A continental-continental plate boundary is typically associated with the formation of mountain ranges due to the collision of two continental plates. This collision results in intense compression, leading to uplift and the creation of features like fold mountains. An example of this type of boundary is the Himalayas, formed by the collision of the Indian and Eurasian plates. Additionally, earthquakes are common in these regions due to the stress and strain generated by the tectonic interactions.
Mountain formation is a feature associated with a continental plate boundary, where the collision of two continental plates results in the uplift of the Earth's crust, creating mountain ranges such as the Himalayas.
1. Oceanic-oceanic convergent plate boundary. 2. Continental-continental convergent plate boundary. and 3. Oceanic-continental convergent plate boundary.
A Collision plate boundary, where two continental plates that are the same in density and thickness, push against each other forming fold mountains and crumble zones. This causes Earthquakes from the pressure and stress but not volcanoes.
Convergent plate boundaries.
A deep ocean trench is commonly formed at a plate boundary where oceanic crust converges with continental crust. The oceanic crust is denser and is forced beneath the lighter continental crust, creating a deep trench.
Mountain formation is a feature associated with a continental plate boundary, where the collision of two continental plates results in the uplift of the Earth's crust, creating mountain ranges such as 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.
The Himalayas and the Tibetan Plateau are formed by a continental-continental boundary where the Indian continental plate is moving north against the Eurasian continental plate.
1. Oceanic-oceanic convergent plate boundary. 2. Continental-continental convergent plate boundary. and 3. Oceanic-continental convergent plate boundary.
Mt. Fuji is located in Japan. It is near a continental convergent boundary, a continental transform boundary, and an oceanic transform boundary.
continental plate? divergent boundary? convergent boundary? continental drift?
No. It subducts under the continental plate.
The three types of convergent boundaries are oceanic-oceanic plate boundary (e.g. Japan Trench), oceanic-continental plate boundary (e.g. Andes Mountains), and continental-continental plate boundary (e.g. Himalayas).
either a continental plate divergent boundary convergent boundary or a continental drift lol
Convergent plate boundaries.
A Collision plate boundary, where two continental plates that are the same in density and thickness, push against each other forming fold mountains and crumble zones. This causes Earthquakes from the pressure and stress but not volcanoes.