In this fault the hanging wall moves up relative to the footwall.
Type of fault where the hanging wall moves upward.
A is the type of fault that is produced when the hanging wall moves upward relative to the footwall.
Fill in the blank 1.
What type of fault is shown here.
Occurs where the hanging wall moves up or is thrust over the foot wall.
Reverse faults indicate compressive shortening of the crust.
Any fault plane can be completely described with two measurements.
In this fault the.
Angular ridges formed by the differential erosion of inclined sedimentary strata are called hogbacks.
Occurs when the hanging wall moves down relative to the foot wall reverse fault.
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.
Its strike and its dip.
Describe three types of faults.
The dip of a reverse fault is relatively steep greater than 45.
This is caused by shear stress.
When the fault plane is vertical there is no hanging wall or footwall.
Reverse folds have limbs that dip gently and the angle between the limbs is large.
When the hanging wall moves up in relative to the footwall it is called a fault.
A fault where the hanging wall moves up relative to the footwall is referred to as a fault.
There are three different types of faults normal faults reverse faults and strike slip faults.
This type of faulting occurs in response to extension.
A dip slip fault in which the upper block above the fault plane moves up and over the lower block.
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.
When the hanging wall moves down in relative to the footwall it is called a fault.
The terminology of normal and reverse comes from coal mining in england where normal faults are the most common.
The hanging wall will slide upwards right.
Strike slip faults have a different type of movement than normal and reverse faults.
A reverse fault is the opposite of a normal 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.
A strike slip fault or a latteral fault moves in opposition of each other.
These usually occur when tectonic forces cause tension that pulls rocks apart.