It moves downward.. the force behind it is tension
Where fault blocks collide into each other. The most prominent example of this are the Himalayan Mountains formed by the collision of the Indian plate and the Eurasian Plate making what is called a folded mountain.
people die get over it!
There are 3 main types of faults 1. Normal 2. Strike slip 3. Reverse(Thrust) In a normal fault the foot wall stays in place while the hanging wall moves DOWNWARDS In a strike slip the tectonic plate(s) slide past each other horizontally In a reverse fault, the hanging wall gets pushed UPWARDS over the foot wall (The pictures are in the reverse order)
No, the closer an object is to the lens, the more the spherical it is.
A sudden movement of the Earth's crust is called an earthquake.
An Earthquake happens.
it moves downwards
A sudden shift of the earth's crust along a fault could result in an earthquake.
the hanging wall moves down relative to the footwall
The sudden movement could result in an earthquake.
A Reverse fault is happens when tectonic forces cause compression that PUSHES rocks together. Normal fault happens when tectonic forces cause tension that PULLS rocks apart.Normal fault is when the hanging block moves down relative to foot block wall where as the reverse fault is formed when the hanging block wall moves up relative to the foot block walls a result of tension and compression force respectively
High friction on opposite sides of a fault can cause stress to build up in the rocks. When the stress exceeds the strength of the rocks, it can result in an earthquake as the rocks suddenly shift along the fault line.
a normal fault
In a normal fault, the hanging wall moves down relative to the footwall, whereas in a reverse fault, the hanging wall moves up relative to the footwall.
A normal fault moves because it is under tension. In a normal fault, the hanging wall moves down relative to the footwall due to the pulling apart of the Earth's crust, creating space and tension that cause the fault to move.
A reverse fault occurs when rock above the fault moves upward at the fault line. This type of fault is associated with compressional stress where the hanging wall moves up relative to the footwall. Reverse faults are common in regions undergoing compression, such as convergent plate boundaries.