It's 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. The rock above it is the hanging wall and the rock below it is the footwall. In a normal fault, the hanging wall moves downwards relative to the footwall.
This is called a strike slip fault.
Earthquakes with "Faults" or "Fault Lines"
Normal fault
A fault zone is created when directed stress (as opposed to isotropic stress that simply compacts materials) overcomes the physical strength of the rock to withstand pressure leading to a pervasive crack. If the stress that created the fault is pulling the rock apart, the block that lies above the fault (the hanging wall) is bound to sink and the rocks below the fault will move upwards relative to the hanging wall. This situation is termed a "normal fault" and occurs for example in rift zones all over the world. If confining pressure produces a fault, the hanging wall is pushed on top of the rocks below the fault. This is known as a "reverse fault" and is a common phenomenon in many mountain ranges. In a special type of stress regime, faults are created along which rocks are sliding past each other horizontally. They are called "transform faults".
Tension in Earth's crust pulls rock apart, causing hanging walls. In a normal fault, the fault is at an angle, so one block of rock lies above the fault while the other block lies below the fault. The block of rock that lies above is called the hanging wall. The rock that lies 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. The rock above it is the hanging wall and the rock below it is the footwall. In a normal fault, the hanging wall moves downwards relative to the footwall.
Tension in Earth's crust pulls rock apart, causing hanging walls. In a normal fault, the fault is at an angle, so one block of rock lies above the fault while the other block lies below the fault. The block of rock that lies above is called the hanging wall. The rock that lies below is called the footwall.
Actually the first one is right! In my science book its clearly says :normal fault, the fault is at an angle so one block of rock lies above the fault while the other fault lies below the fault. When movement occurs along a normal fault, the hanging wall slips downward. sorry Smallvillegirl... SO THE ANSWER IS NORMAL FAULTSActually, that's wrong. I have the same crossword puzzle whoever answered the question, and it was assigned for homework, and if number 6 across is shearing, number 5 down would have to be reverse. It is reverse fault.=SmallvilleGrl=Old Answer:The answer to this question is easy! Unless you don't know your Earth Science of course! There are three different types of faults:Normal Faults, Reverse Faults, and Strike-slip Faults.A strike-slip fault(or a latteral fault) moves in opposition of each other.A reverse fault is when the hanging wall moves upward caused by compression.A normal fault is when the hanging wall moves downward caused by tension.So there you have it! The answer to your question is obviously a NORMAL FAULT!!!!!If you need any more answers' about Earth Science post some more questions and I'll answer them for ya!!!!!sincerely,~Anonymous~
Faults are breaks in the crust where the crust has moved. The types of dip-slip faults are normal and reverse faults. In both of these, the movement is along the slope of the fault. Sudden movements along these faults can produce fault scarps. Layers of rock being misaligned is evidence of fault movement. Fault creep is caused by slow movement along the fault.In a normal fault, the plates are moving away from each other. This is due to tension. When the fault moves, the footwall rises relative to the hanging wall. Normal faults occur at divergent boundaries, such as ocean ridges. Normal faults can produce fault-block mountains.In a reverse fault, the plates are moving towards each other. This is due to compression. Here, the footwall falls relative to the hanging wall. A thrust fault is a special type of reverse fault, where the angle is shallow. Reverse faults occur at convergent boundaries, like subduction zones.A strike-slip fault is where the two plates move horizontally past each other. The force between them is called shearing. This type of fault is often called a transform fault, because they occur at transform boundaries.
There are 3 main types of faults 1. Normal 2. Strike slip 3. Reverse(Thrust) In a normal fault the foot wall stays in place while the hanging wall moves DOWNWARDS In a strike slip the tectonic plate(s) slide past each other horizontally In a reverse fault, the hanging wall gets pushed UPWARDS over the foot wall (The pictures are in the reverse order)
This is called a strike slip fault.
THRUST
Earthquakes with "Faults" or "Fault Lines"
The crack that forms when rocks break and move past each other is called a fault . The blocks of rock that are on either side of the fault are called fault blocks .
Normal fault
Answer : Normal Fault Explanation : Normal fault is the cliche kinds of fault.It forms when rock above an inclined fracture plane moves downward, sliding along the rock on the other side of the fracture.