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California Volcano Observatory images.

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An expansive view from the top of a tall hill shows a large lake bordered by a large forested mountain with several peaks.
Mount Konocti, Clear Lake Volcanic Field
Mount Konocti, Clear Lake Volcanic Field
Mount Konocti, Clear Lake Volcanic Field

A southwesterly view of Mount Konocti, which is one of the largest volcanic features in the Clear Lake Volcanic Field. Buckingham Peninsula can also be seen stretching from the base of Mount Konocti into the foreground toward the eastern shore of the lake.  USGS photo by J.Ball

A southwesterly view of Mount Konocti, which is one of the largest volcanic features in the Clear Lake Volcanic Field. Buckingham Peninsula can also be seen stretching from the base of Mount Konocti into the foreground toward the eastern shore of the lake.  USGS photo by J.Ball

A hiker looks up at a cliff of pockmarked, grungy gray rock which has fractures and multiple shades of white and tan breaking up its surface. The pockmarks resemble honeycomb, and the overall texture of the rock shows that it has numerous chunks of smaller rocks embedded in a white matrix.
Intracaldera tuff on Mount St. Helena, Sonoma Volcanic Field, CA
Intracaldera tuff on Mount St. Helena, Sonoma Volcanic Field, CA
Intracaldera tuff on Mount St. Helena, Sonoma Volcanic Field, CA

Ash-flow tuff (ignimbrite) on the fire road leading to the summit of Mount St. Helena, mapped as part of the intracaldera Sonoma volcanics. 

A dark red, rubbly cliff of lava angles sharply into the background over a flat terrace of bright green grass
Berkeley Hills Volcanic Field
Berkeley Hills Volcanic Field
Berkeley Hills Volcanic Field

The Moraga Volcanics, one of several volcanic formations found in the Berkeley Hills Volcanic Field, frame a view of Mount Diablo to the east. The basaltic lava flows and their associated lapilli tuffs can be found in the Sibley Volcanic Regional Preserve. USGS photo by J. Ball

The Moraga Volcanics, one of several volcanic formations found in the Berkeley Hills Volcanic Field, frame a view of Mount Diablo to the east. The basaltic lava flows and their associated lapilli tuffs can be found in the Sibley Volcanic Regional Preserve. USGS photo by J. Ball

A geologist in a blue shirt and khakis supports a basketball-sized chunk of lava on his knee. A bright white "rind" makes up about half of the chunk, surrounding a core of dark gray lava speckled with white crystals. A marker rests on the chunk for a sense of scale, and similar white chunks of lava make up the background of the photo.
A heavily hydrothermally-altered sample of lava from the Clear Lake Volcanic Field
A heavily hydrothermally-altered sample of lava from the Clear Lake Volcanic Field
A heavily hydrothermally-altered sample of lava from the Clear Lake Volcanic Field

Geologists often break off the weathered surfaces of rocks in the field to get at the fresh, clean cores. This makes it easier to see the original mineralogy of the rock in question without oxidation, alteration, or other environmental impacts. USGS photo by D. Blatter

Geologists often break off the weathered surfaces of rocks in the field to get at the fresh, clean cores. This makes it easier to see the original mineralogy of the rock in question without oxidation, alteration, or other environmental impacts. USGS photo by D. Blatter

A geologist wearing a blue button-down shirt, khaki pants, and an orange ball cap uses a rock hammer to break smaller chunks off the large, weathered, brownish boulders that surround him. The interior of the chunks is revealed to be a pale, speckled gray.
Breaking off the weathered surface of lavas in the Clear Lake Volcanic Field to sample the fresh, unaltered cores
Breaking off the weathered surface of lavas in the Clear Lake Volcanic Field to sample the fresh, unaltered cores
Breaking off the weathered surface of lavas in the Clear Lake Volcanic Field to sample the fresh, unaltered cores

Geologists often break off the weathered surfaces of rocks in the field to get at the fresh, clean cores. This makes it easier to see the original mineralogy of the rock in question without oxidation, alteration, or other environmental impacts. USGS photo by D. Blatter.

A geologist in tan pants, a blue button-down shirt and an orange hat stands with one foot on a boulder at the side of a road, holding up a baggie of rocks. Behind him the ground has been scraped bare by construction equipment.
Basalt, Clear Lake Volcanic Field
Basalt, Clear Lake Volcanic Field
Basalt, Clear Lake Volcanic Field

These freshly excavated boulders along Spruce Grove Road are basalt, which is an iron and magnesium-rich rock that’s fairly uncommon in the Clear Lake Volcanic Field.

These freshly excavated boulders along Spruce Grove Road are basalt, which is an iron and magnesium-rich rock that’s fairly uncommon in the Clear Lake Volcanic Field.

A male geologist in an orange ballcap and blue button-down shirt holds a rock hammer in one hand and a rock in the other.
Eruption Episode 3 rocks, Clear Lake Volcanic Field, California
Eruption Episode 3 rocks, Clear Lake Volcanic Field, California
Eruption Episode 3 rocks, Clear Lake Volcanic Field, California

Eruption episode 3 is the most voluminous in the history of the Clear Lake Volcanic Field. Episode 3 rocks are of intermediate composition, primarily dacite, and make up many of the topographic high points in the field, including Mt. Konocti, where this photo is taken.

Eruption episode 3 is the most voluminous in the history of the Clear Lake Volcanic Field. Episode 3 rocks are of intermediate composition, primarily dacite, and make up many of the topographic high points in the field, including Mt. Konocti, where this photo is taken.

In front of an outcrop of matte grey rock splotched with lichens, a young man in an orange safety vest gives a happy thumbs up and an older man sits writing notes in a small notebook and smiles at the camera. The rocks are perched on a moderate slope covered in brushy manzanita and scraggly pine trees.
CalVO geologists take paleomag samples from a basaltic andesite lava flow on Ash Creek Butte
CalVO geologists take paleomag samples from a basaltic andesite lava flow on Ash Creek Butte
CalVO geologists take paleomag samples from a basaltic andesite lava flow on Ash Creek Butte

Andy Calvert and Tony Pivarunas drill into the face of a lava flow on Ash Creek Butte, a Pleistocene shield volcano northeast of Mount Shasta. USGS photo by Dawnika Blatter

Geophysicist works at station PR05, part of the Mount Rainier lahar detection network.
Station PR05 is part of the Mount Rainier lahar detection network.
Station PR05 is part of the Mount Rainier lahar detection network.
Station PR05 is part of the Mount Rainier lahar detection network.

USGS-Cascades Volcano Observatory geophysicist Rebecca Kramer works on station PR05, which is part of the Mount Rainier lahar detection network (Mount Rainier is pictured in the distance). The purpose of the site visit was to upgrade the power system and deploy infrasound equipment. 

USGS-Cascades Volcano Observatory geophysicist Rebecca Kramer works on station PR05, which is part of the Mount Rainier lahar detection network (Mount Rainier is pictured in the distance). The purpose of the site visit was to upgrade the power system and deploy infrasound equipment. 

This photo looks across an active rock quarry at a conical hill that has been mined, revealing a dark red interior
Clearlake Oaks cinder cone, Clear Lake Volcanic Field, California
Clearlake Oaks cinder cone, Clear Lake Volcanic Field, California
Clearlake Oaks cinder cone, Clear Lake Volcanic Field, California

Cinder cones (or scoria cones) are relatively small, steep-sided volcanoes that are constructed around a single vent when lava is ejected into the air, breaks into smaller pieces, and builds up around the sides of the vent. This photo is looking across the quarry which exposes the interior of a cinder cone east of Clearlake Oaks in the Clear Lake Volcanic Field.

Cinder cones (or scoria cones) are relatively small, steep-sided volcanoes that are constructed around a single vent when lava is ejected into the air, breaks into smaller pieces, and builds up around the sides of the vent. This photo is looking across the quarry which exposes the interior of a cinder cone east of Clearlake Oaks in the Clear Lake Volcanic Field.

A view on a clear day, looking down from a high volcanic peak at a cratered promontory in the blue waters of Clear Lake.
Buckingham Peninsula, Clear Lake, CA
Buckingham Peninsula, Clear Lake, CA
Buckingham Peninsula, Clear Lake, CA

Located at the midpoint of Clear Lake in Lake County, California, Buckingham Peninsula shows evidence of young explosive volcanism in the Clear Lake Volcanic Field. Little Borax Lake, enclosed within the Buckingham golf course, is a water-filled maar crater, as is Horseshoe Bay to its northeast. USGS photo by J. Ball.

Located at the midpoint of Clear Lake in Lake County, California, Buckingham Peninsula shows evidence of young explosive volcanism in the Clear Lake Volcanic Field. Little Borax Lake, enclosed within the Buckingham golf course, is a water-filled maar crater, as is Horseshoe Bay to its northeast. USGS photo by J. Ball.

A scientist in a broad-brimmed hat sits on a large gray boulder of volcanic rock, surrounded by similar boulders. They are holding a rock hammer against the rock in preparation to break off a sample. In the distance, several hazy mountain ridges can be seen.
Sampling lava flows on Cobb Mountain, California
Sampling lava flows on Cobb Mountain, California
Sampling lava flows on Cobb Mountain, California

Collecting samples on Cobb Mountain south of the Clear Lake Volcanic Field helps CalVO scientists unravel the eruptive history of the area. By examining these samples on the macro and micro scales, they can derive the geochemical evolution and eruption age of the lavas that form Cobb Mountain. USGS photo by Sally Stevens.

Collecting samples on Cobb Mountain south of the Clear Lake Volcanic Field helps CalVO scientists unravel the eruptive history of the area. By examining these samples on the macro and micro scales, they can derive the geochemical evolution and eruption age of the lavas that form Cobb Mountain. USGS photo by Sally Stevens.

A deep blue lake is nestled in pine forest at the foot of a rocky, hilly peak
Mammoth Mountain
Mammoth Mountain
Mammoth Mountain

View of the Mammoth Mountain lava dome complex overlooking Horseshoe Lake.

View of the Mammoth Mountain lava dome complex overlooking Horseshoe Lake.

Eddy covariance station at Mammoth Mountain, California
Eddy covariance station at Mammoth Mountain, California
Eddy covariance station at Mammoth Mountain, California
Eddy covariance station at Mammoth Mountain, California

Photograph of permanent eddy covariance station installed since 2014 in area of volcanic CO2 emissions on Mammoth Mountain, California. USGS photo by Jennifer Lewicki, August 2019.

Viewed from a distance, a small mountain range sits isolated among broad, flat fields.
Sutter Buttes
Sutter Buttes
Sutter Buttes

Located 50 miles north-northwest of Sacramento, Sutter Buttes are the only volcano in the Central Valley. They consist of a central core of andesite, dacite, and rhyolite domes and flows. These are surrounded by a large apron of fragmental volcanic debris.

Located 50 miles north-northwest of Sacramento, Sutter Buttes are the only volcano in the Central Valley. They consist of a central core of andesite, dacite, and rhyolite domes and flows. These are surrounded by a large apron of fragmental volcanic debris.

Rear-arc basalt lava outcrop
Rear-arc basalt lava outcrop
Rear-arc basalt lava outcrop
Rear-arc basalt lava outcrop

A 3-4m (10-12 ft) high outcrop of basalt lava, part of a broader lava flow. These flows were erupted about 300,000 years ago following basalt dike intrusions in a rear-arc region of northern California. The eruptions of three of these flows are thought to have taken place within several hundred years of each other.

A 3-4m (10-12 ft) high outcrop of basalt lava, part of a broader lava flow. These flows were erupted about 300,000 years ago following basalt dike intrusions in a rear-arc region of northern California. The eruptions of three of these flows are thought to have taken place within several hundred years of each other.

A two part figure with a shaded-relief map view of the Long Valley Caldera marked with the outlines of its resurgent dome, Mammoth Mountain, Crowley Lake, the caldera outline, and major roads. Below is a west-to-east cross-section cartoon of the caldera, showing the locations of these features as well as the depth of caldera fill, basement rocks, and the paths of cold and hot water near magmatic intrusions.
Simplified geologic map (left) and diagrammatic cross section (right) of Long Valley Caldera.
Simplified geologic map (left) and diagrammatic cross section (right) of Long Valley Caldera.
High-resolution, bare-earth, airborne light detection and ranging (...
Lidar image of Rocky Ridge and raised shorelines along Lake Tahoe
Lidar image of Rocky Ridge and raised shorelines along Lake Tahoe
Lidar image of Rocky Ridge and raised shorelines along Lake Tahoe

High-resolution, bare-earth, airborne light detection and ranging (LiDAR) image, looking obliquely northwest into Rocky Ridge.

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