Mountains form along convergent boundaries when 2 plates collide. These are also called colliding boundaries.
The Alps, Urals, and Appalachians are examples of fold mountains, which form due to tectonic plate movement and the folding of rock layers over time.
Folding, bending, and cracking of the earth's crust due to plate movement can result in the formation of mountains, earthquakes, and volcanic activity. This process is known as tectonic activity and is responsible for shaping the Earth's surface over millions of years.
convergent plate boundaries
Mountains can form at non-plate boundaries due to processes like hot spot volcanism or tectonic activity within a single plate, such as rifting or folding. Hot spot volcanism occurs when a mantle plume creates volcanic activity away from plate boundaries, while tectonic activity within a plate can lead to the uplift of mountain ranges through processes like folding and faulting.
Folding and Faulting usually work together to form mountains. Faulting works by one plate shifting up and one plate submerging. Folding however works by both plates pushing against each other slowly folding over and over. Faulting and Folding and work together to make mountains by as one plate moves down the other up causes the plate going up to roll over or move on top of the other plate then as the bottom plate gets heat from the earths core it rises folding the plate on top again to bring it even higher. Hoped it helped you
Folded mountains - formed by the folding of rock layers due to tectonic plate movement. Fault-block mountains - formed by the movement of tectonic plates causing blocks of the Earth's crust to uplift. Volcanic mountains - formed by the accumulation of lava and volcanic ash from volcanic eruptions. Dome mountains - formed by the uplift of large areas of the Earth's crust without significant folding or faulting.
Folding and faulting in mountains occurs because of the movement of lithospheric plates as described in the theory of plate tectonics. Continent to continent collision compresses the crust and its sedimentary cover rocks, displacing and distorting them upwards (folding) and fracturing them (faulting). Folding and faulting can also occur in oceanic crust-continental crust collisions, in areas above subduction zones.
two plate boundaries .
Folding in rock layers occurs due to compressional forces created by the movement of tectonic plates. When two plates collide, one plate is forced over the other, causing the layers of rock in between to fold and deform. This process is known as orogeny and is a result of plate tectonics and the movement of the Earth's lithosphere.
It is called folding when rocks bend without breaking because of plate movement.
because the tectonic plate that their on are folding on top of each other.
There are two reasons. First, the movement along plate boundaries and the accompanying folding and faulting can create hills and mountains. If the slopes become too steep they are unstable and prone to landslides. Second, movement along plate boundaries also generates earthquakes, which can trigger landslides.