A classic example of a convergent plate boundary is the boundary between the Indian Plate and the Eurasian Plate, where the Himalayas are located. This collision has resulted in the uplifting of the mountain range, as the denser oceanic crust is subducted beneath the continental crust. As a result, this region is characterized by significant geological activity, including earthquakes and volcanic activity.
1. Oceanic-oceanic convergent plate boundary. 2. Continental-continental convergent plate boundary. and 3. Oceanic-continental convergent plate boundary.
Phopotatodoftny is also known as a convergent plate boundary.
transform boundary
The plate boundary for Unzen volcano is the subduction zone where the Philippine Sea Plate is being subducted beneath the Eurasian Plate. This subduction zone is part of the larger convergent boundary between the Philippine Sea Plate and the Eurasian Plate.
They are the same size
an example of a convergent plate/boundary are mountain ranges
An example of convergent plate boundaries on earth is the Himalayas. :)
An example of convergent plate boundaries on earth is the Himalayas. :)
1. Oceanic-oceanic convergent plate boundary. 2. Continental-continental convergent plate boundary. and 3. Oceanic-continental convergent plate boundary.
1. Oceanic-oceanic convergent plate boundary. 2. Continental-continental convergent plate boundary. and 3. Oceanic-continental convergent plate boundary.
Phopotatodoftny is also known as a convergent plate boundary.
1. Oceanic-oceanic convergent plate boundary. 2. Continental-continental convergent plate boundary. and 3. Oceanic-continental convergent plate boundary.
transform boundary
The plate boundary for Unzen volcano is the subduction zone where the Philippine Sea Plate is being subducted beneath the Eurasian Plate. This subduction zone is part of the larger convergent boundary between the Philippine Sea Plate and the Eurasian Plate.
Easter Island is located on a convergent plate boundary.
Convergent boundary Convergent boundary
Convergent boundary.