mountain ranges
a mountain forms
continental plates meeting form fault lines
convergent boundary
Along their colliding (convergent) boundary.
A convergent boundary between two continental plates causes both plates to crumple to form fold mountains e.g. the HimalayasA convergent boundary between a continental and an oceanic causes one to rise above the other. Granite is less dense than basalt, so the continental plate rises above the oceanic plate. This also forms mountains, like the Andes.
a mountain forms
This is called a convergent boundary, because the two plates are converging, or coming together.
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.
1. Oceanic-oceanic convergent plate boundary. 2. Continental-continental convergent plate boundary. and 3. Oceanic-continental convergent plate boundary.
continental plates meeting form fault lines
convergent plate boundary, subduction. the plates are colliding.
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 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
convergent boundary
Along their colliding (convergent) boundary.
The Himalayas are found at a convergent plate boundary also known as a subduction zone where one plate slips under the other driving the land mass up.
A convergent boundary between two continental plates causes both plates to crumple to form fold mountains e.g. the HimalayasA convergent boundary between a continental and an oceanic causes one to rise above the other. Granite is less dense than basalt, so the continental plate rises above the oceanic plate. This also forms mountains, like the Andes.