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The seismic waves created by the release of rock stress is usually recorded as an earthquake.
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.