10 Facts about Block Mountains

Thursday, July 23rd 2015. | Mountain

Facts about Block Mountains present the detail information about the fault block mountain. It is made of a very long and large block of rocks. The block mountain is formed because the earth crust has the localized stresses or even tectonic movement. The faults break the large bedrock into blocks. Check out more interesting facts about Block Mountains below:

Facts about Block Mountains 1: the crustal blocks

The crustal block is used to call the largest one from the fault blocks.  You can call them terranes when the crustal blocks are broken from the tectonic plates.

Facts about Block Mountains 2: the continent sized blocks

There are various names used to call the continent sized blocks. You can use the term outer highs, extensional allochthons, H-blocks, microcontinents and continental ribbon

Facts about Block Mountains

Facts about Block Mountains

Facts about Block Mountains 3: the tectonic activity

The moving plates on earth are always associated with the tectonic activity. The horizontal movement is very common to occur between the blocks. The vertical movement can happen as well. It usually gives the bigger impact on the blocks.

Facts about Block Mountains 4: the formation

The formation of Block Mountain is because of the underground pressure which makes the large rock mass to break away into blocks.

Block Mountains

Block Mountains

Facts about Block Mountains 5: the causes

There are several causes which make the mountain wear down like the frost erosion, wind and mass wasting.

Facts about Block Mountains 6: the landforms

The vertical movement of the block mountain can create landforms. As I have stated before, the vertical movement can bring more dramatic effect than the horizontal movement. There is no need to wonder that valleys, lakes, ridges, mountains and hills are formed as the result of the vertical displacement.

Block Mountains Facts

Block Mountains Facts

Facts about Block Mountains 7: the rifting process

The rifting process can lead into the formation of fault Block Mountain.   The examples for this rifting can be seen on the Death Valley in California and East African Rift Zone. Get facts about Andes Mountain here.

Facts about Block Mountains 8: the types of Block Mountains

The lifted and sloped mountains are the two types of Block Mountains. The former one is characterized with side scarps located on the two steep sides of the mountain.

Block Mountain

Block Mountain

Facts about Block Mountains 9: the examples of Block Mountains

The lifted mountains lead the formation of graben terrains. The examples can be seen on the graben located in Black Forest in Germany, Vosges Mountain in France, and Upper Rhine valley. Check facts about Alps here.

Facts about Block Mountains 10: the sloped block mountains

The sloping mountain is characterized with one steep site. You can find it in the western US.

Block Mountain Image

Block Mountain Image

Are you impressed after reading facts about Block Mountains?

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