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Fishing Cone, West Thumb
Fishing Cone, West Thumb
Fishing Cone, West Thumb
Fishing Cone, West Thumb

Fishing cone, a hot springs on the floor of Yellowstone Lake. The hot spring rim sits at lake level.

Fishing cone, a hot springs on the floor of Yellowstone Lake. The hot spring rim sits at lake level.

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GPS station P361, on Sawtell Peak
GPS station P361, on Sawtell Peak
GPS station P361, on Sawtell Peak

GPS station P361, on Sawtell Peak, on a nice clear day. Electrical storms destroyed multiple antennas, including the GPS antenna--here under a protective plastic dome--and three communications antennas on the tower. Data from P361, along with data from other stations in the Yellowstone region, are sent to UNAVCO for free and open distribution.

GPS station P361, on Sawtell Peak, on a nice clear day. Electrical storms destroyed multiple antennas, including the GPS antenna--here under a protective plastic dome--and three communications antennas on the tower. Data from P361, along with data from other stations in the Yellowstone region, are sent to UNAVCO for free and open distribution.

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Mount Baker and Glacier Peak - Active Volcanoes
Mount Baker and Glacier Peak - Active Volcanoes
Mount Baker and Glacier Peak - Active Volcanoes

Are you ready for an eruption? Mount Baker dominates the skyline of northwestern Washington and southwestern British Columbia. Glacier Peak is mostly hidden from view. Both volcanoes have erupted in recent centuries and will erupt again, disrupting the landscape and the lives of people downstream and downwind. Learn what to do and where to get information.

Are you ready for an eruption? Mount Baker dominates the skyline of northwestern Washington and southwestern British Columbia. Glacier Peak is mostly hidden from view. Both volcanoes have erupted in recent centuries and will erupt again, disrupting the landscape and the lives of people downstream and downwind. Learn what to do and where to get information.

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Mount Rainier is an active volcano. Are you Ready for an Eruption?
Mount Rainier is an active volcano. Are you Ready for an Eruption?
Mount Rainier is an active volcano. Are you Ready for an Eruption?

Mount Rainier is much more than a mountain in the sky. Constructed of hundreds of lava flows, and capped by as much glacier ice as all other Cascade volcanoes combined, Rainier's steep rubbly slopes and abundant water make it prone to landslides and lahars, especially during eruptions. Are you ready for an eruption?

Mount Rainier is much more than a mountain in the sky. Constructed of hundreds of lava flows, and capped by as much glacier ice as all other Cascade volcanoes combined, Rainier's steep rubbly slopes and abundant water make it prone to landslides and lahars, especially during eruptions. Are you ready for an eruption?

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UNAVCO field engineer Dylan Cembalski replaces damaged antennas on the communica
UNAVCO field engineer Dylan Cembalski replaces damaged antennas on the communica
UNAVCO field engineer Dylan Cembalski replaces damaged antennas on the communica

UNAVCO field engineer Dylan Cembalski replaces damaged antennas on the communications tower at Sawtell Peak. The tower is shared by multiple groups that use this regional high point to relay data. (UNAVCO Photo by Summer Rhoades)

UNAVCO field engineer Dylan Cembalski replaces damaged antennas on the communications tower at Sawtell Peak. The tower is shared by multiple groups that use this regional high point to relay data. (UNAVCO Photo by Summer Rhoades)

Hot, molten lava flows slowly into the ocean, and the temperature difference between lava and water is creating steam.
Viscous lava hits ocean water
Viscous lava hits ocean water
Viscous lava hits ocean water

A viscous pāhoehoe flow from Kilauea Volcano, Hawaiʻi , entering the ocean near Isaac Hale Beach Park on the morning of August 5, 2018.

A viscous pāhoehoe flow from Kilauea Volcano, Hawaiʻi , entering the ocean near Isaac Hale Beach Park on the morning of August 5, 2018.

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Volcano collapses mark the beginning and end of USGS scientist's career
Volcano collapses mark the beginning and end of USGS scientist's career
Volcano collapses mark the beginning and end of USGS scientist's career

Left: Horseshoe-shaped crater of Mount St. Helens in 1980, formed by a landslide that removed the top of the volcano. The crater is about 2 km (1.2 mi) wide and the floor is about 600 m (1,970 ft) below the crater rim. Right: Halema'uma'u nestled in the summit crater of Kīlauea Volcano on August 1, the day before the last collapse event.

Left: Horseshoe-shaped crater of Mount St. Helens in 1980, formed by a landslide that removed the top of the volcano. The crater is about 2 km (1.2 mi) wide and the floor is about 600 m (1,970 ft) below the crater rim. Right: Halema'uma'u nestled in the summit crater of Kīlauea Volcano on August 1, the day before the last collapse event.

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Before and after satellite images of Leilani Estates subdivision
Before and after satellite images of Leilani Estates subdivision
Before and after satellite images of Leilani Estates subdivision

This comparison shows satellite images of Leilani Estates subdivision before and after the May-August 2018 eruption. The image on the right, collected in early September 2018, shows that the eastern portion of the subdivision has been covered by lava. The Fissure 8 lava channel runs northeast, with the Fissure 8 cone at the start of the channel.

This comparison shows satellite images of Leilani Estates subdivision before and after the May-August 2018 eruption. The image on the right, collected in early September 2018, shows that the eastern portion of the subdivision has been covered by lava. The Fissure 8 lava channel runs northeast, with the Fissure 8 cone at the start of the channel.

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Before and after satellite images of the Fissure 8 area in Leilani Estates
Before and after satellite images of the Fissure 8 area in Leilani Estates
Before and after satellite images of the Fissure 8 area in Leilani Estates

A close up comparison of the Fissure 8 area in Leilani Estates subdivision. Leilani Avenue runs right-left (east-west) through the center of the images. On the right side, the crater in the Fissure 8 cone is visible, with the Fissure 8 lava channel extending north.

A close up comparison of the Fissure 8 area in Leilani Estates subdivision. Leilani Avenue runs right-left (east-west) through the center of the images. On the right side, the crater in the Fissure 8 cone is visible, with the Fissure 8 lava channel extending north.

A man controlling a computer mouse is sitting at a computer looking at a computer monitor.
Multibeam processing
Multibeam processing
Multibeam processing

USGS scientist Pete Dartnell processes multibeam data collected from off the Pacific Northwest coast on a research cruise aboard NOAA ship Rainier.

USGS scientist Pete Dartnell processes multibeam data collected from off the Pacific Northwest coast on a research cruise aboard NOAA ship Rainier.

Photo of Ground stratification showing different types of Geomorphology
New Jersey Strata 1
New Jersey Strata 1
New Jersey Strata 1

 Exposure of the Cape May Formation in the Kirkwood-Cohansey aquifer system. 

 Exposure of the Cape May Formation in the Kirkwood-Cohansey aquifer system. 

Photo of Ground stratification showing different types of Geomorphology
New Jersey Strata 2
New Jersey Strata 2
New Jersey Strata 2

Exposure of the clay-sand facies of the Cohansey Formation in the Kirkwood-Cohansey aquifer system.

Exposure of the clay-sand facies of the Cohansey Formation in the Kirkwood-Cohansey aquifer system.

Sensor data logger recovered from floor of Yellowstone Lake
Sensor data logger recovered from floor of Yellowstone Lake
Sensor data logger recovered from floor of Yellowstone Lake
Sensor data logger recovered from floor of Yellowstone Lake

A sensor data logger recovered from the floor of Yellowstone Lake in the Deep Hole area in 2018 shows signs of melting due to unexpectedly high temperatures in sediments up to ~3 ft (1 m) away from an active hydrothermal vent. Image acquired by the Global Foundation for Ocean Exploration ROV Yogi on August 4, 2018.

A sensor data logger recovered from the floor of Yellowstone Lake in the Deep Hole area in 2018 shows signs of melting due to unexpectedly high temperatures in sediments up to ~3 ft (1 m) away from an active hydrothermal vent. Image acquired by the Global Foundation for Ocean Exploration ROV Yogi on August 4, 2018.

Sensor deployed in the Deep Hole, Yellowstone Lake floor
Sensor deployed in the Deep Hole, Yellowstone Lake floor
Sensor deployed in the Deep Hole, Yellowstone Lake floor
Sensor deployed in the Deep Hole, Yellowstone Lake floor

Sensor deployed in the Deep Hole, east of Stevenson Island to monitor long-term temperature and chemical variations in an active vent. Image acquired by the Global Foundation for Ocean Exploration ROV Yogi on August 4, 2018.

Sensor deployed in the Deep Hole, east of Stevenson Island to monitor long-term temperature and chemical variations in an active vent. Image acquired by the Global Foundation for Ocean Exploration ROV Yogi on August 4, 2018.

Thermally-deformed sensor recovered from the floor of Yellowstone Lake
Thermally-deformed sensor recovered from the floor of Yellowstone Lake
Thermally-deformed sensor recovered from the floor of Yellowstone Lake
Thermally-deformed sensor recovered from the floor of Yellowstone Lake

Sensor (top), deformed battery/electronics package (bottom), and titanium sheath (left) following recovery from vent location A in teh Deep Hole area on the floor of Yellowstone Lake.

color photograph of volcanic lava channel
Lava in the fissure 8 channel spillway
Lava in the fissure 8 channel spillway
Lava in the fissure 8 channel spillway

Lava in the fissure 8 channel spillway was fairly low this morning, with the lava in the channel moving at a fairly low velocity.

Pāhoehoe Breakout
Pāhoehoe Breakout
Pāhoehoe Breakout

This lava, erupted from fissure 8 on Kīlauea Volcano's lower East Rift Zone, shows classic pāhoehoe behavior. Exposed to the air, the surface of the flow chills to form a thin crust that can be stretched or broken apart, forming pieces of crust that are "subducted" back into the molten interior.

This lava, erupted from fissure 8 on Kīlauea Volcano's lower East Rift Zone, shows classic pāhoehoe behavior. Exposed to the air, the surface of the flow chills to form a thin crust that can be stretched or broken apart, forming pieces of crust that are "subducted" back into the molten interior.

Color image of three scientists walking towards volcanic vent
USGS gas geochemist and colleagues at fissure 8
USGS gas geochemist and colleagues at fissure 8
USGS gas geochemist and colleagues at fissure 8

A USGS gas geochemist and colleagues from the United Kingdom carry multi-gas sensors as they approach the degassing fissure 8 cone during Kīlauea Volcano's 2018 eruption.

A USGS gas geochemist and colleagues from the United Kingdom carry multi-gas sensors as they approach the degassing fissure 8 cone during Kīlauea Volcano's 2018 eruption.

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