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Multimedia related to Valles Caldera.

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Panoramic image of Valles Caldera, New Mexico
Panoramic image of Valles Caldera, New Mexico
Panoramic image of Valles Caldera, New Mexico
Panoramic image of Valles Caldera, New Mexico

Panoramic image of Valles Caldera, New Mexico, looking at the Valle Grande, part of the calderas “moat.”  The resurgent dome is the high topography at the left side of the image, while the hills at the center and right are lava domes.  USGS photo by Mike Poland, June 10, 2022.

Panoramic image of Valles Caldera, New Mexico, looking at the Valle Grande, part of the calderas “moat.”  The resurgent dome is the high topography at the left side of the image, while the hills at the center and right are lava domes.  USGS photo by Mike Poland, June 10, 2022.

Panoramic image of the Sulphur Springs thermal area in Valles Caldera, New Mexico
Panoramic image of the Sulphur Springs thermal area in Valles Caldera, New Mexico
Panoramic image of the Sulphur Springs thermal area in Valles Caldera, New Mexico
Panoramic image of the Sulphur Springs thermal area in Valles Caldera, New Mexico

Panoramic image of the Sulphur Springs thermal area in Valles Caldera, New Mexico.  The altered surface, composed of clays, strongly resembles acid-sulfate thermal areas in Yellowstone National Park, like the Mud Volcano region.  USGS photo by Mike Poland, June 10, 2022.

Panoramic image of the Sulphur Springs thermal area in Valles Caldera, New Mexico.  The altered surface, composed of clays, strongly resembles acid-sulfate thermal areas in Yellowstone National Park, like the Mud Volcano region.  USGS photo by Mike Poland, June 10, 2022.

The Bandelier Tuff near Los Alamos, New Mexico
The Bandelier Tuff near Los Alamos, New Mexico
The Bandelier Tuff near Los Alamos, New Mexico
The Bandelier Tuff near Los Alamos, New Mexico

The Bandelier Tuff near Los Alamos, New Mexico.  The Jemez Mountains, home to the Valles and Toledo calderas where the tuff originated, rise in the distance.  The tuff was hot and thick when it was deposited by caldera-forming eruptions 1.61 and 1.25 million years ago, and so it is welded in places, forming a dense and resistant rock.  USGS photo by M

The Bandelier Tuff near Los Alamos, New Mexico.  The Jemez Mountains, home to the Valles and Toledo calderas where the tuff originated, rise in the distance.  The tuff was hot and thick when it was deposited by caldera-forming eruptions 1.61 and 1.25 million years ago, and so it is welded in places, forming a dense and resistant rock.  USGS photo by M

Landsat-7 satellite image of Jemez Mountains and Valles Caldera, New Mexico
Landsat-7 satellite image of Jemez Mountains and Valles Caldera, New Mexico
Landsat-7 satellite image of Jemez Mountains and Valles Caldera, New Mexico
Landsat-7 satellite image of Jemez Mountains and Valles Caldera, New Mexico

Landsat-7 satellite image of Jemez Mountains and Valles Caldera, New Mexico.  The Valles and Toledo Caldera margins are approximated by dashed yellow lines, and the resurgent dome and lava domes are labeled.  The Banco Bonito lava flow is the youngest in the region at 68,000 years old.  The town of Los Alamos is located just east of the caldera. 

Landsat-7 satellite image of Jemez Mountains and Valles Caldera, New Mexico.  The Valles and Toledo Caldera margins are approximated by dashed yellow lines, and the resurgent dome and lava domes are labeled.  The Banco Bonito lava flow is the youngest in the region at 68,000 years old.  The town of Los Alamos is located just east of the caldera.