Not all scientists are convinced that
deep mantle plumes can propel tectonic plates, or are responsible for hot spots areas of unusually high volcanic activity such as the one under Réunion island.
«For the scientists who do not believe hot spots like Réunion are due to
deep mantle plumes, this should be a challenge.»
They slow down the seismic waves caused by earthquakes and may be the culprit for
deep mantle plumes, which can lead to volcanic hotspots like those that created Yellowstone National Park or the Hawai'ian Islands.
Not exact matches
Scientists studying volcanic hotspots have strong evidence of this, finding high helium - 3 relative to helium - 4 in some
plumes, the upwellings from Earth's
deep mantle.
Iceland is also where scientists have long debated whether a
mantle plume — a vertical jet of hot rock originating from
deep inside Earth — intersects the mid-ocean ridge.
The Hawaii research relies on a new seismic technique for detecting aligned flows of rock that has yet to be verified, says marine geophysicist Cecily Wolfe of the Woods Hole Oceanographic Institution in Massachusetts and the Carnegie Institution of Washington, D.C.. However, the Iceland study is «very clear and compelling,» she says, and consistent with a
deep mantle origin for the
plume.
Since the island «birth order» moves from east to west, the Canaries must have formed as the continental plate drifted eastward over a stationary, periodically erupting
plume of hot magma
deep in Earth's
mantle.
One of the most contentious debates in geoscience has centred on whether piles of rock in the
deep mantle — to which
plumes are anchored — have remained stationary, unaffected by
mantle flow over hundreds of millions of years.
These
plumes of hot rock welling up from
deep in the
mantle are a key link in the plate - tectonic cycle.
The magma comes from within the upper 200 kilometers of the
mantle and not thousands of kilometers
deep, as the
mantle -
plume theory suggests.
Since the 1970s, geologists have theorized that the Hawaiian Islands formed from magma generated by a hot, rising
deep -
mantle formation known as a
plume.
«For the first time we could obtain images of the
deeper crustal structure in the region where the Walvis Ridge joins the African continent, in order to study the impact of a
mantle plume» explains Trond Ryberg from GFZ.
It is commonly assumed that enormous masses of magma ascended from the
deep mantle up to higher levels, and that this hot
mantle plume (the Tristan
mantle plume) weakened the continental lithosphere, eventually causing the break - up of the continental plate of Gondwana.
«This new constraint on
plume structure has important implications for how
deep mantle material is entrained in
plumes, and it gives us the clearest picture yet for the chemical structure of an upwelling
mantle plume.»
«This is consistent with the idea of a relatively
deep - seated
mantle plume,» she said.
That indicates the
plume comes from a relatively
deep source, though the data doesn't allow the team to peer
deeper into the
mantle, near the core.
Peter Nelson is a fourth - year doctoral student in the Jackson School of Geosciences at the University of Texas at Austin and co-author of the new paper, which provides the first convincing evidence of a
deep -
mantle plume beneath Yellowstone.
But despite widespread acceptance of the
deep plume theory, geoscientists have failed to produce seismic imaging of just such a mushroom - shaped
plume extending 3,000 kilometers down to the core -
mantle boundary.
According to the NASA press release, the study «adds evidence that a geothermal heat source called a
mantle plume lies
deep below Antarctic Marie Byrd Land, explaining some of the melting that creates lakes and rivers under the ice sheet.»
A new NASA study adds evidence that a geothermal heat source called a
mantle plume lies
deep below Antarctica's Marie Byrd Land, explaining some of the melting that creates lakes and rivers under the ice sheet.