The down thrown block is known as a Graben. If the extensional stress in the crust continues, then eventually a rift valley will form. The crustal blocks on either side of a Graben are known as Horst structures.
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a rift valley
grabens
A ridge forms a major boundary of a catchment. A horst is the elevated block of land between two normal faults.
The answer is a fault-block mountain
Fold-block mountains form when tension makes the lithosphere break into many normal faults.
A fault- block mountain
mountains
fault block mountian
Normal fault. The fault itself does not cause the sinking but is part or an effectof the process. The sunken block between two faults is called a "graben".
It is called Graben
by two normal faults
Normal Faultin a normal fault, the hanging wall slips down relative to the footwallfootwall- the rock that lies belowhanging wall- the block of rock that lies abovenormal fault- tension in Earth's crust pulls rock apart which causes normal fault2. The Land Between Two Normal Faults Moves Upward To Form What?is a Fault - Block Mountain.
by two normal faults
A large elongated depression with steep walls formed by the downward displacement of a block of the earth's surface between nearly parallel faults or fault systems.
A ridge forms a major boundary of a catchment. A horst is the elevated block of land between two normal faults.
Normal Faultin a normal fault, the hanging wall slips down relative to the footwallfootwall- the rock that lies belowhanging wall- the block of rock that lies abovenormal fault- tension in Earth's crust pulls rock apart which causes normal fault2. The Land Between Two Normal Faults Moves Upward To Form What?is a Fault - Block Mountain.
along nearly parallel normal faults.
The answer is a fault-block mountain
Yes, and a mountain range