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How well do you know USGS volcano observatories? Part 1: Cascades...
How well do you know USGS volcano observatories? Part 1: Cascades
How well do you know USGS volcano observatories? Part 1: Cascades
How well do you know USGS volcano observatories? Part 1: Cascades

Mount St. Helens in December 2004, a few months after the start of the volcano's most recent eruption, as seen from the Johnston Ridge Observatory in Mount St. Helens National Volcanic Monument in Washington. Inset: The USGS Cascades Volcano Observatory in Vancouver, WA, monitors volcanoes in Washington, Oregon, and Idaho. USGS photos.

Mount St. Helens in December 2004, a few months after the start of the volcano's most recent eruption, as seen from the Johnston Ridge Observatory in Mount St. Helens National Volcanic Monument in Washington. Inset: The USGS Cascades Volcano Observatory in Vancouver, WA, monitors volcanoes in Washington, Oregon, and Idaho. USGS photos.

Ongoing activity at Kamokuna ocean entry...
Ongoing activity at Kamokuna ocean entry
Ongoing activity at Kamokuna ocean entry
Ongoing activity at Kamokuna ocean entry

Part of what's left of the eastern Kamokuna lava delta following the New Year's Eve collapse can be seen in the center foreground of this image. Visible cracks on the surface of this rocky shelf indicate potential instability and serve as reminders for visitors to the lava viewing area to heed all warning signs.

Part of what's left of the eastern Kamokuna lava delta following the New Year's Eve collapse can be seen in the center foreground of this image. Visible cracks on the surface of this rocky shelf indicate potential instability and serve as reminders for visitors to the lava viewing area to heed all warning signs.

A telephoto lens captured the cascade of lava streaming from the la...
A telephoto lens captured the cascade of lava streaming from the la...
A telephoto lens captured the cascade of lava streaming from the la...
A telephoto lens captured the cascade of lava streaming from the la...

A telephoto lens captured the cascade of lava streaming from the lava tube. Hot lava mixing with cool seawater produces an explosive interaction that results in fragmented lava—spatter, Pele's hair, and black sand—flying upward, landing on the sea cliff above the ocean entry and being thrown seaward.

A telephoto lens captured the cascade of lava streaming from the lava tube. Hot lava mixing with cool seawater produces an explosive interaction that results in fragmented lava—spatter, Pele's hair, and black sand—flying upward, landing on the sea cliff above the ocean entry and being thrown seaward.

A closer view of lava cascading from the lava tube at the Kamokuna ...
A closer view of lava cascading from the lava tube at the Kamokuna ...
A closer view of lava cascading from the lava tube at the Kamokuna ...
A closer view of lava cascading from the lava tube at the Kamokuna ...

A closer view of lava cascading from the lava tube at the Kamokuna ocean entry, with spatter (fragments of molten lava) and black sand (volcanic glass) being thrown skyward.

A closer view of lava cascading from the lava tube at the Kamokuna ocean entry, with spatter (fragments of molten lava) and black sand (volcanic glass) being thrown skyward.

A glove provides scale for spatter (lighter gray, shiny fragments) ...
A glove provides scale for spatter (lighter gray, shiny fragments) ...
A glove provides scale for spatter (lighter gray, shiny fragments) ...
A glove provides scale for spatter (lighter gray, shiny fragments) ...

A glove provides scale for spatter (lighter gray, shiny fragments) that landed on the sea cliff above the Kamokuna ocean entry.

A glove provides scale for spatter (lighter gray, shiny fragments) that landed on the sea cliff above the Kamokuna ocean entry.

Pele's hair, filaments of volcanic glass, formed from the explosive...
Pele's hair, filaments of volcanic glass, formed from the explosive...
Pele's hair, filaments of volcanic glass, formed from the explosive...
Pele's hair, filaments of volcanic glass, formed from the explosive...

Pele's hair, filaments of volcanic glass, formed from the explosive interaction of hot lava entering the ocean, accumulates on the lava surface above the ocean entry. Some is also blown far downwind of the ocean entry.

Pele's hair, filaments of volcanic glass, formed from the explosive interaction of hot lava entering the ocean, accumulates on the lava surface above the ocean entry. Some is also blown far downwind of the ocean entry.

Updated Kamokuna ocean entry map...
Updated Kamokuna ocean entry map
Updated Kamokuna ocean entry map
Updated Kamokuna ocean entry map

This map updates the preliminary ocean entry map below, based on mapping conducted on January 3, 2017. The map of the coastline at the lava flow ocean entry at Kamokuna shows the areas of the lava delta and adjacent coastline that collapsed into the ocean on December 31, 2016.

This map updates the preliminary ocean entry map below, based on mapping conducted on January 3, 2017. The map of the coastline at the lava flow ocean entry at Kamokuna shows the areas of the lava delta and adjacent coastline that collapsed into the ocean on December 31, 2016.

Kamokuna lava delta collapse also takes part of old sea cliff...
Kamokuna lava delta collapse also takes part of old sea cliff
Kamokuna lava delta collapse also takes part of old sea cliff
Kamokuna lava delta collapse also takes part of old sea cliff

The rocky shelf at the base of the sea cliff is all that remains of the Kamokuna lava delta following the New Year's Eve collapse (Dec. 31, 2016), which sent acres of rock plunging into the sea.

The rocky shelf at the base of the sea cliff is all that remains of the Kamokuna lava delta following the New Year's Eve collapse (Dec. 31, 2016), which sent acres of rock plunging into the sea.

In addition to most of the Kamokuna lava delta disappearing into th...
In addition to most of the Kamokuna lava delta disappearing into oc...
In addition to most of the Kamokuna lava delta disappearing into oc...
In addition to most of the Kamokuna lava delta disappearing into oc...

In addition to most of the Kamokuna lava delta disappearing into the ocean on New Year's Eve day, a large section of the older sea cliff east of the delta also collapsed. Here you can see the "bite" taken out by the collapse of the sea cliff.

In addition to most of the Kamokuna lava delta disappearing into the ocean on New Year's Eve day, a large section of the older sea cliff east of the delta also collapsed. Here you can see the "bite" taken out by the collapse of the sea cliff.

Kamokuna ocean entry map...
Kamokuna ocean entry map
Kamokuna ocean entry map
Kamokuna ocean entry map

This map shows the coastline at the Kamokuna lava entry on Kīlauea Volcano, with labels denoting areas impacted by the large, progressive lava-delta collapse on December 31, 2016. Nearly all the Kamokuna lava delta collapsed into the sea, along with a large section of the older sea cliff east of the delta.

This map shows the coastline at the Kamokuna lava entry on Kīlauea Volcano, with labels denoting areas impacted by the large, progressive lava-delta collapse on December 31, 2016. Nearly all the Kamokuna lava delta collapsed into the sea, along with a large section of the older sea cliff east of the delta.

image related to volcanoes. See description
Many forms of sulfur are found on Kīlauea Volcano
Many forms of sulfur are found on Kīlauea Volcano
Many forms of sulfur are found on Kīlauea Volcano

Continued degassing from fumaroles at fissures on Kīlauea Volcano's lower East Rift Zone produce native sulfur crystals when sulfur dioxide and hydrogen sulfide gases react and cool upon reaching the surface. The delicate sulfur crystals are 5–15 mm (0.2–0.6 in) long. USGS photos by A. Lerner, 2018.

Continued degassing from fumaroles at fissures on Kīlauea Volcano's lower East Rift Zone produce native sulfur crystals when sulfur dioxide and hydrogen sulfide gases react and cool upon reaching the surface. The delicate sulfur crystals are 5–15 mm (0.2–0.6 in) long. USGS photos by A. Lerner, 2018.

image related to volcanoes. See description
White laze plumes mark locations where lava enters the ocean over a broad area.
White laze plumes mark locations where lava enters the ocean over a broad area.
White laze plumes mark locations where lava enters the ocean over a broad area.

White laze plumes mark locations where lava enters the ocean over a broad area. An open lava channel flows into the ocean at the southern-most plume (middle) near the southern flow margin. The boat ramp at Pohoiki is about 940 m (0.58 mi) farther south of the flow margin. View is toward the west-southwest.

White laze plumes mark locations where lava enters the ocean over a broad area. An open lava channel flows into the ocean at the southern-most plume (middle) near the southern flow margin. The boat ramp at Pohoiki is about 940 m (0.58 mi) farther south of the flow margin. View is toward the west-southwest.

banding of Panum pumice and obsidian
Flow banding of Panum pumice and obsidian
Flow banding of Panum pumice and obsidian
Flow banding of Panum pumice and obsidian

Flow banding of Panum pumice and obsidian of the same composition.

Girls points to a location on a map laying on the ground.
GeoGirls learn about the eruption of Mount St. Helens
GeoGirls learn about the eruption of Mount St. Helens
GeoGirls learn about the eruption of Mount St. Helens

GeoGirls learn about how the May 18, 1980 eruption of Mount St. Helens impacted the ecology of the area.

Group of students and scientists stand in semi circle with mountain in the background.
GeoGirls hike onto the Pumice Plain and learn about Mount St. Helens
GeoGirls hike onto the Pumice Plain and learn about Mount St. Helens
GeoGirls hike onto the Pumice Plain and learn about Mount St. Helens

GeoGirls hike onto the Pumice Plain to learn more about Mount St. Helens’ historical

eruptions.

Digital Elevation Model for Newberry Volcano and vicinity....
Digital Elevation Model for Newberry Volcano and vicinity.
Digital Elevation Model for Newberry Volcano and vicinity.
Digital Elevation Model for Newberry Volcano and vicinity.

High-resolution digital elevation dataset for Newberry Volcano and vicinity, Oregon, based on lidar survey of August-September, 2010 and bathymetric survey of June, 2001.

High-resolution digital elevation dataset for Newberry Volcano and vicinity, Oregon, based on lidar survey of August-September, 2010 and bathymetric survey of June, 2001.

Large euhedral shape (brown) in a fine-grained matrix of rectangles
Rock thin section: andesite
Rock thin section: andesite
Rock thin section: andesite

Photomicrograph of sample 09RDWES301 - an andesite collected during the Redoubt 2009 eruption. A rock thin section is created by gluing a small piece of rock onto a glass slide, then grinding it down to a thickness of 30 microns (the average human hair is about 100 microns in diameter) so that light shines through it when examined under the microscope.

Photomicrograph of sample 09RDWES301 - an andesite collected during the Redoubt 2009 eruption. A rock thin section is created by gluing a small piece of rock onto a glass slide, then grinding it down to a thickness of 30 microns (the average human hair is about 100 microns in diameter) so that light shines through it when examined under the microscope.

Photograph of eddy covariance and Multi-GAS stations
Eddy covariance and Multi-GAS stations
Eddy covariance and Multi-GAS stations
Eddy covariance and Multi-GAS stations

Photograph of eddy covariance and Multi-GAS stations that were deployed in a temporary configuration near Norris Geyser Basin in 2016. Research conducted under permit YELL-2016-SCI-7082.

Photograph of eddy covariance and Multi-GAS stations that were deployed in a temporary configuration near Norris Geyser Basin in 2016. Research conducted under permit YELL-2016-SCI-7082.

Allan Lerner
Allan Lerner
Allan Lerner
Allan Lerner

Allan Lerner works in the USGS volcanic gas geochemistry group. The photo was taken in the crater of Mount St. Helens, with Spirit Lake and Mount Rainier in the distance. USGS photo by P. Kelly.

Allan Lerner works in the USGS volcanic gas geochemistry group. The photo was taken in the crater of Mount St. Helens, with Spirit Lake and Mount Rainier in the distance. USGS photo by P. Kelly.

Kīlauea Volcano's East Rift Zone eruption: here's what happened in ...
Kīlauea's ERZ eruption: what happened in 2017
Kīlauea's ERZ eruption: what happened in 2017
Kīlauea's ERZ eruption: what happened in 2017

On May 24, 2016, two new flows broke out on the flanks of the Pu‘u ‘Ō‘ō cone on Kīlauea Volcano's East Rift Zone. The silvery sheen of new lava erupting from the northern 61f breakout (center) and eastern 61g breakout (upper left) stands out in contrast to the older flows on and around Pu‘u ‘Ō‘ō (right).

On May 24, 2016, two new flows broke out on the flanks of the Pu‘u ‘Ō‘ō cone on Kīlauea Volcano's East Rift Zone. The silvery sheen of new lava erupting from the northern 61f breakout (center) and eastern 61g breakout (upper left) stands out in contrast to the older flows on and around Pu‘u ‘Ō‘ō (right).

19th century virtual reality brings Hawaiian volcano to life...
19th century virtual reality brings Hawaiian volcano to life
19th century virtual reality brings Hawaiian volcano to life
19th century virtual reality brings Hawaiian volcano to life

This building housed the Kīlauea cyclorama at the Chicago World's Fair in1893. Positioned above the entrance to the cyclorama was a statue of Pele, the Hawaiian volcano goddess, standing on a lava flow and holding a flame. For more info, please see https://chicagology.com/columbiaexpo/fair052/.

This building housed the Kīlauea cyclorama at the Chicago World's Fair in1893. Positioned above the entrance to the cyclorama was a statue of Pele, the Hawaiian volcano goddess, standing on a lava flow and holding a flame. For more info, please see https://chicagology.com/columbiaexpo/fair052/.