Yes, and a mountain range
by two normal faults
no
by two normal faults
san andreas
The two types of faults that can result in mountains are thrust faults and normal faults. Thrust faults occur when older rock is pushed on top of younger rock, causing uplift and mountain formation. Normal faults occur when tensional forces cause one block of rock to drop down relative to another block, creating valleys and mountain ranges.
The answer is a fault-block mountain
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.
Fault-block mountains are created due to the movement of tectonic plates along normal faults. As the block of crust is uplifted, the surrounding material erodes, leaving a narrow mountain range with steep slopes on one side and a gentler slope on the other. Examples of fault-block mountains include the Sierra Nevada in California and the Tetons in Wyoming.
A graben forms when two normal faults cause valleys to drop down on either side of a block of rock. This landform is characterized by a depressed area between two parallel faults, with the central block lowered relative to the surrounding blocks.
Fault-block mountains are associated with normal faults, where blocks of crust are uplifted along one side of the fault while the other side drops down. As the movement along the fault continues, it can lead to the formation of a mountain range with steep slopes on one side and gentler slopes on the other.
False. Dome mountains are formed by the uplifting and folding of rock layers, not by normal faults. Mountains formed by blocks of rock uplifted by normal faults are called fault-block mountains.
A fault-block mountain is the type of mountain that is bounded by faults, where blocks of the Earth's crust are pushed up or dropped down along fault lines, creating mountain ranges with steep, rugged edges.