The University of Utah's Hsin - Hua Huang has solved another mystery from Yellowstone, the site of one of the world's
largest supervolcanoes.
Not exact matches
A cross section of the
supervolcano beneath Yellowstone illustrates the previously known magma chamber and the deeper, much
larger magma reservoir discovered through new imaging techniques.
Large - scale eruptions happen roughly on 25 - million - year timescales; a regional
supervolcano could erupt at Yellowstone in the next few thousand.
Yellowstone is one of the
largest remaining active
supervolcanoes.
University of Utah seismologists discovered and made images of a reservoir of hot, partly molten rock 12 to 28 miles beneath the Yellowstone
supervolcano, and it is 4.4 times
larger than the shallower, long - known magma chamber.
The consensus is that several factors are important: atmospheric composition (the concentrations of carbon dioxide, methane); changes in the Earth's orbit around the Sun known as Milankovitch cycles (and possibly the Sun's orbit around the galaxy); the motion of tectonic plates resulting in changes in the relative location and amount of continental and oceanic crust on the Earth's surface, which could affect wind and ocean currents; variations in solar output; the orbital dynamics of the Earth - Moon system; and the impact of relatively
large meteorites, and volcanism including eruptions of
supervolcanoes.
A Ph.D. student from the University of Texas used an innovative method for analyzing deep seismic waves from
large earthquakes to reveal a cylindrical column of hotter - than - normal magma rising from deep below Mexico and surfacing right below the Yellowstone
supervolcano, according to a paper published in Nature Geoscience.