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Volcano Monitoring

Volcano monitoring at Long Valley Caldera.

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Seismic Monitoring at Long Valley Caldera

Seismic monitoring is the most used technique for volcano surveillance.
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Seismic Monitoring at Long Valley Caldera

Seismic monitoring is the most used technique for volcano surveillance.
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Deformation measurements at Long Valley Caldera

When magma moves into a volcanic system, and closer to the surface of the earth, the area surrounding the volcano may move upward and outward. This swelling is typically measured using the Global Positioning System (GPS) and tiltmeters (tilt).
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Deformation measurements at Long Valley Caldera

When magma moves into a volcanic system, and closer to the surface of the earth, the area surrounding the volcano may move upward and outward. This swelling is typically measured using the Global Positioning System (GPS) and tiltmeters (tilt).
Learn More

Gas Monitoring at Long Valley and the Surrounding Region

By monitoring the relative abundances of carbon dioxide (CO2) and sulfur dioxide (SO2), scientists may be able to infer magma movement through the volcanic system.
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Gas Monitoring at Long Valley and the Surrounding Region

By monitoring the relative abundances of carbon dioxide (CO2) and sulfur dioxide (SO2), scientists may be able to infer magma movement through the volcanic system.
Learn More

Hydrothermal Monitoring at Long Valley Caldera

Long Valley Caldera hosts a large hydrothermal system, with hot groundwater, boiling springs, and fumaroles.
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Hydrothermal Monitoring at Long Valley Caldera

Long Valley Caldera hosts a large hydrothermal system, with hot groundwater, boiling springs, and fumaroles.
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