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).
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), so it is questionable whether anyone could get permission to develop geothermal energy in the region outside the park.
There are other natural heat sources in the United States that are being used for geothermal energy. In California, about 4-5 gigawatts of electricity is generated at power plants at The Geysers, Salton Sea, Coso, Casa Diablo, and other geothermal systems. This is enough to provide energy for several million people. There are also geothermal power plants in Nevada and Utah. A geothermal power plant in Hawaii was closed in 2018 due to lava flows from Kilauea volcano.
Learn more:
Related
Can we drill into Yellowstone to stop it from erupting?
How hot is Yellowstone?
What is the relationship between volcanism and the geysers and hot springs in Yellowstone?
What type of eruption will Yellowstone have if it erupts again?
How does an earthquake affect groundwater levels and water quality in wells?
What is groundwater?

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).

Mushroom Pool, in the Lower Geyser Basin of Yellowstone National Park, as it looked in June 23, 1967. The sample that would be the source of Thermus aquaticus strain YT-1 came from this hot spring. Pictured is Thomas Brock standing near the edge of the pool. Image from the self-published "A Scientist in Yellowstone National Park" (Brock, 2017).
Mushroom Pool, in the Lower Geyser Basin of Yellowstone National Park, as it looked in June 23, 1967. The sample that would be the source of Thermus aquaticus strain YT-1 came from this hot spring. Pictured is Thomas Brock standing near the edge of the pool. Image from the self-published "A Scientist in Yellowstone National Park" (Brock, 2017).

eruption of Lone Star Geyser, Yellowstone National Park
eruption of Lone Star Geyser, Yellowstone National Park
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).
A geothermal power plant at The Geysers near Santa Rosa, California. The USGS researches and assesses geothermal resources.
A geothermal power plant at The Geysers near Santa Rosa, California. The USGS researches and assesses geothermal resources.
a discussion of present opportunities and future challenges
by Colin F. Williams, USGS Geophysicist
a discussion of present opportunities and future challenges
by Colin F. Williams, USGS Geophysicist
USGS Scientist-in-Charge of Yellowstone Volcano Observatory, Jake Lowenstern, answers the following questions to explain volcanic features at Yellowstone: "How do we know Yellowstone is a volcano?", "What is a Supervolcano?", "What is a Caldera?","Why are there geysers at Yellowstone?", and "What are the other geologic hazards in Yellowstone?"
USGS Scientist-in-Charge of Yellowstone Volcano Observatory, Jake Lowenstern, answers the following questions to explain volcanic features at Yellowstone: "How do we know Yellowstone is a volcano?", "What is a Supervolcano?", "What is a Caldera?","Why are there geysers at Yellowstone?", and "What are the other geologic hazards in Yellowstone?"
Yellowstone Volcano Observatory 2022 annual report
Yellowstone Volcano Observatory 2020 annual report
Geologic field-trip guide to the volcanic and hydrothermal landscape of the Yellowstone Plateau
Hydrogeology of the Old Faithful area, Yellowstone National Park, Wyoming, and its relevance to natural resources and infrastructure
Steam explosions, earthquakes, and volcanic eruptions -- what's in Yellowstone's future?
Geothermal energy: clean power from the Earth's heat
The Beowawe Geysers, Nevada, before geothermal development
Whistle, a nearly dormant geyser in Upper Geyser Basin, Yellowstone National Park, Wyoming; the first geyser to be studied by research drilling
Related
Can we drill into Yellowstone to stop it from erupting?
How hot is Yellowstone?
What is the relationship between volcanism and the geysers and hot springs in Yellowstone?
What type of eruption will Yellowstone have if it erupts again?
How does an earthquake affect groundwater levels and water quality in wells?
What is groundwater?

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).

Mushroom Pool, in the Lower Geyser Basin of Yellowstone National Park, as it looked in June 23, 1967. The sample that would be the source of Thermus aquaticus strain YT-1 came from this hot spring. Pictured is Thomas Brock standing near the edge of the pool. Image from the self-published "A Scientist in Yellowstone National Park" (Brock, 2017).
Mushroom Pool, in the Lower Geyser Basin of Yellowstone National Park, as it looked in June 23, 1967. The sample that would be the source of Thermus aquaticus strain YT-1 came from this hot spring. Pictured is Thomas Brock standing near the edge of the pool. Image from the self-published "A Scientist in Yellowstone National Park" (Brock, 2017).

eruption of Lone Star Geyser, Yellowstone National Park
eruption of Lone Star Geyser, Yellowstone National Park
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).
A geothermal power plant at The Geysers near Santa Rosa, California. The USGS researches and assesses geothermal resources.
A geothermal power plant at The Geysers near Santa Rosa, California. The USGS researches and assesses geothermal resources.
a discussion of present opportunities and future challenges
by Colin F. Williams, USGS Geophysicist
a discussion of present opportunities and future challenges
by Colin F. Williams, USGS Geophysicist
USGS Scientist-in-Charge of Yellowstone Volcano Observatory, Jake Lowenstern, answers the following questions to explain volcanic features at Yellowstone: "How do we know Yellowstone is a volcano?", "What is a Supervolcano?", "What is a Caldera?","Why are there geysers at Yellowstone?", and "What are the other geologic hazards in Yellowstone?"
USGS Scientist-in-Charge of Yellowstone Volcano Observatory, Jake Lowenstern, answers the following questions to explain volcanic features at Yellowstone: "How do we know Yellowstone is a volcano?", "What is a Supervolcano?", "What is a Caldera?","Why are there geysers at Yellowstone?", and "What are the other geologic hazards in Yellowstone?"