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California Volcano Observatory

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As a part of the U.S. Geological Survey's Volcano Hazards Program, the California Volcano Observatory aims to advance scientific understanding of volcanic processes and lessen the harmful impacts of volcanic activity in the volcanically active areas of California and Nevada. 

The U.S. Geological Survey California Volcano Observatory (USGS CalVO) was formed in 2012 and is headquartered at Moffett Field, CA. It replaced the former Long Valley Observatory (LVO), which was established in 1982 to monitor the restless Long Valley Caldera and Mono-Inyo Craters region of Eastern California. CalVO now monitors these and other potentially hazardous volcanoes in California and Nevada to help communities and government authorities understand, prepare for, and respond to, volcanic activity. 

Sixteen young volcanoes designated as Low Threat to Very High Threat are dispersed throughout the State. Partially molten rock (magma) resides beneath at least seven of these—Medicine Lake Volcano, Mount Shasta, Lassen Volcanic Center, Clear Lake Volcanic Field, the Long Valley Volcanic Region, Coso Volcanic Field, and Salton Buttes— producing volcanic earthquakes(seismicity), toxic gas emissions, hot springs, and (or) ground movement (deformation).

News

Mount Shasta's spectacular lenticular clouds

Mount Shasta's spectacular lenticular clouds

Hazard-ception: Fires are a hazard for monitoring California's hazardous volcanoes

Hazard-ception: Fires are a hazard for monitoring California's hazardous volcanoes

Paleomagnetic analysis is (super) cool with a cryogenic magnetometer

Paleomagnetic analysis is (super) cool with a cryogenic magnetometer

Publications

Multidisciplinary constraints on magma compressibility, the pre-eruptive exsolved volatile fraction, and the H2O/CO2 molar ratio for the 2006 Augustine eruption, Alaska Multidisciplinary constraints on magma compressibility, the pre-eruptive exsolved volatile fraction, and the H2O/CO2 molar ratio for the 2006 Augustine eruption, Alaska

Geodetically modeled reservoir volume changes during volcanic eruptions are commonly much smaller than the observed eruptive volumes. This discrepancy is thought to be partially due to the compressibility of magma, which is largely controlled by the presence of exsolved volatiles. The 2006 eruption of Augustine Volcano, Alaska, produced an eruptive volume that was ∼3 times larger than...
Authors
Valerie Wasser, Taryn M. Lopez, Kyle Anderson, Pavel Izbekov, Jeffrey T. Freymueller

California’s exposure to volcanic hazards California’s exposure to volcanic hazards

The potential for damaging earthquakes, landslides, floods, tsunamis, and wildfires is widely recognized in California. The same cannot be said for volcanic eruptions, despite the fact that they occur in the state about as frequently as the largest earthquakes on the San Andreas Fault. At least ten eruptions have taken place in the past 1,000 years, and future volcanic eruptions are...
Authors
Margaret Mangan, Jessica Ball, Nathan Wood, Jamie L. Jones, Jeff Peters, Nina Abdollahian, Laura Dinitz, Sharon Blankenheim, Johanna Fenton, Cynthia Pridmore

Eruption probabilities for the Lassen Volcanic Center and regional volcanism, northern California, and probabilities for large explosive eruptions in the Cascade Range Eruption probabilities for the Lassen Volcanic Center and regional volcanism, northern California, and probabilities for large explosive eruptions in the Cascade Range

Chronologies for eruptive activity of the Lassen Volcanic Center and for eruptions from the regional mafic vents in the surrounding area of the Lassen segment of the Cascade Range are here used to estimate probabilities of future eruptions. For the regional mafic volcanism, the ages of many vents are known only within broad ranges, and two models are developed that should bracket the...
Authors
Manuel Nathenson, Michael Clynne, L.J. Muffler

Science

Volcano Hazards Assessments

Geologists create hazard maps to convey the types of hazards that may occur during future eruptions and to identify the areas of potential impact. Specific hazards to people and property depend on eruption style, the volume of lava erupted, the location of the eruptive vent, the eruption duration, and local hydrologic conditions. As geologic research progresses, these maps are updated and created.
Volcano Hazards Assessments

Volcano Hazards Assessments

Geologists create hazard maps to convey the types of hazards that may occur during future eruptions and to identify the areas of potential impact. Specific hazards to people and property depend on eruption style, the volume of lava erupted, the location of the eruptive vent, the eruption duration, and local hydrologic conditions. As geologic research progresses, these maps are updated and created.
Learn More

Volcano Monitoring at California Volcano Observatory

CalVO monitors volcanoes in California with GPS sensors, tiltmeters, strainmeters, and satellite imagery.
Volcano Monitoring at California Volcano Observatory

Volcano Monitoring at California Volcano Observatory

CalVO monitors volcanoes in California with GPS sensors, tiltmeters, strainmeters, and satellite imagery.
Learn More

California has active and hazardous volcanoes

Threat rankings issued by the U.S. Geological Survey (USGS) for California identify fifteen volcanic centers of Low-, Moderate-, High-, or Very High Threat.
California has active and hazardous volcanoes

California has active and hazardous volcanoes

Threat rankings issued by the U.S. Geological Survey (USGS) for California identify fifteen volcanic centers of Low-, Moderate-, High-, or Very High Threat.
Learn More

Multimedia

In this photo of a bare, rocky hill in the middle of a fire-blackened forest, a pole and strapping are laying on the ground next to a charred stump. In the foreground, a dented and warped box contains the melted remains of several large bits of electronics. USGS photo by Ryan Presser, NCSN.
Fire-damaged seismic station in the Lassen Volcanic Center
Fire-damaged seismic station in the Lassen Volcanic Center
A silvery scientific instrument in a wooden room. The instrument consists of two open frameworks of slotted gray aluminum bars, in which is a large silver cylinder with another off to it side. Cables and tubes snake out of the instrument to power outlets, motor boxes, and sensor boxes. The instrument is tall and protrudes into an opening in the roof of the room.
Cryogenic magnetometer in the USGS California Volcano Observatory Paleomagnetics Laboratory
Cryogenic magnetometer in the USGS California Volcano Observatory Paleomagnetics Laboratory
A stylized circular logo reads "California Volcano Observatory U.S. Geological Survey" in black on gray font with a central vector image of a brown bear in profile on red ground. Green forests are visible in the mid ground and the two peaks of Mount Shasta and Shastina are shown in the distance.
USGS California Volcano Observatory logo
USGS California Volcano Observatory logo
Aerial view of Mount Konocti, highlighting Little Borax Lake, the Black Forest landslide scarp and deposits
The lava dome complex of Mount Konocti, Clear Lake Volcanic Field
The lava dome complex of Mount Konocti, Clear Lake Volcanic Field
Map of faults around the Clear Lake volcanic field, highlighting the Bartlett Springs and Maacama faults and the field bounds
Faults bounding the Clear Lake Volcanic Field
Faults bounding the Clear Lake Volcanic Field
Map of faults around the Geysers Geothermal Field with the Maacama in green and Collayami in purple
Faults bounding the Geysers Geothermal Complex
Faults bounding the Geysers Geothermal Complex
An oblique map view of Cobb Mountain and surrounding landscape, featuring Clear Lake, Mount Konocti, and The Geysers
Cobb Mountain and The Geysers geothermal field
Cobb Mountain and The Geysers geothermal field
A geologist wearing a green USGS shirt and ballcap is seen from the back, standing at the top of a hill overlooking a lake and a large mountain. The lake is divided by a long peninsula dotted with homes and trees, and the mountain has two prominent peaks that are covered in dark forest.
Mount Konocti, Clear Lake Volcanic Field, and CalVO geologist Seth Burgess
Mount Konocti, Clear Lake Volcanic Field, and CalVO geologist Seth Burgess
A 3D block diagram showing a cross-section of geologic layers being split by a fault. The block on the right side of the diagram is being dropped down along an incline below the block on the left.
Normal fault
Normal fault
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