Plume tectonics
Encyclopedia
Plume tectonics is a geophysical theory that finds its roots in the mantle doming concept (which did not accept major plate movements and continental drifting) which was especially popular during the 1930s, and survived throughout the seventies up till today in various forms and presentations. It has slowly evolved into a concept that recognises and accepts large scale plate motions such as envisaged by plate tectonics
Plate tectonics
Plate tectonics is a scientific theory that describes the large scale motions of Earth's lithosphere...

, but placing them in a framework where large mantle plume
Mantle plume
A mantle plume is a hypothetical thermal diapir of abnormally hot rock that nucleates at the core-mantle boundary and rises through the Earth's mantle. Such plumes were invoked in 1971 to explain volcanic regions that were not thought to be explicable by the then-new theory of plate tectonics. Some...

s are the major driving force of the system.

The theory focuses on the movements of postulated mantle plumes under tectonic plates viewing them as the major driving force of movements of (parts of) the Earth's crust. It tries to reconcile in one single geodynamic model the horizontalistic concept of Plate tectonics, and the verticalistic concepts of mantle plumes and hot spots
Hotspot (geology)
The places known as hotspots or hot spots in geology are volcanic regions thought to be fed by underlying mantle that is anomalously hot compared with the mantle elsewhere. They may be on, near to, or far from tectonic plate boundaries. There are two hypotheses to explain them...

, together with the existence of various super continents in Earth history. This theory has little support in mainstream geology. More plausible is the view that mantle plumes do not make an appreciable contribution to plate motions, or to volcanism on Earth's surface.

See also

  • Hotspot (geology)
    Hotspot (geology)
    The places known as hotspots or hot spots in geology are volcanic regions thought to be fed by underlying mantle that is anomalously hot compared with the mantle elsewhere. They may be on, near to, or far from tectonic plate boundaries. There are two hypotheses to explain them...

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