It is called a "convergent boundary".
The place where two plates come together is called a "plate boundary." These boundaries can be classified as convergent, divergent, or transform based on how the plates are moving in relation to each other.
When two continental plates come together, they can form convergent boundaries where one plate is forced beneath the other in a process known as subduction. This can lead to the formation of mountain ranges, earthquakes, and volcanic activity as the plates interact and collide.
When oceanic plates come together, they create a subduction zone where one plate is forced beneath the other. This process forms deep ocean trenches and can lead to the formation of volcanic arcs and islands.
Tectonic plates are separated by "faults," places where the structure of the Earth is cracked. Most earthquakes occur along fault lines.
Tectonic plates come together at convergent boundaries. Some examples include the boundary between the Pacific Plate and the North American Plate along the west coast of the United States, where the plates are converging and creating the Cascade Range of mountains. Another example is the boundary between the Indian Plate and the Eurasian Plate, where the plates are colliding and creating the Himalayas.
The place where tectonic plates come together is named an Destructive Boundary
Converging plates come together. They converge together. Diverging plates come apart.
Converging plates come together. They converge together. Diverging plates come apart.
When two plates come together it's known as the Convergent Boundry
Convergent
Boner.
The plates come together
The plates come together
A convergent boundary is the place where two plates come together.Convergent boundary
The African, Arabian, and Eurasian plates.
call them
colliding boundary