they are moving south and west at the same time
The Indian plate is moving northward at a rate of about 5 centimeters per year relative to the Eurasian plate, which it is colliding with. This tectonic movement has led to the formation of the Himalayas and continues to impact the geology and geography of the region.
The North American plate is moving very slowly, only about one inch per year. Other tectonic plates are moving much faster; up to eight or nine inches per year.
Mount. Merapi is on the Sunda Plate, which forms a convergent margin with the Indian-Australian Plate
The South American plate is moving at a rate of about 2.5 centimeters per year in a generally westward direction. This is considered a relatively slow rate compared to some other tectonic plates on Earth.
The North American Plate moves at a speed of approximately 2.3 to 4.7 centimeters per year. It is a relatively slow-moving tectonic plate compared to others around the world.
The speed at which tectonic plates move is relatively constant over long time scales, so they are not moving faster right now compared to the past. However, the rates of plate movement vary depending on the plate boundary type and geological forces acting on them.
It is moving at 4.65 cm per year
Australia moves at a speed of approximately 6.8 centimeters per year to the northeast due to the movement of the tectonic plate it sits on. This movement is part of the larger process of plate tectonics where continents drift slowly over the Earth's surface.
It moves extremely slowly as do all the plates
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.
fast moving
Africa is moving northward at a rate of about 2.5 cm per year relative to the Eurasian Plate due to plate tectonics. This movement is driven by the spreading of the Atlantic Ocean, causing Africa to drift away from South America.