When the fault plane is vertical there is no hanging wall or footwall.
Type of fault where the hanging wall moves upward.
The dip of a reverse fault is relatively steep greater than 45.
Its strike and its dip.
In this fault the hanging wall moves up relative to the footwall.
When movement along a fault is the reverse of what you would expect with normal gravity we call them reverse faults.
In this fault the.
Any fault plane can be completely described with two measurements.
The terminology of normal and reverse comes from coal mining in england where normal faults are the most common.
Then there is also a strike slip fault which happens at a transform boundary.
When the hanging wall moves down in relative to the footwall it is called a fault.
The hanging wall will slide upwards right.
A strike slip fault or a latteral fault moves in opposition of each other.
Where the fault plane is sloping as with normal and reverse faults the upper side is the hanging wall and the lower side is the footwall.
A dip slip fault in which the upper block above the fault plane moves up and over the lower block.
Angular ridges formed by the differential erosion of inclined sedimentary strata are called hogbacks.
These usually occur when tectonic forces cause tension that pulls rocks apart.
This type of faulting occurs in response to extension.
Reverse folds have limbs that dip gently and the angle between the limbs is large.
A reverse fault is the opposite of a normal fault the hanging wall moves up relative to the footwall.
A fault where the hanging wall moves up relative to the footwall is referred to as a fault.
Describe three types of faults.
You probably noticed that the blocks that move on either side of a reverse or normal fault slide up or down along a dipping fault surface.
This type of faulting is common in areas of compression when the dip angle is shallow a reverse fault is often described as a thrust fault.
A is the type of fault that is produced when the hanging wall moves upward relative to the footwall.
Strike slip faults have a different type of movement than normal and reverse faults.
Occurs where the hanging wall moves up or is thrust over the foot wall.
A reverse fault is when.
Reverse faults indicate compressive shortening of the crust.
This is caused by shear stress.
Occurs when the hanging wall moves down relative to the foot wall reverse fault.
When the hanging wall moves up in relative to the footwall it is called a fault.