Not exact matches
University of California, Berkeley, seismologists have produced for the first time a sharp, three - dimensional scan of Earth's interior that conclusively connects plumes of hot rock rising through the mantle
with surface
hotspots that generate
volcanic island chains like Hawaii, Samoa and Iceland.
Senior author Barbara Romanowicz, a UC Berkeley professor of earth and planetary science, noted that the connections between the lower - mantle plumes and the
volcanic hotspots are not direct because the tops of the plumes spread out like the delta of a river as they merge
with the less viscous upper mantle rock.
Slow - moving seismic waves, hotter than surrounding material, interact
with plumes rising from the mantle to affect the formation of
hotspot volcanic islands.
A group of former and current Arizona State University researchers say chemical differences found between rocks samples at
volcanic hotspots around the world can be explained by a model of mantle dynamics that involves plumes, upwellings of abnormally hot rock within the Earth's mantle, that originate in the lower mantle and physically interact
with chemically distinct piles of material.
Washington, DC — Plumes of hot magma from the
volcanic hotspot that formed Réunion Island in the Indian Ocean rise from an unusually primitive source deep beneath the Earth's surface, according to new work in Nature from Carnegie's Bradley Peters, Richard Carlson, and Mary Horan along
with James Day of the Scripps Institution of Oceanography.
The island's volcanism is associated
with the rifting along the Azores Triple Junction; the spread of the crust along the existing faults and fractures has produced many of the active
volcanic and seismic events, [22] while supported by buoyant upwelling in the deeper mantle, some associate
with an Azores
hotspot.