fault block mountian
parallel normal faults.
Graben
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".
Faults form in the lithosphere. This is composed of the crust and the solid rocky portion of the upper mantle. Both these parts of the crust are brittle. This means that they lose cohesion when they fail forming fractures or faults.
Volcanoes are usually found near convergent an divergent plate boundaries, which are themselves major faults and usually create minor faults. Minor faults can also provide a pathway for magma to reach the surface.
parallel 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.
parallel normal faults.
parallel normal faults.
parallel normal faults.
parallel normal faults.
HORST
Graben
A rift valley is formed by the depression of a block of the earth's crust between two faults or groups of faults, of approximately parallel orientation.
along nearly parallel normal faults.
It is a depressed block of land, bordered by parallel geological faults.
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".