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Columns of hot rock rising through Earth's mantle are called mantle plumes. These plumes originate near the core-mantle boundary and can cause volcanic activity on the Earth's surface when they reach the crust, creating features like hotspot volcanoes.
Plumes of molten rock originating deep within the mantle are known as mantle plumes. These plumes are believed to be responsible for hotspots and volcanic activity at the Earth's surface.
Mantle plumes. These are hot upwellings of magma from the Earth's mantle that can cause volcanic activity on the surface, such as hotspot volcanoes like those in Hawaii.
The phenomenon described is known as mantle plumes. They are thought to be responsible for volcanic hotspots such as Hawaii and Iceland due to the upwelling material creating magma and forming volcanoes as it reaches the Earth's surface.
A mantle plume is a column of hot rock rising from deep within the Earth's mantle to the surface. These plumes can cause volcanic activity and create features like hotspots and mid-ocean ridges. Mantle plumes are thought to be responsible for some of the most significant geological phenomena on Earth.
Confirmation of the existence of mantle plumes can be supported by evidence such as hotspots causing volcanic activity not associated with plate boundaries, geochemical signatures in volcanic rocks consistent with deep mantle sources, and seismic tomography revealing vertical conduits of hot material rising from deep within the mantle.
Mantle plumes
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A hot plume of mantle material, which may extend to extend to the core-mantle boundary, produces a(n) a volcanic region a few hundred kilometers across
Melted rock in the mantle will rise when it becomes less dense than the surrounding solid rock and forms buoyant plumes. This can be triggered by heat sources such as mantle plumes or subduction zones.
Convection currents rese and sink through the mantle and the liquid outer core. In Earth's mantle, large amounts of heat are transferred by convection currents. Heat from the core and the mantle itself causes convection currents in the mantle.
It is on the edge not very close by the mantle plumes