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Volcano Hazard Program images.

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Deposit of the largest lahar from Mount Baker, Washington, exposed ...
Deposit of the largest lahar from Mount Baker, WA, exposed near con...
Deposit of the largest lahar from Mount Baker, WA, exposed near con...
Deposit of the largest lahar from Mount Baker, WA, exposed near con...

Note the protruding logs and branches from living trees that were knocked down and carried by the lahar. Ice axe, 3 ft, shows scale. Lahars are the greatest hazard at Mount Baker.

Timeline for eruptions at Mount Baker during the Holocene (12,000 y...
Timeline for eruptions at Mount Baker during Holocene
Timeline for eruptions at Mount Baker during Holocene
Airplane taking off with snow covered volcano in the background.
Mount Hood lies approximately 70 km (45 mi) from Portland International Airport. Volcanic Ash from eruptions can damage aircraft engines.
Mount Hood lies approximately 70 km (45 mi) from Portland International Airport. Volcanic Ash from eruptions can damage aircraft engines.
Graphic depicting the distribution of Yellowstone ash across the U....
Map of volcanic ash fall as a result of eruptions from Yellowstone,...
Map of volcanic ash fall as a result of eruptions from Yellowstone,...
Map of volcanic ash fall as a result of eruptions from Yellowstone,...

Map of volcanic ashfall. Areas of the United States that once were covered by volcanic ash from Yellowstone's giant eruptions 2 million and 630,000 years ago, compared with ashfall from the 760,000-year-old Long Valley caldera eruptions at Mammoth Lakes, California, and the 1980 eruption of Mount St. Helens, Washington.

Map of volcanic ashfall. Areas of the United States that once were covered by volcanic ash from Yellowstone's giant eruptions 2 million and 630,000 years ago, compared with ashfall from the 760,000-year-old Long Valley caldera eruptions at Mammoth Lakes, California, and the 1980 eruption of Mount St. Helens, Washington.

Craters of the Moon, Idaho, Landsat 7 true-color image viewed from ...
Craters of the Moon, Idaho, Landsat 7 true-color image viewed from ...
Craters of the Moon, Idaho, Landsat 7 true-color image viewed from ...
Craters of the Moon, Idaho, Landsat 7 true-color image viewed from ...

Craters of the Moon, Idaho, Landsat 7 true-color image viewed from the east. Pioneer Mountain Range along the western border. Image created by NASA EArth Observatory.

Cutaway views showing the internal structure of the Earth. Left: To...
Cutaway views showing the internal structure of the Earth. Left: To...
Cutaway views showing the internal structure of the Earth. Left: To...
Cutaway views showing the internal structure of the Earth. Left: To...

Cutaway views showing the internal structure of the Earth. Left: To scale drawing shows that Earth's crust is very thin. Right: Not to scale, more detail of three main layers (crust, mantle, core).

Cutaway views showing the internal structure of the Earth. Left: To scale drawing shows that Earth's crust is very thin. Right: Not to scale, more detail of three main layers (crust, mantle, core).

Image: Grímsvötn Caldera
Grímsvötn Caldera
Grímsvötn Caldera
Grímsvötn Caldera

Photograph from the southwestern wall of the Grímsvötn caldera in Vatnajökull on December, 19 1998.

 

Photograph from the southwestern wall of the Grímsvötn caldera in Vatnajökull on December, 19 1998.

 

Image: Measuring a Superheated Fumarole
Measuring a Superheated Fumarole
Measuring a Superheated Fumarole
Measuring a Superheated Fumarole

USGS geochemist Bill Evans measures the temperature of a superheated (hotter than the boiling point) fumarole in Lassen Volcanic National Park.

USGS geochemist Bill Evans measures the temperature of a superheated (hotter than the boiling point) fumarole in Lassen Volcanic National Park.

Profile of Mauna Kea showing inferred contact (dot-dashed line) bet...
Profile of Mauna Kea showing inferred contact (dot-dashed line) bet...
Profile of Mauna Kea showing inferred contact (dot-dashed line) bet...
Profile of Mauna Kea showing inferred contact (dot-dashed line) bet...

Profile of Mauna Kea showing inferred contact (dot-dashed line) between postshield-stage Hamakua Volcanics and underlying shield-stage lavas. Approximate contact with Laupahoehoe Volcanics dashed.

Vog conditions on the Island of Hawai‘i vary depending on wind dire...
Vog conditions on the Island of Hawai‘i vary depending on wind direction
Vog conditions on the Island of Hawai‘i vary depending on wind direction
Vog conditions on the Island of Hawai‘i vary depending on wind direction

During prevailing trade wind conditions, the nearly constant stream of volcanic smog (vog) produced by Kīlauea Volcano on the Island of Hawai‘i is blown to the southwest and west. The trade winds (blue arrows) blow the vog from its main source on the volcano (white plume) to the southwest, where wind patterns send it up the island's Kona coast.

During prevailing trade wind conditions, the nearly constant stream of volcanic smog (vog) produced by Kīlauea Volcano on the Island of Hawai‘i is blown to the southwest and west. The trade winds (blue arrows) blow the vog from its main source on the volcano (white plume) to the southwest, where wind patterns send it up the island's Kona coast.

View of the Mono Lake-Long Valley volcanic region
View of the Mono Lake-Long Valley volcanic region
View of the Mono Lake-Long Valley volcanic region
View of the Mono Lake-Long Valley volcanic region

An aerial view looking south of the Long Valley volcanic region in the area of Mono Lake, showing a line of rhyolite lava domes and explosion craters. An inset map shows the locations of silcic magmatic centers in the Long Valley area.

An aerial view looking south of the Long Valley volcanic region in the area of Mono Lake, showing a line of rhyolite lava domes and explosion craters. An inset map shows the locations of silcic magmatic centers in the Long Valley area.

Geologic map of Mauna Kea with generalized surface distribution of ...
Geologic map of Mauna Kea with generalized surface distribution of ...
Geologic map of Mauna Kea with generalized surface distribution of ...
Geologic map of Mauna Kea with generalized surface distribution of ...

Geologic map of Mauna Kea with generalized surface distribution of Hamakua Volcanics. Laupahoehoe Volcanics are inferred to overlie a vast area of Hamakua Volcanics on the upper flanks and summit.

Volcanic gases react with the atmosphere in various ways
Volcanic gases react with the atmosphere in various ways
Volcanic gases react with the atmosphere in various ways
Volcanic gases react with the atmosphere in various ways

Volcanic gases react with the atmosphere in various ways; the conversion of sulfur dioxide (SO2) to sulfuric acid (H2SO4) has the most significant impact on climate.

Volcanic gases react with the atmosphere in various ways; the conversion of sulfur dioxide (SO2) to sulfuric acid (H2SO4) has the most significant impact on climate.

Geologic map of Mauna Kea, showing generalized distribution of lava...
Geologic map of Mauna Kea, showing generalized distribution of lava...
Geologic map of Mauna Kea, showing generalized distribution of lava...
Geologic map of Mauna Kea, showing generalized distribution of lava...

Geologic map of Mauna Kea, showing generalized distribution of lava flows, cinder cones, and glacial deposits of the Laupahoehoe Volcanics.

Image: Coso Volcanic Field Tumulus
Coso Volcanic Field Tumulus
Coso Volcanic Field Tumulus
Coso Volcanic Field Tumulus

A tumulus in the Coso Volcanic Field, California. This lava was probably more viscous than the lava found in the Hawaii tumuli.

A tumulus in the Coso Volcanic Field, California. This lava was probably more viscous than the lava found in the Hawaii tumuli.

Image: A'a' Channel
A'a' Channel
A'a' Channel
A'a' Channel

Detail of levee on an active channelized aa flow. Note the pahoehoe overflows in the levees and the level of the active flow below the tops of the levees. This lower flow level is not allowed in the commonly used "Bingham" model of lava flows.

Detail of levee on an active channelized aa flow. Note the pahoehoe overflows in the levees and the level of the active flow below the tops of the levees. This lower flow level is not allowed in the commonly used "Bingham" model of lava flows.

Mount Konocti, a 1,312 m (4,305 ft) mountain on the eastern shore o...
Mount Konocti, a 1,312 m (4,305 ft) mountain on the eastern shore o...
Mount Konocti, a 1,312 m (4,305 ft) mountain on the eastern shore o...
Mount Konocti, a 1,312 m (4,305 ft) mountain on the eastern shore o...

Mt. Konocti erupted during the most recent stage of volcanism (01. Ma to 10,000 years ago), and a future eruption from the same site would be devastating to the nearby inhabitants.

Image: Vatnajökull Jökulhlaup
Vatnajökull Jökulhlaup
Vatnajökull Jökulhlaup
Vatnajökull Jökulhlaup

Photograph of the large jökulhlaup that spread out across Skeiðarársandur (glacial outwash plain) from the terminus of Skeiðarárjökull, an outlet glacier of Vatnajökull.

Photograph of the large jökulhlaup that spread out across Skeiðarársandur (glacial outwash plain) from the terminus of Skeiðarárjökull, an outlet glacier of Vatnajökull.

Tephra-jet explosion hurls spatter 50 m (165 ft) high, Kīlauea Volc...
Tephra-jet explosion hurls spatter 50 m (165 ft) high to create a l...
Tephra-jet explosion hurls spatter 50 m (165 ft) high to create a l...
Tephra-jet explosion hurls spatter 50 m (165 ft) high to create a l...

Lava fragments explode onto the sides of a littoral cone on the south coast of Kīlauea Volcano as lava pours into the sea from a lava tube.

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