Orogeny is the process of mountain creation, or a period of mountain creation.
Plateaus and most mountains are created by uplift.
uplift
Mountains are uplifted as tectonic plates smash into each other or magma rises up from under volcanoes.
Uplift is the process in which structural highs are created (e.g. mountains). Tectonism is largely responsible for uplift.
The Andes mountains and the islands of Japan are both formed by subduction zones which was caused by volcanoes. The Himalayas were formed by convergent plate boundaries but no subduction zone. Instead the plates collided and there was uplift causing the mountains.
Structural highs (e.g. mountains) are created by uplift. The uplifted rocks are commonly heavily folded and faulted as a result of uplift.
Mountains
Mountains are caused by the uplift of landmasses either by volcanic action or by continental plates colliding.
The Andes mountains and the islands of Japan are both formed by subduction zones which was caused by volcanoes. The Himalayas were formed by convergent plate boundaries but no subduction zone. Instead the plates collided and there was uplift causing the mountains.
The Andes mountains and the islands of Japan are both formed by subduction zones which was caused by volcanoes. The Himalayas were formed by convergent plate boundaries but no subduction zone. Instead the plates collided and there was uplift causing the mountains.
Uplift is when things like mountains, hills, and, plateaus are created. Subsidence is the opposite of thins, like when sink holes and valleys are made.
Uplift and subsequent erosion