Some fault blocks found in the Philippines include the Sierra Madre block in Luzon, the Cotabato block in Mindanao, and the Samar block in the Eastern Visayas region. These fault blocks are characterized by uplifted mountains or plateaus bounded by faults which have shifted vertically.
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.
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.
This is known as the foot wall of the fault.
Fault block mountain can be high.
look for chocolate hills in bohol type that in google
fault block plateaus are formed when a large block of earth is uplifted
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
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.
This is known as the foot wall of the fault.
Seismograph
nope fault block
The block of rock below a fault is the "footwall" if you are referring to geology/earthquake terms.
Fault block mountain can be high.
Fault block mountains are formed when tectonic plates move along fault lines, causing blocks of crust to be uplifted and tilted. The movement along fault lines is crucial in creating the varying elevations and angles of the blocks that form fault block mountains. The rocking and sliding along fault lines result in the unique landscape of fault block mountains.