Yellowstone magma is primarily composed of silicate minerals, predominantly andesitic to rhyolitic in composition. It contains high levels of silica, which contributes to its viscous nature. Additionally, the magma contains various gases, such as water vapor, carbon dioxide, and sulfur dioxide, which can significantly influence volcanic activity and eruptions. The unique composition of Yellowstone's magma is influenced by the underlying hot spot and the melting of the Earth's crust.
The Yellowstone caldera.
the role of asthenosphere in magma generetion
The magma is primarily granitic/rhyolitic, but there are occasional basaltic lava flows.
1550 km
magma type\
The magma in the earth had to go somewhere and it has accumulated around the Yellowstone area for many thousands of years.
It is an acidic magma and has a huge caldera.
The Yellowstone caldera is a supervolcano located in Yellowstone National Park. While it is an active volcanic system, there is no current indication that it is about to erupt. The USGS monitors Yellowstone closely, and any signs of increased volcanic activity would be detected well in advance.
Yellowstone's last magma eruption was about 70,000 years ago. The last super eruption was approximately 640,000 years ago.
A few miles under Yellowstone is an enormous magma chamber associated with a supervolcano.
The heat for Yellowstone's geysers comes from magma beneath the Earth's surface. This magma heats up the water in underground reservoirs, creating pockets of steam that eventually erupt through geysers.
A magma chamber.