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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.


Fault-block mountains often result from rifting, another indicator of tensional tectonic forces. These can be small or form extensive rift valley systems, such as the East African Rift zone. Death Valley in California is a smaller example.


Fault-block mountains are formed by the movement of large crustal blocks when forces in the Earth’s crust pull it apart. Some parts of the Earth are pushed upward and others collapse down.


A fault-block mountain can be found in Death Valley, California and also in the Sierra Nevada mountains in California. Movement of large crustal blocks form fault-block mountains.


* Block mountains are formed when large areas or blocks of earth are broken and subsides vertically. * The uplifted blocks are termed as horsts and the lowered blocks are called graben. * The Great African Rift Valley (valley floor is graben) * T...


2. Fault-Block Mountains - These type of Mountains are formed when faults or cracks in the Earth's crust force some materials or blocks of rock up and others down. Instead of the Earth folding over, the Earth's crust fractures (pulls apart).


The origin of the names of mountains may have historical or regional significance. For example, the Himalaya mountain range derives its name from Sanskrit. "Himalaya' literally means the region or ...


Fault-block mountains (or just “block mountain“) are created when faults or cracks in the Earth’s crust force materials upward. So instead of folding, like the plate collision we get with ...


Fault Block Mountains. Fault block mountains are distinguished by great sheer rock faces. These form when enormous underground pressure forces a whole rock mass to break away from another. The line at which this break takes place is called a fault. On one side of this break the rocks rise; on the other side they sink down.


Block mountains repre­sent the upstanding parts of the ground between two faults or on either side of a rift valley or a graben. Types of Block Mountains: Essentially, block mountains are formed due to fault­ing in the ground surface. Block mountains are gener­ally of two basic types e.g.: