The theory that plates diverge where large columns of hot magma, called hot spots, rise from the lower mantle
The term hot spot is used to describe a very long-lived magma source located deep in the mantle. J. Tuzo Wilson is credited with having originated the concept of hot spots.
A mantle plume is a rising mass of extra hot mantle rock. Mantle plumes are though to be the cause of volcanic activity away from plate boundaries.
A volcano formed by a rising plume of magma that is not located at a plate boundary.
The water evaporates and emerges in a plume of very hot water vapour. An example is the geysers in Yellowstone Park, USA.
Hot Spot
hot spot
Mantle plumes result in the formation of hot spots.
The theory that plates diverge where large columns of hot magma, called hot spots, rise from the lower mantle
The term hot spot is used to describe a very long-lived magma source located deep in the mantle. J. Tuzo Wilson is credited with having originated the concept of hot spots.
A mantle plume is a rising mass of extra hot mantle rock. Mantle plumes are though to be the cause of volcanic activity away from plate boundaries.
of Plume
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
A volcano formed by a rising plume of magma that is not located at a plate boundary.
Deep within the mantle of the planet Earth, there is something very hot, possibly the result of a concentration of radioactive material; this creates a plume of hot magma, which when it reaches the crust, forms volcanoes. Due to continental drift, the location of the plume relative to the crust is slowly shifting, thereby generating a whole chain of volcanoes from a single plume.
A place where hot mantle material rises in a semi-permanent plume, and affects the overlying crust.
A place where hot mantle material rises in a semi-permanent plume, and affects the overlying crust.