Types of Mountains
: a mountain range resulting from dissection of a structural dome (as the Black Hills in South Dakota) — called also domal mountain
A: Some examples of fault-block mountains include the Sierra Nevada and the Grand Tetons in the United States and the Harz Mountains in Germany. Fault-block mountains are formed as a result of cracking or faulting along the planet's surface, leading to several crustal blocks being heaved upwards while other chunks of rocks slide downwards.
A: Some examples of fault-block mountains include the Sierra Nevada and the Grand Tetons in the United States and the Harz Mountains in Germany. Fault-block mountains are formed as a result of cracking or faulting along the planet's surface, leading to several crustal blocks being heaved upwards while other chunks of rocks slide downwards.
Fold Mountains are formed as a result of the compression of tectonic plates, which leads to the formation of large fold-like structures on the earth’s crust. Fold Mountains primarily exist as mountain ranges, and the majority of the earth’s well-known mountain ranges are examples of Fold Mountains.
Fold mountains sometimes are characterized by foreland basins, depressions that run parallel to the mountain range. The Erbo Basin, in northern Spain, is a foreland basin that formed with the Pyrenees, a fold mountain chain created by the continental collision of the microcontinent of Iberia with the massive Eurasian plate.
Difference Between Mountain and Plateau are :-• The main difference between a mountain and a plateau is that the mountain is an elevated, pointed structure whereas a plateau is an elevated area with a flat top. • A plateau is generally lower in height than mountain, though there are plateaus higher than some mountains.
Volcanic mountains form as lava oozes forth from cracks in the earth. The lava builds up around the area where the eruption occurred. Layers build upon layers and over a period of time, a volcanic mountain forms.