The mantle is the Earth's crust. Mantle dynamics are caused by the heating and cooling of this layer of crust. This heating and cooling causes a slow creeping motion in the Earth's rocky mantle.
Heat from the core and the mantle itself causes convection currents in earth's mantle.
The crust stretches and gets thinner so the pressure decreases on the mantle rocks below this causes part of the mantle to melt
The crust stretches and gets thinner so the pressure decreases on the mantle rocks below this causes part of the mantle to melt
Mantle convection causes the tectonic plates of the Earth to move slowly. Mantle convection is when heat moves from the mantle to the surface and causes the mantle, and the tectonic plates to move very slowly.
The weight of the rocks in the crust and upper mantle.
Heat from the core and the mantle itself causes convection currents in earth's mantle.
The crust stretches and gets thinner so the pressure decreases on the mantle rocks below this causes part of the mantle to melt
The crust stretches and gets thinner so the pressure decreases on the mantle rocks below this causes part of the mantle to melt
Mantle convection causes the tectonic plates of the Earth to move slowly. Mantle convection is when heat moves from the mantle to the surface and causes the mantle, and the tectonic plates to move very slowly.
irriversible
The weight of the rocks in the crust and upper mantle.
Auther Holmes is the Scientist who first proposed that theral convection in the mantle causes continental drift.
Auther Holmes is the Scientist who first proposed that theral convection in the mantle causes continental drift.
convection currents
Convection currents in the mantle.
Pressure and extreme heat.
Convection currents in the mantle are what causes tectonic plates to move. Uneven heating of the mantle results from radioactive decay of some long-lived isotopes in the mantle, which are not evenly distributed.