The Appalachian mountain.
The Appalachian Mountains form a boundary with the Canadian Shield. The Canadian Shield is a large geological formation covering much of eastern and northern Canada, while the Appalachian Mountains run along the eastern coast of North America, from Alabama in the U.S. to Newfoundland in Canada.
A mountain chain at a divergent boundary is called a mid-ocean ridge or a rift valley. These formations occur where tectonic plates are pulling apart, allowing magma to rise and create new crust, leading to the formation of underwater mountain chains.
two mountain chains cross Guatemala from west to east
at a boundary between two colliding continenetal plates
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.
Mountain ranges in parallel chains are called "cordilleras."
Major mountain chains in Russia are Great Caucasus Rangeand the Urals
Canada has numerous mountain chains throughout the entire country. Of these, two of the most popular are the Canadian Rockies and the Saint Elias Mountains.
Non-volcanic mountain chains are most likely to form along convergent plate boundaries where tectonic plates collide and uplift occurs due to the compression of rocks. These types of mountain chains can also form in regions where large-scale faulting or folding has occurred, such as along transform plate boundaries or within continental interiors.
Caucasus,
Himalayas
Some of the major mountain chains in North America include the Rocky Mountains, the Appalachian Mountains, the Sierra Nevada, the Cascade Range, and the Brooks Range.