Abyss Pool is about 16 m (53 ft) deep and contains alkaline-chloride hydrothermal fluids that in the summer of 2024 had a temperature of 181 °F (83 °C).
Why is Yellowstone called Yellowstone?
Contrary to popular belief, Yellowstone was not named for the abundant rhyolite lavas in the Grand Canyon of Yellowstone that have been chemically altered by reactions with steam and hot water to create vivid yellow and pink colors. Instead, the name was attributed as early as 1805 to Native Americans who were referring to yellow sandstones along the banks of the Yellowstone River in eastern Montana, several hundred miles downstream and northeast of the Park.
Learn more: Alterations to go! Hydrothermal alteration in Yellowstone
Related
When will the next large earthquake occur in Yellowstone?
Earthquakes cannot be predicted yet, but modern surveillance for earthquakes in Yellowstone conducted with seismographs (instruments that measure earthquake locations and magnitudes) and GPS - Global Positioning Systems (instruments that measure slow ground movements) help scientists understand the state of stress in the Earth's crust. Those stresses could trigger earthquakes as well as magma...
Why are there so many earthquakes at Yellowstone?
Almost all earthquakes at Yellowstone are brittle-failure events caused when rocks break due to crustal stresses. Though we've been looking at Yellowstone for years, no one has yet identified "long-period (LP) events" commonly attributed to magma movement. If LP events are observed, that will NOT mean Yellowstone is getting ready to erupt. LP earthquakes commonly occur at other volcanoes in the...
What is the relationship between volcanism and the geysers and hot springs in Yellowstone?
Heat and volcanic gases from slowly cooling magma rise and warm the dense salty water that occupies fractured rocks above the Yellowstone magma chamber. That brine, in turn, transfers its heat to overlying fresh groundwater which is recharged by rainfall and snowmelt from the surface. Water boiling at depth below the surface is hotter than the temperature of boiling at the surface. If it rises...
How hot is Yellowstone?
Yellowstone is a plateau high in the Rocky Mountains, and is snowbound for over six months per year. The mean annual temperature is 2.2°C (36°F), barely above the freezing point of water. However, Yellowstone is also an active geothermal area with hot springs emerging at ~92°C (~198°F) (the boiling point of water at Yellowstone's mean altitude) and steam vents reported as high as 135°C (275°F)...
How fast is the hotspot moving under Yellowstone?
Actually, the source of the hotspot is more or less stationary at depth within the Earth, and the North America plate moves southwest across it. The average rate of movement of the plate in the Yellowstone area for the last 16.5 million years has been about 4.6 centimeters (1.8 inches) per year. However, if shorter time intervals are analyzed, the plate can be inferred to have moved about 6.1...
Can we use the heat from Yellowstone for energy?
Geothermal energy (heat energy from the Earth's interior) is used to generate electricity in a variety of places throughout the world. Although Yellowstone National Park and its surroundings are a significant geothermal resource, the Park itself is off limits to development. Geothermal developments often cause a decrease in the flow of nearby hot springs and other geothermal features (like geysers...
Abyss Pool, West Thumb Geyser Basin, Yellowstone National Park
Abyss Pool is about 16 m (53 ft) deep and contains alkaline-chloride hydrothermal fluids that in the summer of 2024 had a temperature of 181 °F (83 °C).
Vibrant, multicolored extremophilic bacteria in the outflow from Grand Prismatic Spring, Yellowstone National Park
linkView of the vibrant, multicolored extremophilic bacteria in the outflow from Grand Prismatic Spring at the Midway Geyser Basin, Yellowstone National Park. Photo by Elizabeth Mordensky, May 12, 2024.
Vibrant, multicolored extremophilic bacteria in the outflow from Grand Prismatic Spring, Yellowstone National Park
linkView of the vibrant, multicolored extremophilic bacteria in the outflow from Grand Prismatic Spring at the Midway Geyser Basin, Yellowstone National Park. Photo by Elizabeth Mordensky, May 12, 2024.
Yellowstone River valley northeast of Billings from 37,002 feet, Yellowstone County, Montana
Yellowstone River Valley, northeast of Billings, from 37,002 feet, Delta Flight 610, Seattle to Atlanta, Yellowstone County, Montana . Photograph by Alan Cressler, USGS
Yellowstone River Valley, northeast of Billings, from 37,002 feet, Delta Flight 610, Seattle to Atlanta, Yellowstone County, Montana . Photograph by Alan Cressler, USGS
The Yellowstone Volcano: Past, Present and Future
Public Lecture on Yellowstone Volcano by Jake Lowenstern at Menlo Park, CA on January 23, 2014. The Q&A at the end of the talk can be found on the original source video (Source URL).
Public Lecture on Yellowstone Volcano by Jake Lowenstern at Menlo Park, CA on January 23, 2014. The Q&A at the end of the talk can be found on the original source video (Source URL).
Inside USGS No. 1, Robert Christiansen, Yellowstone
USGS emeritus geologist Robert Christiansen describes his career working on Yellowstone geology from the 1960's through 2014. Bob's work along with his USGS colleagues revealed the details of Yellowstone's explosive volcanic past including mapping and dating of past super eruptions 2.1 million years ago, 1.3 million years ago and 640,000 years ago.
USGS emeritus geologist Robert Christiansen describes his career working on Yellowstone geology from the 1960's through 2014. Bob's work along with his USGS colleagues revealed the details of Yellowstone's explosive volcanic past including mapping and dating of past super eruptions 2.1 million years ago, 1.3 million years ago and 640,000 years ago.
Inside USGS, No. 2, Patrick Muffler, Yellowstone
USGS emeritus geologist Patrick Muffler describes his career working on Yellowstone geysers and hydrothermal systems from the 1960's through 2014. Patrick's work along with his USGS colleagues revealed the details of Yellowstone's explosive volcanic past and how its spectacular geysers and other hydrothermal features work.
USGS emeritus geologist Patrick Muffler describes his career working on Yellowstone geysers and hydrothermal systems from the 1960's through 2014. Patrick's work along with his USGS colleagues revealed the details of Yellowstone's explosive volcanic past and how its spectacular geysers and other hydrothermal features work.
Inside USGS, No. 3, Robert Fournier, Yellowstone
USGS emeritus geologist RobertFournier describes his career working on Yellowstone geysers and hydrothermal systems from the 1960's through 2014. Bob's work along with his USGS colleagues revealed the details of Yellowstone's explosive volcanic past and how its spectacular geysers and other hydrothermal features work.
USGS emeritus geologist RobertFournier describes his career working on Yellowstone geysers and hydrothermal systems from the 1960's through 2014. Bob's work along with his USGS colleagues revealed the details of Yellowstone's explosive volcanic past and how its spectacular geysers and other hydrothermal features work.
Lower Falls of the Yellowstone River, Yellowstone National Park, WY
This is nearly the same view depicted in the 1872 sketch by Thomas Moran, and printed for the 150th anniversary commemoration of DOI.
This is nearly the same view depicted in the 1872 sketch by Thomas Moran, and printed for the 150th anniversary commemoration of DOI.
Interpretive reconstruction of the Yellowstone Plateau region before initial plateau volcanism
Interpretive reconstruction of the Yellowstone Plateau region before initial plateau volcanism (a little before 2 million years ago). The region was entirely an elevated and faulted mountainous terrain with no basin in the present plateau area.
Interpretive reconstruction of the Yellowstone Plateau region before initial plateau volcanism (a little before 2 million years ago). The region was entirely an elevated and faulted mountainous terrain with no basin in the present plateau area.
Related
When will the next large earthquake occur in Yellowstone?
Earthquakes cannot be predicted yet, but modern surveillance for earthquakes in Yellowstone conducted with seismographs (instruments that measure earthquake locations and magnitudes) and GPS - Global Positioning Systems (instruments that measure slow ground movements) help scientists understand the state of stress in the Earth's crust. Those stresses could trigger earthquakes as well as magma...
Why are there so many earthquakes at Yellowstone?
Almost all earthquakes at Yellowstone are brittle-failure events caused when rocks break due to crustal stresses. Though we've been looking at Yellowstone for years, no one has yet identified "long-period (LP) events" commonly attributed to magma movement. If LP events are observed, that will NOT mean Yellowstone is getting ready to erupt. LP earthquakes commonly occur at other volcanoes in the...
What is the relationship between volcanism and the geysers and hot springs in Yellowstone?
Heat and volcanic gases from slowly cooling magma rise and warm the dense salty water that occupies fractured rocks above the Yellowstone magma chamber. That brine, in turn, transfers its heat to overlying fresh groundwater which is recharged by rainfall and snowmelt from the surface. Water boiling at depth below the surface is hotter than the temperature of boiling at the surface. If it rises...
How hot is Yellowstone?
Yellowstone is a plateau high in the Rocky Mountains, and is snowbound for over six months per year. The mean annual temperature is 2.2°C (36°F), barely above the freezing point of water. However, Yellowstone is also an active geothermal area with hot springs emerging at ~92°C (~198°F) (the boiling point of water at Yellowstone's mean altitude) and steam vents reported as high as 135°C (275°F)...
How fast is the hotspot moving under Yellowstone?
Actually, the source of the hotspot is more or less stationary at depth within the Earth, and the North America plate moves southwest across it. The average rate of movement of the plate in the Yellowstone area for the last 16.5 million years has been about 4.6 centimeters (1.8 inches) per year. However, if shorter time intervals are analyzed, the plate can be inferred to have moved about 6.1...
Can we use the heat from Yellowstone for energy?
Geothermal energy (heat energy from the Earth's interior) is used to generate electricity in a variety of places throughout the world. Although Yellowstone National Park and its surroundings are a significant geothermal resource, the Park itself is off limits to development. Geothermal developments often cause a decrease in the flow of nearby hot springs and other geothermal features (like geysers...
Abyss Pool, West Thumb Geyser Basin, Yellowstone National Park
Abyss Pool is about 16 m (53 ft) deep and contains alkaline-chloride hydrothermal fluids that in the summer of 2024 had a temperature of 181 °F (83 °C).
Abyss Pool is about 16 m (53 ft) deep and contains alkaline-chloride hydrothermal fluids that in the summer of 2024 had a temperature of 181 °F (83 °C).
Vibrant, multicolored extremophilic bacteria in the outflow from Grand Prismatic Spring, Yellowstone National Park
linkView of the vibrant, multicolored extremophilic bacteria in the outflow from Grand Prismatic Spring at the Midway Geyser Basin, Yellowstone National Park. Photo by Elizabeth Mordensky, May 12, 2024.
Vibrant, multicolored extremophilic bacteria in the outflow from Grand Prismatic Spring, Yellowstone National Park
linkView of the vibrant, multicolored extremophilic bacteria in the outflow from Grand Prismatic Spring at the Midway Geyser Basin, Yellowstone National Park. Photo by Elizabeth Mordensky, May 12, 2024.
Yellowstone River valley northeast of Billings from 37,002 feet, Yellowstone County, Montana
Yellowstone River Valley, northeast of Billings, from 37,002 feet, Delta Flight 610, Seattle to Atlanta, Yellowstone County, Montana . Photograph by Alan Cressler, USGS
Yellowstone River Valley, northeast of Billings, from 37,002 feet, Delta Flight 610, Seattle to Atlanta, Yellowstone County, Montana . Photograph by Alan Cressler, USGS
The Yellowstone Volcano: Past, Present and Future
Public Lecture on Yellowstone Volcano by Jake Lowenstern at Menlo Park, CA on January 23, 2014. The Q&A at the end of the talk can be found on the original source video (Source URL).
Public Lecture on Yellowstone Volcano by Jake Lowenstern at Menlo Park, CA on January 23, 2014. The Q&A at the end of the talk can be found on the original source video (Source URL).
Inside USGS No. 1, Robert Christiansen, Yellowstone
USGS emeritus geologist Robert Christiansen describes his career working on Yellowstone geology from the 1960's through 2014. Bob's work along with his USGS colleagues revealed the details of Yellowstone's explosive volcanic past including mapping and dating of past super eruptions 2.1 million years ago, 1.3 million years ago and 640,000 years ago.
USGS emeritus geologist Robert Christiansen describes his career working on Yellowstone geology from the 1960's through 2014. Bob's work along with his USGS colleagues revealed the details of Yellowstone's explosive volcanic past including mapping and dating of past super eruptions 2.1 million years ago, 1.3 million years ago and 640,000 years ago.
Inside USGS, No. 2, Patrick Muffler, Yellowstone
USGS emeritus geologist Patrick Muffler describes his career working on Yellowstone geysers and hydrothermal systems from the 1960's through 2014. Patrick's work along with his USGS colleagues revealed the details of Yellowstone's explosive volcanic past and how its spectacular geysers and other hydrothermal features work.
USGS emeritus geologist Patrick Muffler describes his career working on Yellowstone geysers and hydrothermal systems from the 1960's through 2014. Patrick's work along with his USGS colleagues revealed the details of Yellowstone's explosive volcanic past and how its spectacular geysers and other hydrothermal features work.
Inside USGS, No. 3, Robert Fournier, Yellowstone
USGS emeritus geologist RobertFournier describes his career working on Yellowstone geysers and hydrothermal systems from the 1960's through 2014. Bob's work along with his USGS colleagues revealed the details of Yellowstone's explosive volcanic past and how its spectacular geysers and other hydrothermal features work.
USGS emeritus geologist RobertFournier describes his career working on Yellowstone geysers and hydrothermal systems from the 1960's through 2014. Bob's work along with his USGS colleagues revealed the details of Yellowstone's explosive volcanic past and how its spectacular geysers and other hydrothermal features work.
Lower Falls of the Yellowstone River, Yellowstone National Park, WY
This is nearly the same view depicted in the 1872 sketch by Thomas Moran, and printed for the 150th anniversary commemoration of DOI.
This is nearly the same view depicted in the 1872 sketch by Thomas Moran, and printed for the 150th anniversary commemoration of DOI.
Interpretive reconstruction of the Yellowstone Plateau region before initial plateau volcanism
Interpretive reconstruction of the Yellowstone Plateau region before initial plateau volcanism (a little before 2 million years ago). The region was entirely an elevated and faulted mountainous terrain with no basin in the present plateau area.
Interpretive reconstruction of the Yellowstone Plateau region before initial plateau volcanism (a little before 2 million years ago). The region was entirely an elevated and faulted mountainous terrain with no basin in the present plateau area.
Updated Date: February 5, 2025