Hanging Wall Direction Of Strike-Slip Fault at Darrell Matthew blog

Hanging Wall Direction Of Strike-Slip Fault. Reverse faults form when the hanging wall moves up. If the fault develops in a. The body of rock above the fault is called the hanging wall, and the body of rock below it is called the footwall. They are common at convergent boundaries. The forces creating reverse faults are compressional, pushing the sides together. If these are not clear, think of a geologist standing in a small cave exactly on a fault plane that dips moderately. Normal faults occur when two plates, one on top of the other, slide past each other and create the.

3.9 Earthquakes, Faults, and Earthquake Faults Geosciences LibreTexts
from geo.libretexts.org

The body of rock above the fault is called the hanging wall, and the body of rock below it is called the footwall. Reverse faults form when the hanging wall moves up. If these are not clear, think of a geologist standing in a small cave exactly on a fault plane that dips moderately. If the fault develops in a. The forces creating reverse faults are compressional, pushing the sides together. They are common at convergent boundaries. Normal faults occur when two plates, one on top of the other, slide past each other and create the.

3.9 Earthquakes, Faults, and Earthquake Faults Geosciences LibreTexts

Hanging Wall Direction Of Strike-Slip Fault Reverse faults form when the hanging wall moves up. If the fault develops in a. If these are not clear, think of a geologist standing in a small cave exactly on a fault plane that dips moderately. Reverse faults form when the hanging wall moves up. Normal faults occur when two plates, one on top of the other, slide past each other and create the. The body of rock above the fault is called the hanging wall, and the body of rock below it is called the footwall. They are common at convergent boundaries. The forces creating reverse faults are compressional, pushing the sides together.

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