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Normal faults thin and extend the earth's crust. Reverse faults cause crustal shortening and thickening.
fault
a2. Crustal features would include those expressed on the surface, (such as mountains, rivers, and lakes) as well as those not as visible (such as volcanic feed pipes, earthquake fault lines, Geological formations, and aquifer formations.)
It is on a transform fault boundary.
The section of rock that lies below a fault is called the footwall.
Normal faults thin and extend the earth's crust. Reverse faults cause crustal shortening and thickening.
a fault
This kind of fault is called a normal fault and is usually a sign of crustal extension.
Stress
normal
This kind of fault is called a normal fault and is usually a sign of crustal extension.
in places where earth crustal rocks are weak.
Crustal plates are grinding past each other in a strike-slip fault.
fault
It is called a "don't cheat on your Intro to Physical Geography" quiz.
A fault-block mountain can be found in Death Valley, California and also in the Sierra Nevada mountains in California. Movement of large crustal blocks form fault-block mountains.
A fault-block mountain can be found in Death Valley, California and also in the Sierra Nevada mountains in California. Movement of large crustal blocks form fault-block mountains.