by two normal faults
no
by two normal faults
fault block plateaus are formed when a large block of earth is uplifted
Yes, and a mountain range
A block of rock above a fault is called the hanging wall. In a fault, the hanging wall is the block of rock that is positioned above the fault plane, while the block below the fault is called the footwall.
Fault-block mountains
Fault block mountains are created when tectonic plates move along faults, causing one block to be uplifted and the other to drop down. They have steep sides and a flat top due to the nature of their formation. Examples of fault block mountains include the Sierra Nevada in the United States and the Tetons in Wyoming.
The block above the fault is called the hanging wall.
A normal fault causes a fault-block mountain to form. In a normal fault, one block of rock moves downward relative to the other, creating a step-like feature. Over time, repeated movements along the fault can uplift and deform the crust, leading to the formation of fault-block mountains.
Fault-block mountains form from vertical fault movement. These mountains are created when blocks of the Earth's crust are pushed up and down along fault lines, resulting in steep, jagged peaks and valleys. An example of a fault-block mountain range is the Sierra Nevada in California.
This is known as the foot wall of the fault.
Seismograph