Convergent plate boundaries.
continental slope
When continental crust collides with the same type of crust, it can result in the formation of mountain ranges through a process called continental collision. The force of the collision forces the crust to crumple and buckle, leading to the uplift of land and the creation of large mountain belts. An example of this process is the collision between the Indian Plate and the Eurasian Plate, which formed the Himalayan mountain range.
Yes. It is a convergent boundary where both masses consist of continental crust.
Yes, the continental slope descends steeply from the continental shelf into the deep ocean floor. It marks the boundary between the continental crust and the oceanic crust.
This is called a destructive plate boundary. It occurs due to the fact that the oceanic crust is far denser than the continental crust. As a result it subducts into the mantle and is incenerated. Hope it helped:)
tides will occur.
The boundary between continental crust and oceanic crust occurs at the base of the lithosphere. This boundary is known as the Mohorovičić discontinuity, or Moho. It separates the less dense continental crust from the more dense oceanic crust below.
Crust is destroyed at the convergent plate boundary. This is usually between the oceanic and continental plates. This is where subduction of the more dense crust occurs.
Trench
When continental crust collides with continental crust, it can form large mountain ranges through a process called continental collision. This collision causes the crust to fold and thrust upwards, leading to the formation of extensive mountain systems like the Himalayas.
tides will occur.
it subducts underneath the crustal plate
The boundary between the oceanic crust and continental crust is known as the continental shelf. This is the shallowest part of the ocean that extends from the shore to the continental slope.
continental slope
continental slope
The portion of the continental margin that serves as a boundary between the oceanic crust and the continental crust is called the continental shelf. This is the shallowest part of the margin, located between the shoreline and the continental slope.
The two types of Crust is the Continental Crust and the Oceanic Crust.