Like a jiggsaw puzzel, the Earth's crust is broken up into tectonic plates that move. When they colide they create what we call an EARTHQUAKE .
they move against one another
The earth's crust moves because the earth has tectonic plates that move because the magma under the earth's surface is constantly boiling. Since the water moves, it causes the earth's crust to move.
scientist thought someone moved it
One of the way is they move towards each other and converge,or collide
as the plates move towards each other the denser plate subducts into the asthenphere
No the can’t
At the edge of tectionic plates
Tectonic plates are large sections of the Earth's lithosphere that float on the semi-fluid asthenosphere underneath. These plates constantly move and interact with each other, causing various geological phenomena like earthquakes, volcanic activity, and mountain formation. The theory of plate tectonics explains how these movements shape the Earth's surface over long periods of time.
Plates at our planet's surface move because of the intense heat in the Earth's core that causes molten rock in the mantle layer to move. It moves in a pattern called a convection cell that forms when warm material rises, cools, and eventually sink down. As the cooled material sinks down, it is warmed and rises again.
Plates move apart on divergent plate boundaries.
No, tectonic plates move at different rates. Some plates move faster than others, while some plates move very slowly. The movement of the plates is driven by the underlying convection currents in the Earth's mantle.
the ocean plates move because of the movement of the the tectonic plates beneath the ocean and do to the motion of the oceans currents.
tectonic plates
No(see the explanation of the question "Why do the tectonic plates move?"
A convergent boundary is where plates move together.
they both form or happen from plate tectionic
When convection currents sink near the mantle, they create drag on the lithospheric plates above. This drag causes the plates to move in the direction of the sinking current. As the plates move, they can interact with other plates, leading to processes like subduction or mountain formation.