Fault plane is called the hanging wall or headwall.
The hanging wall of a fault is.
When the hanging wall moves up in relative to the footwall it is called a fault.
The block below is called the footwall.
When rocks slip past each other in faulting the upper or overlying block along the fault plane is called the hanging wall or headwall.
The dip of a fault plane is its angle of inclination measured from the horizontal.
The keweenaw fault is a thrust fault the name we give to prominent reverse faults.
Grabens are formed by what type of faulting.
These usually occur when tectonic forces cause tension that pulls rocks apart.
The hanging wall occurs above the fault plane and the footwall occurs below it.
The fault strike is the direction of the line of intersection between the fault plane and earth s surface.
So the hanging wall is above the plane of the fault and over your head and the footwall is below the plane of the fault and is under your feet.
When the hanging wall moves down in relative to the footwall it is called a fault.
Its strike and its dip.
Any fault plane can be completely described with two measurements.
That s the hanging wall.
Describe three types of faults.
In a non vertical fault where the fault plane dips the footwall is the section of the fault that lies under the fault while the hanging wall lies over the fault the names come about from the.
Fill in the blank 1.
The crust is shortened and thickened.
This terminology comes from mining.
The two sides of a non vertical fault are known as the hanging wall and footwall.
In a n fault the hanging wall block moves up with the respect to the footwall 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.
The fault strike is the direction of the line of intersection between the fault plane and earth s surface.
When the fault plane is vertical there is no hanging wall or footwall.
The block below is called the footwall.
In a normal fault the fault is at an angle so one block of rock lies above the fault while the other lies below it.
When working a tabular ore body the miner stood with the footwall under his feet and with the hanging wall above him.
They are driven by significant tectonic events that affect large areas like continental collisions.
The walls of the fault are the rocks on either side of the plane.
