What are three types of convergent boundaries subduction?
There are three types of convergent plate boundaries: oceanic-oceanic boundaries, oceanic-continental boundaries, and continental-continental boundaries.
What is a convergent boundary with subduction?
A convergent boundary (also known as a destructive boundary) is an area on Earth where two or more lithospheric plates collide. One plate eventually slides beneath the other, a process known as subduction. The geologic features related to convergent boundaries vary depending on crust types.
What are the three 3 types of plate boundaries and differentiate from each other?
Tectonic Plates and Plate Boundaries
- There are three main types of plate boundaries:
- Convergent boundaries: where two plates are colliding.
- Divergent boundaries – where two plates are moving apart.
- Transform boundaries – where plates slide passed each other.
Which two types of convergent have subduction?
Three Types of Convergent Boundaries
- Oceanic/Oceanic Convergent Boundaries. Where different oceanic plates run into each other, the older – and therefore cooler and denser – one dives beneath the other; in other words, it subducts.
- Oceanic/Continental Convergent Boundaries.
- Continental/Continental Convergent Boundaries.
What are the three types of convergent plate boundaries quizlet?
How will you identify the 3 types of plate boundaries?
Divergent boundaries: where new crust is generated as the plates pull away from each other. Convergent boundaries: where crust is destroyed as one plate dives under another. Transform boundaries: where crust is neither produced nor destroyed as the plates slide horizontally past each other.