Intraplate volcanism is volcanism that takes place away from the margins of tectonic plates. Most volcanic activity takes place on plate margins, and there is broad consensus among geologists that this activity is explained well by the theory of plate tectonics. However, the origins of volcanic activity within plates remains controversial.
- 1 Mechanisms
- 1.1 Plume model
- 1.2 Plate theory
- 1.3 The impact hypothesis
- 1.4 Comparison of the hypotheses
- 2 See also
- 3 References
- 4 Further reading
- 5 External links
Mechanisms that have been proposed to explain intraplate volcanism include mantle plumes; non-rigid motion within tectonic plates (the plate model); and impact events. It is likely that different mechanisms accounts for different cases of interplate volcanism.
Plume modelA superplume generated by cooling processes in the mantle (LVZ=low-velocity zone)
A mantle plume is a proposed mechanism of convection of abnormally hot rock within the Earth's mantle. Because the plume head partly melts on reaching shallow depths, a plume is often invoked as the cause of volcanic hotspots, such as Hawaii or Iceland, and large igneous provinces such as the Deccan and Siberian traps. Some such volcanic regions lie far from tectonic plate boundaries, wh... ...read more