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Map of flow field...
Map of flow field
Map of flow field
Map of flow field

This map shows recent changes to Kīlauea's East Rift Zone lava flow field. The area of the active flow field as of February 16 is shown in pink, while widening and advancement of the active flow as of February 24 is shown in red. Older Pu‘u ‘Ō‘ō lava flows (1983-2016) are shown in gray.

This map shows recent changes to Kīlauea's East Rift Zone lava flow field. The area of the active flow field as of February 16 is shown in pink, while widening and advancement of the active flow as of February 24 is shown in red. Older Pu‘u ‘Ō‘ō lava flows (1983-2016) are shown in gray.

Remotely measuring the temperature of Kīlauea lava...
Remotely measuring the temperature of Kīlauea lava
Remotely measuring the temperature of Kīlauea lava
Remotely measuring the temperature of Kīlauea lava

A U.S. Geological Survey scientist used a custom-built, high-speed camera to remotely measure the temperature of spattering lava on the surface of Kīlauea Volcano's summit lava lake (background). This particular experiment, conducted from the Jaggar Museum overlook in Hawai‘i Volcanoes National Park on December 10, 2016, was part of a NASA-funded research project.

A U.S. Geological Survey scientist used a custom-built, high-speed camera to remotely measure the temperature of spattering lava on the surface of Kīlauea Volcano's summit lava lake (background). This particular experiment, conducted from the Jaggar Museum overlook in Hawai‘i Volcanoes National Park on December 10, 2016, was part of a NASA-funded research project.

A hillside showing landslides with debris from one landslide impacting a house at the bottom of the slope.
Rainfall and Landslides in Northern CA
Rainfall and Landslides in Northern CA
Rainfall and Landslides in Northern CA

Shallow landslides damaged homes and closed many roads in the San Francisco East Bay region as a result of storms in January and February, 2017.

Shallow landslides damaged homes and closed many roads in the San Francisco East Bay region as a result of storms in January and February, 2017.

61g coastal lava flow remains active...
61g coastal lava flow remains active
61g coastal lava flow remains active
61g coastal lava flow remains active

Today (February 22, 2017), the breakout along the eastern edge of Kīlauea Volcano's episode 61g flow remains active and had advanced approximately 570 m (620 yards) since it was last mapped on February 14.

Today (February 22, 2017), the breakout along the eastern edge of Kīlauea Volcano's episode 61g flow remains active and had advanced approximately 570 m (620 yards) since it was last mapped on February 14.

Aerial photo of snow-covered mountaIns with umbrella-shaped volcanic ash plume rising in the background
Bogoslof volcano eruption plume
Bogoslof volcano eruption plume
Bogoslof volcano eruption plume

February 19 Bogoslof eruption plume as seen from Unalaska Island, 53 miles ESE of Bogoslof volcano. Photo taken from helicopter during fieldwork by AVO geologists at 5:22PM, approximately 14 minutes after the start of the eruption.

February 19 Bogoslof eruption plume as seen from Unalaska Island, 53 miles ESE of Bogoslof volcano. Photo taken from helicopter during fieldwork by AVO geologists at 5:22PM, approximately 14 minutes after the start of the eruption.

Map of flow field...
Map of flow field
Map of flow field
Map of flow field

This map shows recent changes to Kīlauea's East Rift Zone lava flow field. The area of the active flow field as of January 12 is shown in pink, while widening and advancement of the active flow as of February 16 is shown in red. Older Pu‘u ‘Ō‘ō lava flows (1983-2016) are shown in gray.

This map shows recent changes to Kīlauea's East Rift Zone lava flow field. The area of the active flow field as of January 12 is shown in pink, while widening and advancement of the active flow as of February 16 is shown in red. Older Pu‘u ‘Ō‘ō lava flows (1983-2016) are shown in gray.

NASA practices for Mars exploration on Kīlauea Volcano...
NASA practices for Mars exploration on Kīlauea
NASA practices for Mars exploration on Kīlauea
NASA practices for Mars exploration on Kīlauea

Left: Astronauts James A. Lovell, Jr., and Fred W. Haise, Jr., members of NASA's third team of moon explorers, carried cameras, communications equipment, and an Apollo Lunar Hand Tools scoop during a simulation of a lunar traverse at Kīlauea Volcano in December 1969.

Left: Astronauts James A. Lovell, Jr., and Fred W. Haise, Jr., members of NASA's third team of moon explorers, carried cameras, communications equipment, and an Apollo Lunar Hand Tools scoop during a simulation of a lunar traverse at Kīlauea Volcano in December 1969.

Map Kīlauea's active East Rift Zone lava flow field in relation to ...
Map Kīlauea's active ERZ lava flow field in relation to SEern part ...
Map Kīlauea's active ERZ lava flow field in relation to SEern part ...
Map Kīlauea's active ERZ lava flow field in relation to SEern part ...

This small-scale map shows Kīlauea's active East Rift Zone lava flow field in relation to the southeastern part of the Island of Hawai?i. The area of the active flow field as of January 12 is shown in pink, while widening and advancement of the active flow as of February 16 is shown in red. Older Pu‘u ‘Ō‘ō lava flows (1983-2016) are shown in gray.

This small-scale map shows Kīlauea's active East Rift Zone lava flow field in relation to the southeastern part of the Island of Hawai?i. The area of the active flow field as of January 12 is shown in pink, while widening and advancement of the active flow as of February 16 is shown in red. Older Pu‘u ‘Ō‘ō lava flows (1983-2016) are shown in gray.

An FTIR instrument is set up on the rim of Halema‘uma‘u Crater to m...
An FTIR instrument is set up on the rim of Halema‘uma‘u to measure ...
An FTIR instrument is set up on the rim of Halema‘uma‘u to measure ...
An FTIR instrument is set up on the rim of Halema‘uma‘u to measure ...

An FTIR instrument is set up on the rim of Halema‘uma‘u Crater to measure volcanic gases from the summit lava lake. The open-path Fourier transform infrared (FTIR) spectrometer continuously measures the gases in a volcanic plume, measuring the relative abundance of each.

An FTIR instrument is set up on the rim of Halema‘uma‘u Crater to measure volcanic gases from the summit lava lake. The open-path Fourier transform infrared (FTIR) spectrometer continuously measures the gases in a volcanic plume, measuring the relative abundance of each.

A telephoto view of the east lake margin showed that the spattering...
A telephoto view of the east lake margin showed that the spattering...
A telephoto view of the east lake margin showed that the spattering...
A telephoto view of the east lake margin showed that the spattering...

A telephoto view of the east lake margin showed that the spattering was focused in small embayments created by promontories of cooled, congealed lava jutting from the vent wall.

At times, spattering along the east lake margin reached heights of ...
At times, spattering along the east lake margin reached heights of ...
At times, spattering along the east lake margin reached heights of ...
At times, spattering along the east lake margin reached heights of ...

At times, spattering along the east lake margin reached heights of 6-9 m (20-30 ft), as shown in this telephoto image.

View of the lava lake within Halema‘uma‘u Crater from the FTIR spec...
View of the lava lake within Halema‘uma‘u from the FTIR spectromete...
View of the lava lake within Halema‘uma‘u from the FTIR spectromete...
View of the lava lake within Halema‘uma‘u from the FTIR spectromete...

View of the lava lake within Halema‘uma‘u Crater from the FTIR spectrometer monitoring location. At Hawaiian volcanoes, magma ascends from the mantle more than 60 km (about 40 mi) below the surface, to a reservoir less than 2 km (about 1.2 mi) deep. As the pressure decreases, the gases dissolved in the magma bubble out and escape.

View of the lava lake within Halema‘uma‘u Crater from the FTIR spectrometer monitoring location. At Hawaiian volcanoes, magma ascends from the mantle more than 60 km (about 40 mi) below the surface, to a reservoir less than 2 km (about 1.2 mi) deep. As the pressure decreases, the gases dissolved in the magma bubble out and escape.

USGS Hawaiian Volcano Observatory office building is located on the...
USGS HVO office building is located on the rim of Kīlauea Caldera i...
USGS HVO office building is located on the rim of Kīlauea Caldera i...
image related to volcanoes. See description
At the coast, the lava flow in the Ahalanui area remains less than 0.1 miles fro
At the coast, the lava flow in the Ahalanui area remains less than 0.1 miles fro
At the coast, the lava flow in the Ahalanui area remains less than 0.1 miles fro

At the coast, the lava flow in the Ahalanui area remains less than 0.1 miles from the Pohoiki boat ramp (left of center in this photo) in Isaac Hale Park. The active ocean entry is a few hundred yards east (right) of this photograph.

At the coast, the lava flow in the Ahalanui area remains less than 0.1 miles from the Pohoiki boat ramp (left of center in this photo) in Isaac Hale Park. The active ocean entry is a few hundred yards east (right) of this photograph.

A Valentine's Day view of Kīlauea Volcano's summit lava lake...
A Valentine's Day view of Kīlauea's summit lava lake
A Valentine's Day view of Kīlauea's summit lava lake
A Valentine's Day view of Kīlauea's summit lava lake

Today, Kīlauea Volcano's summit lava lake level was 21 m (69 ft) below the vent rim. A long stretch of active spattering was visible along the east lake margin from the rim of Halema‘uma‘u Crater, an area that remains closed to the public due to ongoing hazards. The usual spatter source to the southeast was small by comparison.

Today, Kīlauea Volcano's summit lava lake level was 21 m (69 ft) below the vent rim. A long stretch of active spattering was visible along the east lake margin from the rim of Halema‘uma‘u Crater, an area that remains closed to the public due to ongoing hazards. The usual spatter source to the southeast was small by comparison.

High-tech instruments track volcanic gases at Kīlauea Volcano...
High-tech instruments track volcanic gases at Kīlauea
High-tech instruments track volcanic gases at Kīlauea
High-tech instruments track volcanic gases at Kīlauea

HVO's geochemist uses a Fourier Transform Infrared Spectrometer (FTIR) instrument to track volcanic gases emitted from the lava lake with Halema‘uma‘u Crater. These measurements help detect changes in gas composition, which can provide insight into the inner workings of Kīlauea Volcano.

HVO's geochemist uses a Fourier Transform Infrared Spectrometer (FTIR) instrument to track volcanic gases emitted from the lava lake with Halema‘uma‘u Crater. These measurements help detect changes in gas composition, which can provide insight into the inner workings of Kīlauea Volcano.

61g flow coastal breakout still active...
61g flow coastal breakout still active
61g flow coastal breakout still active
61g flow coastal breakout still active

The 61g flow breakout that started on February 10 on Pulama Pali was still active today. The flow front (shown here) is approximately 2.3 km (1.4 mi) from the base of the pali and 1.2 km (0.75 mi) from the ocean. The flow front is on the eastern side of the 61g flow field, and is outside the National Park boundary.

The 61g flow breakout that started on February 10 on Pulama Pali was still active today. The flow front (shown here) is approximately 2.3 km (1.4 mi) from the base of the pali and 1.2 km (0.75 mi) from the ocean. The flow front is on the eastern side of the 61g flow field, and is outside the National Park boundary.

USGS Hawaiian Volcano Observatory is located in Hawai‘i Volcanoes N...
USGS HVO is located in Hawai‘i Volcanoes National Park adjacent to ...
USGS HVO is located in Hawai‘i Volcanoes National Park adjacent to ...
USGS HVO is located in Hawai‘i Volcanoes National Park adjacent to ...

USGS Hawaiian Volcano Observatory is located in Hawai‘i Volcanoes National Park adjacent to Jaggar Museum.

High-flying NASA aircraft instruments simulate future satellite ima...
NASA aircraft instruments simulate future images over Hawaii volcanoes
NASA aircraft instruments simulate future images over Hawaii volcanoes
NASA aircraft instruments simulate future images over Hawaii volcanoes

NASA ER-2 aircrafts have played an important role in Earth science research because of their ability to fly into the lower stratosphere at subsonic speeds, enabling virtual satellite simulation missions.

NASA ER-2 aircrafts have played an important role in Earth science research because of their ability to fly into the lower stratosphere at subsonic speeds, enabling virtual satellite simulation missions.

Photo of the upper portion of the "firehose" taken with a telephoto...
Photo of the upper portion of the "firehose" taken with a telephoto...
Photo of the upper portion of the "firehose" taken with a telephoto...
Photo of the upper portion of the "firehose" taken with a telephoto...

Photo of the upper portion of the "firehose" taken with a telephoto lens as the lava exits the 61g flow lava tube. There is no sign of a lava delta rebuilding as the lava continues to spill into the ocean.

Photo of the upper portion of the "firehose" taken with a telephoto lens as the lava exits the 61g flow lava tube. There is no sign of a lava delta rebuilding as the lava continues to spill into the ocean.

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