Fault The Hanging Wall Moves Down

Normal faults are common. Block position under the hanging wall. If we hold the foot wall stationary gravity will normally want to pull the hanging wall down right.

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Compare the image to the right with the normal fault above.

Fault the hanging wall moves down.

Hanging wall and footwall. Other articles where normal fault is discussed. A n fault forms when the hanging wall moves down relative to the footwall a. Formed by compressional stress rocks are pushed towards.

When working a tabular ore body the miner stood with the footwall under his feet and with the hanging wall above him. Block position over the fault. But that is when the foot wall moves down the hanging wall moves up. In a strike slip fault they slide past each other the foot wall and hanging wall are not there because it has.

They bound many of the mountain ranges of the world and many of the rift valleys found along spreading margins. The two sides of a non vertical fault are known as the hanging wall and footwall. The hanging wall moves up relative to the foot wall. Normal fractures in rock with no offset where there has been no motion are called.

The hanging wall moves down relative to the foot wall. Normal dip slip faults are produced by vertical compression as earth s crust lengthens. This terminology comes from mining. The hanging wall occurs above the fault plane and the footwall occurs below it.

The hanging wall slides down relative to the footwall. Formed by tensional stress rocks are stretched away from each other reverse fault. Faults that move the way you would expect gravity to move them normally are called normal faults.

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