release was ground shaking felt throughout the summit area.

On June 6, at 4:07 p.m. HST, an explosion within Halema‘uma‘u sent an ash and gas plume to a height of about 10,000 feet above sea level. The explosion released energy equivalent to that of a magnitude-5.6 earthquake; a result of the explosion-related energy release was ground shaking felt throughout the summit area.

Large rocks on the roadway
Kīlauea Volcano — Ballistic Blocks
Kīlauea Volcano — Ballistic Blocks
Kīlauea Volcano — Ballistic Blocks

With careful consideration and planning to avoid ongoing volcanic hazards as much as possible, an HVO scientist who has been studying the behavior of Kīlauea's summit for decades, briefly visited the parking area for the former Halema‘uma‘u overlook (closed since 2008) on June 5 to make direct observations of and gather data from the effects of recent explosions wit

With careful consideration and planning to avoid ongoing volcanic hazards as much as possible, an HVO scientist who has been studying the behavior of Kīlauea's summit for decades, briefly visited the parking area for the former Halema‘uma‘u overlook (closed since 2008) on June 5 to make direct observations of and gather data from the effects of recent explosions wit

crack in parking lot
Kīlauea Volcano — Crack in Parking Lot
Kīlauea Volcano — Crack in Parking Lot
Kīlauea Volcano — Crack in Parking Lot

The median between two areas of the parking lot has been warped and broken by cracks. Ash accumulation in the parking area was generally not more than 4 cm (1.5 in) thick.

The median between two areas of the parking lot has been warped and broken by cracks. Ash accumulation in the parking area was generally not more than 4 cm (1.5 in) thick.

Crack in the road
Kīlauea Volcano — Crack on Crater Rim Drive
Kīlauea Volcano — Crack on Crater Rim Drive
Kīlauea Volcano — Crack on Crater Rim Drive

Crack on Crater Rim Drive just east of the parking lot, with the National Park sign indicating "Halema‘uma‘u" at right. This crack shows 42 cm (16.5 in) of right lateral offset—as measured by fitting the center stripe on the road back together)—and was about 25 cm (10 in) wide.

Crack on Crater Rim Drive just east of the parking lot, with the National Park sign indicating "Halema‘uma‘u" at right. This crack shows 42 cm (16.5 in) of right lateral offset—as measured by fitting the center stripe on the road back together)—and was about 25 cm (10 in) wide.

Crack in road
Kīlauea Volcano — Halema`uma`u Parking Lot
Kīlauea Volcano — Halema`uma`u Parking Lot
Kīlauea Volcano — Halema`uma`u Parking Lot

The Halema‘uma‘u parking lot is sliced into blocks by cracks. These cracks, first noted in a very early stage on May 13, now are the dominant features of the parking lot. The cracks, which are circumferential to Halema‘uma‘u, warp and offset the pavement and curbing, as seen here. The crack responsible for warping this curbstone is visible on both sides of it.

The Halema‘uma‘u parking lot is sliced into blocks by cracks. These cracks, first noted in a very early stage on May 13, now are the dominant features of the parking lot. The cracks, which are circumferential to Halema‘uma‘u, warp and offset the pavement and curbing, as seen here. The crack responsible for warping this curbstone is visible on both sides of it.

Crack in the ground
Kīlauea Volcano — Large Crack in Parking Lot
Kīlauea Volcano — Large Crack in Parking Lot
Kīlauea Volcano — Large Crack in Parking Lot

An even larger crack, shown here, arcs across the parking lot and bounds one of the large blocks mentioned above.

An even larger crack, shown here, arcs across the parking lot and bounds one of the large blocks mentioned above.

Large rocks on the parking lot
Kīlauea Volcano — Large Rocks on Parking Lot
Kīlauea Volcano — Large Rocks on Parking Lot
Kīlauea Volcano — Large Rocks on Parking Lot

Many large blocks appeared to be in depressions in the ash, but upon closer examination, it was concluded that wind had winnowed ash from around the blocks, creating a false impression that the depressions were made by impact.

Many large blocks appeared to be in depressions in the ash, but upon closer examination, it was concluded that wind had winnowed ash from around the blocks, creating a false impression that the depressions were made by impact.

Lava fountaining with lava flow
Kīlauea Volcano — Lava Fountain (Fissure 8)
Kīlauea Volcano — Lava Fountain (Fissure 8)
Kīlauea Volcano — Lava Fountain (Fissure 8)

 Fissure 8 lava fountain heights fluctuated between about 40 m (130 ft) and 70 m (230 ft) during this morning's overflight at about 6:30 a.m. HST.

 Fissure 8 lava fountain heights fluctuated between about 40 m (130 ft) and 70 m (230 ft) during this morning's overflight at about 6:30 a.m. HST.

lava fountain with lava flow
Kīlauea Volcano — Lava Fountain and Flow (Fissure 8)
Kīlauea Volcano — Lava Fountain and Flow (Fissure 8)
Kīlauea Volcano — Lava Fountain and Flow (Fissure 8)

View of the fissure 8 lava fountain and lava channel that travels to the ocean, a distance of about 12.5 km (7.8 mi). Photo taken during this morning's overflight at about 6:30 a.m. HST.

View of the fissure 8 lava fountain and lava channel that travels to the ocean, a distance of about 12.5 km (7.8 mi). Photo taken during this morning's overflight at about 6:30 a.m. HST.

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