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The lithosphere (which is composed of the crust and solid brittle upper mantle) makes up the Earth's tectonic plates.
This was known as Pangaea.
The average rate of movement of tectonic plates per year is roughly one to two inches. Individual parts of interacting plates can move more than several feet during earthquakes. Over large time spans, tectonic plates can move to all parts of the globe.
Because heat rises from the earth's mantle and creates such pressure that the parts of the crust called tectonic or lithospheric plates move is the reason why earthquakeshappen.
At the margins of colliding tectonic plates.
Tectonic Plates
Movement of tectonic plates which are parts of the Earth's crust.
Nothing, all parts of the earth are moving relative to the other parts.
The lithosphere (which is composed of the crust and solid brittle upper mantle) makes up the Earth's tectonic plates.
This was known as Pangaea.
The average rate of movement of tectonic plates per year is roughly one to two inches. Individual parts of interacting plates can move more than several feet during earthquakes. Over large time spans, tectonic plates can move to all parts of the globe.
Tectonic Plates
Volcanoes are only found on the edge of tectonic plates & they can also be found on cracks in the tectonic plates which is un-common
Oceanic trenches are the gaps which form when the tectonic plates move apart. They are the very deepest parts of the ocean.
Tectonic plates are very large (their highest points form the continents) and constitute the hard crust of the planet. They sit afloat the mantle - molten material called magma - and they are formed from- and return to- magma as parts of the plates are cooled or heated.
Because heat rises from the earth's mantle and creates such pressure that the parts of the crust called tectonic or lithospheric plates move is the reason why earthquakeshappen.
Mt. Erubus has tectonic plates made up of parts of the lithosphere. These plates grind together or pull apart and this causes volcanoes to erupt.