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