The boundary between the Eurasian Plate and the Indian Plate at the Himalayas
The boundary between the Nazca Plate and the South American Plate along the west coast of South America
Divergentboundary
Two plates that are moving apart from each other
Divergent boundaries
The boundary between the African Plate and the Arabian Plate in the Red Sea
The boundary between the Pacific and Antarctic Plates
The Mid-Atlantic Ridge, made up of the boundary between the North American and Eurasian Plates in the North Atlantic, crossing Iceland, and the South American and the African Plates in the South Atlantic
Transform boundary
Two plates slide past each other
Transform plate boundaries
The boundary between the Pacific Plate and the Australian Plate, crossing New Zealand
The boundary between the Pacific Plate and the North American Plate in California
The rock making up continental plates is generally lighter and less dense than oceanic rock, so it is too light to get pulled under the earth and turned into magma
A collision between two continentalplates crunches and folds the rock at the boundary, lifting it up and leading to the formation of mountains and mountain ranges
The denser oceanic crust undergoes subduction, where it bends and is pulled under the continental crust
This leads to the formation of a volcanic arc near the edge of the continental leading plate
Volcanic arc
An arc-shaped chain of volcanoes formed above a subduction zone
Trench
A steep-sided depression in the ocean floor
Subduction zone
The area where one plate is being pulled under the edge of another
Oceanic crust
The earth's crust found underneath the oceans
Volcano
A vent in the earth's surface through which magma and gases erupt
The world's deepest parts of the ocean are found along trenches, e.g. The Mariana Trench is 11 km deep
Underwater earthquakes, especially the stronger ones, can generate tsunamis, which are a series of ocean waves with very long wavelengths caused by large-scale disturbances of the ocean
When two oceanic plates collide, trenches are formed, which become the sources of earthquakes
The leading edge of the subducted plate will eventually reach the mantle, causing it to melt and turn into magma, which will rise to the surface creating an island arc parallel to the trench