mountain ranges
convergent boundary
Both Plates are pushed upwards and rocks are folded and faulted to form mountain ranges. For Example this occurred in Europe when the Eurasian and African plates collided to form the Alps. And a Subduction zone is formed when a continental and Oceanic plates collide as the oceanic plate is forced downwards into the mantle.
A convergent boundary that does not have a subduction zone is a continental-continental convergent boundary. At this type of boundary, two continental plates collide and crumple, leading to the formation of mountain ranges, such as the Himalayas. Since both plates are buoyant and primarily composed of continental crust, neither plate is forced beneath the other, unlike in oceanic-continental or oceanic-oceanic boundaries.
Along their colliding (convergent) boundary.
When continental plates move toward each other, it is called a convergent plate boundary. This can lead to the collision and subduction of the plates, causing mountain building and deep ocean trench formation.
1. Oceanic-oceanic convergent plate boundary. 2. Continental-continental convergent plate boundary. and 3. Oceanic-continental convergent plate boundary.
The movement or action of the plate determines what type it is. When two plates collide, they are creating a convergent boundary. Therefore you could state that they are convergent (or colliding) tectonic plates.
The categories are a continental and a continental plate colliding, continental and oceanic plates colliding, and oceanic and oceanic plates colliding. The two continental plates form mountains. The continental and oceanic plated colliding cause subduction zones and volcanoes. Oceanic and oceanic plates colliding form a trench.
The Mariana Trench is a convergent boundary, where two tectonic plates are colliding and one plate is forced beneath the other.
At a convergent boundary, two lithospheric plates are colliding. This collision can involve oceanic lithosphere converging with either oceanic or continental lithosphere, or continental lithosphere converging with continental lithosphere. The type of lithosphere involved in the collision influences the resulting geological features, such as subduction zones or mountain ranges.
convergent boundary
Both Plates are pushed upwards and rocks are folded and faulted to form mountain ranges. For Example this occurred in Europe when the Eurasian and African plates collided to form the Alps. And a Subduction zone is formed when a continental and Oceanic plates collide as the oceanic plate is forced downwards into the mantle.
Along their colliding (convergent) boundary.
The Cascade Mountains are a volcanic mountain range located in the western United States. They are considered to be a convergent boundary, where two tectonic plates are colliding.
This is called a convergent boundary, because the two plates are converging, or coming together.
The three types of convergent boundaries are when two plates meet and two oceanic plate meet, or where an oceanic and continental plate meet.the three types of convergent boundaries are continent boundaries , continent - ocean boundaries, and last but not least............. ocean boundaries
When continental plates move toward each other, it is called a convergent plate boundary. This can lead to the collision and subduction of the plates, causing mountain building and deep ocean trench formation.