
Steamboat Geyser erupts on 4 June 2018. Scientists examined how deformation and hydrothermal activity in the northern rim area of the Yellowstone caldera might be linked to magmatic intrusions kilometers beneath the surface.
Yellowstone caldera is a geologic wonderland. It is the source of three of the largest explosive eruptions in the past 3 million years. The caldera itself covers over 1,500 square kilometers (580 square miles) in the northeast corner of Wyoming. As Charles Wicks from the U.S. Geological Survey (USGS) puts it, "Yellowstone's roots seem to extend all the way to the core-mantle boundary. In that dimension, it's a magmatic system of continental scale."
The Yellowstone caldera is packed with geothermal features like geysers, hot springs, mud pots, and geothermal pools. This hydrothermal activity is driven by the vast reservoirs of heat beneath the Yellowstone area, most of which comes from the magma found many kilometers underneath the caldera. All this heat and water mean the land surface at Yellowstone rises and falls frequently, meaning Yellowstone is best described as a "restless caldera."














Comment: For insight into what really happened at the end of the last Ice Age, see: The Seven Destructive Earth Passes of Comet Venus