One example is when the Indian Plate crashed into the European plate. As the Indian plate was driven beneath the European plate, the Himalayas was formed and is still increasing in height.
it does not lie on a plte boundary but near the pacific plate
The boundary between the Nazca Plate and the South American Plate is a convergent plate boundary. At this boundary, the oceanic Nazca Plate is subducting beneath the continental South American Plate, leading to geological features such as the Andes mountain range and volcanic activity. This process is associated with intense seismic activity, including earthquakes.
Convergent on the western perimeter, divergent on the Easter perimeter.
A convergent boundary is formed when plates collide. At this type of boundary, the denser plate sinks beneath the less dense plate in a process known as subduction. This collision often results in the formation of mountain ranges, volcanoes, and deep ocean trenches.
It forms a convergent boundary with the South American Plate, divergent.
A convergent plate boundary occurs between the Nazca Plate and the South American Plate. The Nazca Plate is subducting beneath the South American Plate, leading to the formation of the Andes mountain range.
Convergent boundary, which in this case would lead to mountain building (as in the Himalayas)
convergent plate boundary
each plate boundary has a different boundaries. if you want the movement for a specific plate boundary, write the name of the plate boundary. :]
divergent plate boundary
Divergent
it does not lie on a plte boundary but near the pacific plate
divergent boundary
The type of plate boundary closest to England is a convergent boundary. This is where the Eurasian Plate is colliding with the African Plate, resulting in the uplift of the Alps mountain range and causing seismic activity in regions like Italy.
Usually occurs at plate boundary collision areas.
This occurs at a convergent plate boundary and is known as subduction.
shearing work