The more dense plate subducts (goes under) the less dense plate.
For example if continental and oceanic crust collide oceanic crust will go underneath the continental.
The Indo-Australian Plate is primarily formed by the collision of the Australian Plate and the Indian Plate. This collision is ongoing and has resulted in the uplift of the Himalayas and the Tibetan Plateau.
A convergent boundary is where two plates collide. This can lead to the formation of mountains, earthquakes, and volcanic activity.
The density of the tectonic plates involved determines whether a subduction zone or collision zone is formed at a destructive plate margin. If one plate is denser than the other, it will subduct beneath the other plate, forming a subduction zone. If the plates have similar densities, they will collide and form a collision zone.
A mountain range forms when two of Earth's plates collide. The intense pressure and forces created by the collision push the Earth's crust upwards, creating towering peaks and ranges. Examples include the Himalayas formed by the collision of the Indian Plate and the Eurasian Plate.
A boundary where two plates meet and collide forming mountains is called a convergent boundary. It is also known as destructive plate boundary.
The more dense plate subducts (goes under) the less dense plate. For example if continental and oceanic crust collide oceanic crust will go underneath the continental.
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.
sinks
When two tectonic plates collide, the outcome of which plate comes out on top largely depends on their relative densities and compositions. Generally, the denser oceanic plate tends to subduct beneath the lighter continental plate, leading to the formation of features like ocean trenches and volcanic arcs. In cases where two continental plates collide, neither plate subducts easily, and instead, they can crumple and fold, leading to the creation of mountain ranges. Ultimately, the specific geological circumstances and material properties of the plates involved will dictate the result of the collision.
sinks
sinks
The pacific plate and the cocos plate
Eurasian Plate, African Plate, and Arabian Plate.
Convergent boundary
convergence
The Indo-Australian Plate is primarily formed by the collision of the Australian Plate and the Indian Plate. This collision is ongoing and has resulted in the uplift of the Himalayas and the Tibetan Plateau.
Oceanic plates are denser than continental plates due to their composition, so when they collide, the denser oceanic plate is forced to dive (subduct) beneath the less dense continental plate. This process occurs due to the difference in density between the two types of plates, leading to the oceanic plate sinking into the mantle.