The Denali Fault is in South Central Alaska. One end is near Cantwell, Alaska (about 90 miles south of Fairbanks) and goes to a point near near Mentasa Lake (south of Tok).
No, a thrust fault is a type of reverse fault, where the hanging wall moves up and over the footwall. In contrast, a normal fault is a type of fault where the hanging wall moves down relative to the footwall.
A normal fault.
A transform fault is a general term to describe a plate boundary where the lithosphere is not destroyed or created. A transverse fault is a type of transform fault also known as a strike-slip fault.
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.
If a fault occurs in an area where rock layers have been folded, the type of fault it is likely to be is thrust faulting. This type of fault will have the ground on one side of the fault, move up and over adjacent ground.
The Denali Fault line is located in Alaska.
The answer is the Denali Fault is your mom years old.
In Alaska
San Andreas in California, Denali, Cadell Fault in South Australia
The Mid-Atlantic Ridge or the Marianas Trench.
The major fault line that runs through Alaska is the Denali Fault, which extends for about 560 miles from the central part of the state to the southeastern coast. This fault is capable of generating large earthquakes and is closely monitored by scientists for seismic activity.
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The Hayward Fault is a Strike-slip Fault.
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a strike slip fault