Mountain buildup.
Fault ... ;)
When tectonic plates collide, they can form various geological features depending on the nature of the collision. If two continental plates converge, they can create mountain ranges, such as the Himalayas. When an oceanic plate collides with a continental plate, it can lead to subduction, forming deep ocean trenches and volcanic arcs. Additionally, the collision of two oceanic plates can result in island arcs.
When continental plates collide they form high mountains.
When two continental plates collide,fold mountains are formed.
When two tectonic plates collide, it can result in the formation of mountain ranges due to the intense pressure and folding of the Earth's crust. This process is known as continental collision and can lead to the creation of complex geological features, such as fold mountains and faults, as the plates push against each other.
Both oceanic-oceanic and continental-continental convergent boundaries involve the collision of tectonic plates, leading to geological features such as mountains and earthquakes. In oceanic-oceanic convergence, one oceanic plate subducts beneath another, often creating deep ocean trenches and volcanic island arcs. In contrast, continental-continental convergence occurs when two continental plates collide, resulting in the formation of extensive mountain ranges, like the Himalayas, without significant subduction. The main difference lies in the types of plates involved and the resulting geological features.
Fault
Mountains
Collision...
When two tectonic plates collide, it can form various geological features such as mountain ranges, earthquakes, and volcanic activity. The specific features that form depend on the types of plates involved and the specific boundaries at the collision zone.
Earthquake
sinks