It's a fault-block mountains :)
It's a fault-block mountains :)
A rift valley mountain range is formed when tension causes large blocks of crust to drop down. This type of mountain range typically has steep fault scarps along the edges of the blocks that have dropped down. An example of this type of mountain range is the East African Rift.
The Basin and Range mountain range is formed as a result of tension stress, which causes the crust to be pulled apart and stretched horizontally, resulting in the characteristic alternating valleys and mountain ranges in the region.
It's a fault-block mountains :)
Fault block mountains are formed when large blocks of the Earth's crust are uplifted along faults. Tensional forces cause the blocks to move vertically relative to each other, creating steep mountain ranges and valleys. As the blocks continue to move, the mountains can be further uplifted and shaped by erosion.
A fault-block mountain is typically formed by tensional forces where blocks of the Earth's crust move vertically due to normal faults. These mountains result from the crust being pulled apart, leading to the uplift of fault blocks.
Large blocks of Earth's crust that drops down relative to other blocks, will form a rift valley (trench). The Great Rift Valley in Africa is one example.
A fault-block mountain is formed when higher blocks of land are displaced along a fault line, causing one side of the fault to rise relative to the other. This creates a steep-sided mountain range with a distinctive block-like structure.
fault block
An upwarped mountain is formed by the uplifting of large blocks of Earth's crust without significant faulting. In contrast, a fault-block mountain is created by the displacement of blocks along faults, causing some blocks to be uplifted while others are dropped down. Ultimately, the main difference lies in the processes that lead to the formation of these mountain types.
numerous folds and faults would appear in the bedrock
Fault block mountain can be high.