Skip to main content
U.S. flag

An official website of the United States government

Yellowstone

Find U.S. Volcano
Current Alerts
Yellowstone
green NORMAL, 2024-08-01 15:43:34 UTC

The Yellowstone Plateau volcanic field developed through three volcanic cycles that span two-million years. Two of the eruptions are considered some of the world's largest volcanic events. Yellowstone's youngest eruptions have been lava flows that remain confined to the caldera of present-day Yellowstone National Park. The 77,000 year-old Pitchstone Plateau flow is the volcano's most recent lava.

Quick Facts

Location: Wyoming and Montana

Latitude: 44.615° N

Longitude: 110.6° W

Elevation: 2,805 m / 9,203 f

Volcano type: Caldera

Composition: basalt to rhyolite

Most recent eruption: 70,000 years ago (lava), current hydrothermal explosions

Threat Potential: High*

*based on the National Volcano Early Warning System

Summary

The >2450 km3 (588 mi3) Huckleberry Ridge Tuff erupted about 2.1 million years ago, creating an approximately 75 km (47 mi) wide caldera and thick volcanic deposits. A second eruption cycle concluded with the much smaller Mesa Falls Tuff around 1.3 million years ago. Activity subsequently shifted to the present Yellowstone Plateau and culminated 640,000 years ago with the eruption of the >10003km (240 mi3) Lava Creek Tuff and consequent formation of the 45 x 85 km (28 x 53 mi) caldera. Large volumes of rhyolitic lava flows (approximately 600 km3 (144 mi3) were erupted in the caldera between 180,000 and 70,000 years ago, distributed primarily along two north-south alignments of vents.

No magmatic eruptions have occurred since then, but large hydrothermal explosions have taken place during the Holocene, including from within and near Yellowstone Lake. Uplift and subsidence of the ground surface is centered on two uplifted regions (the Mallard Lake and Sour Creek resurgent domes). Large earthquakes occur just off the plateau along the nearby Teton and Hebgen Lake faults, the latter of which ruptured in 1959 (Ms = 7.5), causing considerable damage to the region. Yellowstone is presently the site of one of the world's largest hydrothermal systems including Earth's largest concentration of geysers.

News

Yellowstone thermal features, from Apollinaris to Zomar

Yellowstone thermal features, from Apollinaris to Zomar

Digging into the history of hydrothermal explosions at Biscuit Basin

Digging into the history of hydrothermal explosions at Biscuit Basin

The probability of hydrothermal explosions in Yellowstone

The probability of hydrothermal explosions in Yellowstone

Publications

2018 update to the U.S. Geological Survey national volcanic threat assessment

When erupting, all volcanoes pose a degree of risk to people and infrastructure, however, the risks are not equivalent from one volcano to another because of differences in eruptive style and geographic location. Assessing the relative threats posed by U.S. volcanoes identifies which volcanoes warrant the greatest risk-mitigation efforts by the U.S. Geological Survey and its partners. This update

Authors
John W. Ewert, Angela K. Diefenbach, David W. Ramsey

Science

Questions About Monitoring Yellowstone

Answers to questions about monitoring at Yellowstone.
link

Questions About Monitoring Yellowstone

Answers to questions about monitoring at Yellowstone.
Learn More

Monitoring Earthquakes in Yellowstone National Park

The Yellowstone region is one of the most seismically active areas in the United States. It experiences an average of around 1,500 to 2,500 located earthquakes per year! The majority of these earthquakes are too small to be felt by humans but are detected by a sophisticated network of about 50 seismometers called the Yellowstone Seismic Network (YSN).
link

Monitoring Earthquakes in Yellowstone National Park

The Yellowstone region is one of the most seismically active areas in the United States. It experiences an average of around 1,500 to 2,500 located earthquakes per year! The majority of these earthquakes are too small to be felt by humans but are detected by a sophisticated network of about 50 seismometers called the Yellowstone Seismic Network (YSN).
Learn More

Monitoring Deformation in Yellowstone National Park

Movement of the ground in Yellowstone can tell scientists a lot about what’s happening below the surface. In order to monitor subtle “deformation” of the ground, YVO relies most heavily on Global Positioning System (GPS) stations, strainmeters, and tiltmeters, with instruments that are maintained by UNAVCO.
link

Monitoring Deformation in Yellowstone National Park

Movement of the ground in Yellowstone can tell scientists a lot about what’s happening below the surface. In order to monitor subtle “deformation” of the ground, YVO relies most heavily on Global Positioning System (GPS) stations, strainmeters, and tiltmeters, with instruments that are maintained by UNAVCO.
Learn More

Multimedia

Update Biscuit Basin Biscuit Basin Update; 65th Anniversary — M7.3 Hebgen Lake Quake (Yellowstone Monthly Update - Aug 2024)
Biscuit Basin Update; 65th Anniversary — M7.3 Hebgen Lake Quake (Yellowstone Monthly Update - Aug 2024)
Plot of size versus annual probability for hydrothermal explosion craters in Yellowstone National Park
Plot of size versus annual probability for hydrothermal explosion craters in Yellowstone National Park
Plot of size versus annual probability for hydrothermal explosion craters in Yellowstone National Park
Graph showing explosions recorded at Black Diamond Pool in Biscuit Basin, Yellowstone National Park, during 2006 through 2016
Graph showing explosions recorded at Black Diamond Pool in Biscuit Basin, Yellowstone National Park, during 2006 through 2016
Graph showing explosions recorded at Black Diamond Pool in Biscuit Basin, Yellowstone National Park, during 2006 through 2016
Photomicrograph showing a quartz-hosted embayment from the Mesa Falls Tuff, accompanied by a map showing the location of the tuff in eastern Idaho.
Quartz-hosted embayment from the Mesa Falls Tuff
Quartz-hosted embayment from the Mesa Falls Tuff
Photomicrograph showing water distribution in a quartz-hosted embayment, with greater concentrations at the embayment mouth. Includes a plot showing that the temperature in which the water circulated must have been about 500 degrees Celsius.
Water distribution in a quartz-hosted embayment from the Mesa Falls Tuff
Water distribution in a quartz-hosted embayment from the Mesa Falls Tuff
Large block of debris in front of a steaming pool.  The block was transported by the July 23, 2024, hydrothermal explosion at Biscuit Basin, Yellowstone National Park
Largest identified boulder displaced by the July 23, 2024, explosion from Black Diamond Pool, Yellowstone National Park
Largest identified boulder displaced by the July 23, 2024, explosion from Black Diamond Pool, Yellowstone National Park
Large cloud of smoke and rock rising from the air. Hydrothermal Explosion in Yellowstone's Biscuit Basin (July 23, 2024)
Hydrothermal Explosion in Yellowstone's Biscuit Basin (July 23, 2024)
High-resolution Planet satellite image of Biscuit Basin, Yellowstone National Park, from July 24, 2024
High-resolution Planet satellite image of Biscuit Basin, Yellowstone National Park, from July 24, 2024
High-resolution Planet satellite image of Biscuit Basin, Yellowstone National Park, from July 24, 2024
Aerial view of Biscuit Basin, Yellowstone National Park, showing debris deposited by the July 23, 2024, hydrothermal explosion from Black Diamond Pool
Aerial view of Biscuit Basin, Yellowstone National Park, showing debris deposited by the July 23, 2024, hydrothermal explosion from Black Diamond Pool
Aerial view of Biscuit Basin, Yellowstone National Park, showing debris deposited by the July 23, 2024, hydrothermal explosion from Black Diamond Pool