the hot magma moves around and they move.
That would be the theory of plate tectonics.
Tectonic plates move from east to west as a whole due to the coreolis (not sure of spelling) effect.
Tectonic plates interact at plate boundariesThey move apart at divergent boundaries
asthenosphere
Earths crust is made of several large tectonic plates. These plates slowly move in three ways. 2 plates may move along side each other, away from each other or toward each other. if 2 plates of equal density collide it will result in rocks being crumpled upward forming mountains. if one plate has less density then the other then the plate with more density will slide beneath the less dense plate
The lithosphere.
The asthenoshere acts like jello and allows the lithosphere, containing the plate, to move. Tectonic plates could not move without the asthenoshere.
The asthenoshere acts like jello and allows the lithosphere, containing the plate, to move. Tectonic plates could not move without the asthenoshere.
The lithosphere is the layer that moves with the tectonic plates. The lithosphere is made up of the crust and the upper part of the mantle, and it is broken into tectonic plates that move and interact with each other.
tectonic plate
crust
what causes the earths tectonic plates to move
The plates that move are called tectonic plates. The lithosphere is made up of these plates, which consist of both the crust and the upper part of the mantle. These plates float on the semi-fluid asthenosphere below, causing them to move and interact with each other at plate boundaries.
The tectonic plates, part of the lithosphere, move around and float on the top of the asthenosphere.
The asthenosphere is the region of the Earth that is soft and putty-like, located beneath the lithosphere. The asthenosphere allows for the movement of tectonic plates due to its semi-fluid state, which allows the plates to slide and move over it.
The soft layer of the mantle on which the tectonic plates move is called the asthenosphere. It is a semi-fluid layer beneath the lithosphere that allows for the movement of the tectonic plates due to convection currents in the mantle.
The tectonic plates are contained within the lithosphere, which is the outermost mechanical layer of the Earth. The lithosphere comprises the crust and the uppermost part of the mantle and is rigid and brittle, allowing the tectonic plates to move and interact at their boundaries. Beneath the lithosphere lies the asthenosphere, a more ductile layer that facilitates the movement of the tectonic plates above it.