west
Cocos Plate is moving towards the north-east.
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 Juan De Fuca Plate is moving eastward and subducting beneath the North American Plate along the Cascadia Subduction Zone.
The North American plate is moving westward at a speed of about 2.3 centimeters per year. This movement is primarily driven by the underlying mantle convection currents and the interactions with neighboring plates along plate boundaries.
north-northwest
Cocos Plate is moving towards the north-east.
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 South American Plate.
roughly southwest
It is moving to the west. As is the north American plate which will make the Atlantic Ocean bigger and the Pacific ocean smaller.
The South American plate primarily moves in a westward direction at a rate of a few centimeters per year. This movement is generally in a direction that is away from the Mid-Atlantic Ridge, where the plate is being formed.
It moves extremely slowly as do all the plates
The Nazca plate is moving southeast towards the South American plate, which is less dense, therefore causing the Nazca plate to be driven under the South American plate at about 77mm per year. The collision of these plates is responsible for lifting the massive Andes Mountains and causing the volcanoes which are strewn throughout them.
The Pacific Plate is currently being subducted under the North American Plate. Subduction zones are when one plate is being forced under another at a convergent boundary (where two plates collide). When the Pacific Plate is being subducted under the North American Plate, the crust of the Pacific Plate melts, and creates volcanoes along the edge of the North American Plate. So, the relative motion of the two plates is that they are converging, or moving together.This same process is happening at the South American and Nazca Plates.
The Juan De Fuca Plate is moving eastward and subducting beneath the North American Plate along the Cascadia Subduction Zone.
So the direction and speed of plate motion is measured with the assumption that the Africa plate is stationary. Using this standard North and South America is moving west away from Africa.
The North American Plate is moving away from the Eurasian Plate in the north and the South American Plate in the south. This movement primarily occurs along the Mid-Atlantic Ridge, where new oceanic crust is formed as magma rises from the mantle. Additionally, the North American Plate is also diverging from the Pacific Plate along the San Andreas Fault in the west.