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Images related to Yellowstone Volcano Observatory.

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Schematic illustration showing the 1912 Novarupta eruption in Alaska and the caldera collapse at Mount Katmai
Schematic illustration showing the 1912 Novarupta eruption in Alaska and the caldera collapse at Mount Katmai
Schematic illustration showing the 1912 Novarupta eruption in Alaska and the caldera collapse at Mount Katmai
Mount Epomeo on the island of Ischia
Mount Epomeo on the island of Ischia
Mount Epomeo on the island of Ischia
Mount Epomeo on the island of Ischia

Mount Epomeo on the island of Ischia. The visible western slope of the resurgent block consists of 55,000 year old rocks that formed one of the most widespread Late Quaternary pyroclastic deposits in the Mediterranean region.  INGV photo (https://www.ingv.it/en/Ischia).

Mount Epomeo on the island of Ischia. The visible western slope of the resurgent block consists of 55,000 year old rocks that formed one of the most widespread Late Quaternary pyroclastic deposits in the Mediterranean region.  INGV photo (https://www.ingv.it/en/Ischia).

View from the SE rim of McDermitt caldera, Nevada and Oregon, showing rhyolite lavas overlain by thin outflow McDermitt Tuff in the south wall of the caldera
View from the SE rim of McDermitt caldera, Nevada and Oregon, of the Thacker Pass area
View from the SE rim of McDermitt caldera, Nevada and Oregon, of the Thacker Pass area
View from the SE rim of McDermitt caldera, Nevada and Oregon, of the Thacker Pass area

View from the SE rim of McDermitt caldera, Nevada and Oregon, showing rhyolite lavas overlain by thin outflow McDermitt Tuff in the south wall of the caldera. The low area that makes up most of the photo is intracaldera tuffaceous sediment. This is Thacker Pass, the site of largest and highest-grade lithium deposits in the region.

View from the SE rim of McDermitt caldera, Nevada and Oregon, showing rhyolite lavas overlain by thin outflow McDermitt Tuff in the south wall of the caldera. The low area that makes up most of the photo is intracaldera tuffaceous sediment. This is Thacker Pass, the site of largest and highest-grade lithium deposits in the region.

Folds in outflow sheets of McDermitt Tuff, from the eruption that formed McDermitt Caldera in Nevada and Oregon
Rheomorphism in outflow sheets of McDermitt Tuff, Nevada and Oregon
Rheomorphism in outflow sheets of McDermitt Tuff, Nevada and Oregon
Rheomorphism in outflow sheets of McDermitt Tuff, Nevada and Oregon

Folds in outflow sheets of McDermitt Tuff, from the eruption that formed McDermitt Caldera in Nevada and Oregon about 16.4 million years ago.  The folding is called “rheomorphism” and occurred as the hot ash deposit flowed under its own weight shortly after it was deposited over preexisting topographic highs and lows.  The texture resembles that of rhyolit

Folds in outflow sheets of McDermitt Tuff, from the eruption that formed McDermitt Caldera in Nevada and Oregon about 16.4 million years ago.  The folding is called “rheomorphism” and occurred as the hot ash deposit flowed under its own weight shortly after it was deposited over preexisting topographic highs and lows.  The texture resembles that of rhyolit

geological map with colors depending different rock units
Excerpt from the MBMG Geological Map of the Gardiner 30’ x 60’ Quadrangle
Excerpt from the MBMG Geological Map of the Gardiner 30’ x 60’ Quadrangle
Excerpt from the MBMG Geological Map of the Gardiner 30’ x 60’ Quadrangle

Excerpt from the Geological Map of the Gardiner 30’ x 60’ Quadrangle, South-Central Montana, by Berg and others (1999), focused on Devil’s Slide (colorful blue-green stripes at center of map excerpt).  Full unit description and map available online as Montana Bureau of Miles and Geology Open File No.

Excerpt from the Geological Map of the Gardiner 30’ x 60’ Quadrangle, South-Central Montana, by Berg and others (1999), focused on Devil’s Slide (colorful blue-green stripes at center of map excerpt).  Full unit description and map available online as Montana Bureau of Miles and Geology Open File No.

Steam rises from a hot pool. The foreground is barren, and the background has some low tropical vegetation.
Agua Shuca thermal area, El Salvador
Agua Shuca thermal area, El Salvador
Agua Shuca thermal area, El Salvador

Steam rises above a hot pool at Agua Shuca, one of many thermal areas of the Ahuachapán geothermal field of El Salvador. A sudden hydrothermal explosion at Agua Shuca in October 1990 ejected steam and debris within a 200-m-radius, and about 25 people living adjacent to the thermal area were killed.

Steam rises above a hot pool at Agua Shuca, one of many thermal areas of the Ahuachapán geothermal field of El Salvador. A sudden hydrothermal explosion at Agua Shuca in October 1990 ejected steam and debris within a 200-m-radius, and about 25 people living adjacent to the thermal area were killed.

Geologists in Little Dipper boat on Grand Prismatic Spring
Geologists in Little Dipper boat on Grand Prismatic Spring
Geologists in Little Dipper boat on Grand Prismatic Spring
Geologists in Little Dipper boat on Grand Prismatic Spring

Yellowstone National Park employees Rick Hutchinson (right) and Jim Peaco (left) guide the specially designed Little Dipper boat into the boiling waters of Grand Prismatic Spring to collect measurements of the temperature and structure of the feature. National Park Service photo by Josh Robbins in 1996.

Yellowstone National Park employees Rick Hutchinson (right) and Jim Peaco (left) guide the specially designed Little Dipper boat into the boiling waters of Grand Prismatic Spring to collect measurements of the temperature and structure of the feature. National Park Service photo by Josh Robbins in 1996.

Queen's Laundry bathhouse, in the Lower Geyser Basin of Yellowstone National Park
Queen's Laundry bathhouse, in Yellowstone's Lower Geyser Basin
Queen's Laundry bathhouse, in Yellowstone's Lower Geyser Basin
Queen's Laundry bathhouse, in Yellowstone's Lower Geyser Basin

Queen's Laundry bathhouse, in the Lower Geyser Basin of Yellowstone National Park.  Building began under superintendent Philetus Norris in 1881 but was never finished.

Gas plume rises above lava fountains in a lava lake in the summit crater of Nyiragongo volcano, Democratic Republic of the Congo, on 20 August 1994
Gas plume rises above lava fountains in a lava lake in the summit crater of Nyiragongo volcano, Democratic Republic of the Congo, on 20 August 1994
Gas plume rises above lava fountains in a lava lake in the summit crater of Nyiragongo volcano, Democratic Republic of the Congo, on 20 August 1994
Gas plume rises above lava fountains in a lava lake in the summit crater of Nyiragongo volcano, Democratic Republic of the Congo, on 20 August 1994

A gas plume rises above lava fountains in a lava lake in the summit crater of Nyiragongo volcano on 20 August 1994. USGS photo by Jack Lockwood.

Black and white line drawing showing the geology of the Wind River Range, Wyoming
Geologic map of the Wind River Range, Wyoming
Geologic map of the Wind River Range, Wyoming
Geologic map of the Wind River Range, Wyoming

Geologic map of the Wind River Range from Blackstone, 1993 (The Wind River Range, Wyoming: An Overview. Wyoming Geological Association. Jubilee Anniversary Field Conference Guidebook: Wyoming Geology, Past, Present, and Future. Pg. 121-140).

Geologic map of the Wind River Range from Blackstone, 1993 (The Wind River Range, Wyoming: An Overview. Wyoming Geological Association. Jubilee Anniversary Field Conference Guidebook: Wyoming Geology, Past, Present, and Future. Pg. 121-140).

Deep-ocean hydrothermal vent system from the East Pacific Rise
Deep-ocean hydrothermal vent system from the East Pacific Rise
Deep-ocean hydrothermal vent system from the East Pacific Rise
Deep-ocean hydrothermal vent system from the East Pacific Rise

Photo of a deep-ocean hydrothermal vent system from the East Pacific Rise at 9º39’N latitude and 2550 m (8366 ft) depth showing vigorously venting “black smoker” hydrothermal fluids (329 °C, or 624 °F) that are dark gray to black due to rapid precipitation of iron, copper, and zinc sulfide minerals as the hot water mixes with cold bottom waters.

Photo of a deep-ocean hydrothermal vent system from the East Pacific Rise at 9º39’N latitude and 2550 m (8366 ft) depth showing vigorously venting “black smoker” hydrothermal fluids (329 °C, or 624 °F) that are dark gray to black due to rapid precipitation of iron, copper, and zinc sulfide minerals as the hot water mixes with cold bottom waters.

Track of the Yellowstone hotspot showing the ages and locations of volcanic fields
Track of the Yellowstone hotspot showing the ages and locations of volcanic fields
Track of the Yellowstone hotspot showing the ages and locations of volcanic fields
Track of the Yellowstone hotspot showing the ages and locations of volcanic fields

Color-shaded relief topographic map of the track of the Yellowstone hotspot showing the ages and locations of volcanic fields and faulting patterns which become younger to the northeast.  Areas in cooler colors (greens and blues) represent low topographic elevations, whereas warmer colors (oranges and reds) represent high elevations.  Adapted from

Color-shaded relief topographic map of the track of the Yellowstone hotspot showing the ages and locations of volcanic fields and faulting patterns which become younger to the northeast.  Areas in cooler colors (greens and blues) represent low topographic elevations, whereas warmer colors (oranges and reds) represent high elevations.  Adapted from

water shoots from a rock wall, with forest in the background
Apollinaris Spring, Yellowstone National Park, in 1987
Apollinaris Spring, Yellowstone National Park, in 1987
Apollinaris Spring, Yellowstone National Park, in 1987

Apollinaris Spring in 1987.  The spring was modified in 1925 so that water would flow through pipes to be emitted from a rock wall.  Yellowstone National Park photo by Jim Peaco.

Apollinaris Spring in 1987.  The spring was modified in 1925 so that water would flow through pipes to be emitted from a rock wall.  Yellowstone National Park photo by Jim Peaco.

La Garita Mountain (elevation 4179 m [13711 ft]), Colorado
La Garita Mountain (elevation 4179 m [13711 ft]), Colorado
La Garita Mountain (elevation 4179 m [13711 ft]), Colorado
La Garita Mountain (elevation 4179 m [13711 ft]), Colorado

La Garita Mountain (elevation 4179 m [13711 ft]), Colorado.  The mountain is a resurgent block of Fish Canyon Tuff that is more than 1 km (0.6 mi) thick—the top is eroded and the base is not exposed.  The tuff formed during the eruption of La Garita caldera about 27.8 million years ago and has a volume of more than 5000 km3 (1200 mi3)

La Garita Mountain (elevation 4179 m [13711 ft]), Colorado.  The mountain is a resurgent block of Fish Canyon Tuff that is more than 1 km (0.6 mi) thick—the top is eroded and the base is not exposed.  The tuff formed during the eruption of La Garita caldera about 27.8 million years ago and has a volume of more than 5000 km3 (1200 mi3)

Mount Vesuvius behind city of Naples, Italy
Mount Vesuvius behind city of Naples, Italy
Mount Vesuvius behind city of Naples, Italy
Mount Vesuvius behind city of Naples, Italy

Mount Vesuvius behind city of Naples. The modern cone of Vesuvius is flanked on the left by Monte Somma, the rim of a caldera that formed about 17,000 years ago. Eight major explosive eruptions have occurred since, including the 79 CE eruption that destroyed Pompeii and other towns.

Mount Vesuvius behind city of Naples. The modern cone of Vesuvius is flanked on the left by Monte Somma, the rim of a caldera that formed about 17,000 years ago. Eight major explosive eruptions have occurred since, including the 79 CE eruption that destroyed Pompeii and other towns.

Novarupta dome, Alaska
Novarupta dome, Alaska
Novarupta dome, Alaska
Novarupta dome, Alaska

 

Novarupta Dome, with Falling Mountain and the upper valley portion of the Valley of Ten Thousand Smokes in the background.  Photo by Tom Miller, June 1979.

 

Novarupta Dome, with Falling Mountain and the upper valley portion of the Valley of Ten Thousand Smokes in the background.  Photo by Tom Miller, June 1979.

1975 earthquake damage just south of Mammoth Hot Springs on the Mammoth-Norris highway
1975 earthquake damage just south of Mammoth Hot Springs on the Mammoth-Norris highway
1975 earthquake damage just south of Mammoth Hot Springs on the Mammoth-Norris highway
1975 earthquake damage just south of Mammoth Hot Springs on the Mammoth-Norris highway

Photo of damage to the Mammoth-Norris highway, just south of Mammoth Hot Springs, caused by the June 30, 1975, magnitude-6 earthquake.  Haynes Inc. photo for the Deseret News.

Gibbon River in Gibbon Meadows immediate following the 1975 Yellowstone National Park earthquake
Gibbon River in Gibbon Meadows immediate following the 1975 Yellowstone National Park earthquake
Gibbon River in Gibbon Meadows immediate following the 1975 Yellowstone National Park earthquake
Gibbon River in Gibbon Meadows immediate following the 1975 Yellowstone National Park earthquake

Gibbon River in Gibbon Meadows immediate following the June 30, 1975, magnitude-6 Yellowstone National Park earthquake.  The muddy color is due to increased sediment load.  NPS photo by Rick Hutchinson.

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