This depends at what point on Earth's surface you are interested in!
For example the Mid Atlantic Ridge separating the North American and Eurasian plates is classified as a "slow" spreading centre with a spreading rate of around 25mm/yr (slow spreading centres generally have a rate of between 20-55 mm per year). This means that the North American plate is moving roughly to the west at a rate of 12.5 mm/yr.
However a number of the spreading centres in the Pacific are considered to be "medium to fast" spreading centres with rates of between 80-120 mm/yr.
Another example is the Indian plate which is moving north-east at a rate of approximately 50mm/yr causing it to collide with the more slowly moving Eurasian plate. This event started (and is continuing to cause) the Himalayan orogeny.
vertical direction
in may affect the internal energy of the earth,also shaking of the earth's crust (earth quake) due to the movement of molten materials in interior of the crust
An earthquake
A place where two tectonic plates meet is a fracture in the Earth.
On geologic time scales, new oceanic crust is constantly being formed ad mid-ocean ridges while older crust is destroyed at subduction zones. The crust forms at the ridge and is carried away by the movement of the plate as new crust forms to take its place. The oceanic crust is youngest new a mid ocean ridge and oldest far away from it.
The tectonic plates of Earth's crust are always moving, but the movement is far too slow to be perceived without sensitive measuring equipment. For example, the northward movement of India at the rate of two inches per year is considered fast. Usually the only times we perceive the movement of Earth's crust are when part of a tectonic plate gets stuck, and the movement of the rest of the plate causes potential energy to build up in the stuck part until it has enough energy to free itself and catch up with the rest of the plate. That is how most earthquakes happen.
The sudden movement of the earth's crust is called and earthquake
Plate tectonic movement and subduction zones.
the movement of earths plates or crust
The movement of magma through the Earth's crust is known as intrusion.
earthquake/fissure
The movement of the crust along a thrust fault is usually a reverse movement unlike the movement along a normal fault.
The movement of the crust along a thrust fault is usually a reverse movement unlike the movement along a normal fault.
a few cent. per year...
The four factors that effect plate movement are when new crust is created, crust being destroyed, the crust sliding horizontally or when plates merge together.
earthquakes
oceanic crust is much more dense than continental crust. Oceanic crust is also responsible for the movement of continental crust.