When two edges of tectonic plates collide (convergent boundary) they can cause a crumpling effect and an upthrust to form mountains. The Himalayas, for instance, were formed when the Indian Plate crashed into the Asian Plate.
Convergent boundary also applies to the situation where one plate moves under the other (subduction) this kind of plate boundary can also form mountain chains. An example of this is the Andes mountains.
by tectonic plates colliding
they are called mid-ocean ridges
Dome Mountains
dome mountains
Fold mountain or mountain chains are formed by the collisions between continental plates.
A food web is formed by overlapping food chains.
The mountains that cross Italy are the Apennine Mountains
They are the Ural Mountains and the Caucasus Mountains.
There are no such mountains.
Volcanic activity can form fold mountains or block mountains. Fold mountains are formed when tectonic plates collide. Block mountains are formed when fault block shifts.
What kind of food chains there are in the mountains will depend on the mountain region. For example, the mountains near the Mohave will have a desert food chain.
A chain of mountains is a series of connected mountain peaks that run along a continuous line or curve. Chains of mountains can be formed by tectonic plate movement, volcanic activity, or erosion over millions of years. Examples include the Andes in South America and the Himalayas in Asia.