Will the Yellowstone magma chamber--make that chambers--ever stop growing? Well, they're not actually growing per se; rather, scientists are discovering that Yellowstone's magma chambers are bigger--and more numerous--than previously believed. In 2013, the upper magma chamber was revealed to be more than double its previously estimated volume. Then, this month, geophysicists announced the existence of an additional, deeper, larger magma reservoir sitting between the upper chamber and the mantle plume feeding the legendary volcano. Check out the video below, by the University of Utah, to see a 3D animation of the setup. You can read more about Yellowstone eruptions in my previous post, which has been updated. Read more
Yellowstone magma: a new chamber, bigger and deeper
Cortney Science & Technology + yellowstone
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Volcano news: how slopes affect lava flows, challenge to traditional volcano model, Mauna Loa waking up
Cortney Science & Technology + geology, hawaii, lava flows, rift zones, volcanoes, yellowstone
The summer of 2014 has been an exciting one for volcano science!
Yellowstone volcanism: the three big eruptions
Cortney Science & Technology + geology, igneous, volcanoes, yellowstone
The Yellowstone Supervolcano, fed by a continental hotspot, has erupted many times over its 70 million year history, but three eruptions blanked the continent. Today, the sponge-like upper magma chamber is 80 km by 20 km, or 4,000 km3 by volume, of which 8% is molten; another deeper and larger magma reservoir, 46,000 km3 by volume, of which 2% is molten, lays 65 km beneath the ground. Despite its deceptive beauty, Yellowstone is an active volcano (perhaps most obviously evidenced by its frequent earthquakes) that will violently erupt at some point in the future. Read more →