© University of Utah/ScienceThis activity is typically linked to changes in magma and gases deep beneath the surface – but for now, the experts say there’s no cause for worry. The Grand Prismatic hot spring (pictured, stock image) is among the park's many hydrothermal features created by the supervolcano.
A new map from the US Geological Survey shows how the ground around the Yellowstone caldera has deformed over the span of two years, as the quakes release uplift-causing pressure, allowing the ground to sink back down.
This activity is typically linked to changes in magma and gases deep below the surface - but for now, the experts say there's no cause for worry.
The map, created by USGS geophysicist Chuck Wicks uses data from June 2015 and July 2017 to show how the region around Yellowstone has changed.
In the map, the colourful rings show the changes in the ground's elevation as seen by a radar satellite, according to USGS.
A bulls-eye shaped section of uplift can be seen at the Norris Geyser Basin, where the ground has risen roughly 3 inches.
