Reverse Fault
A reverse fault occurs when a portion of rock moves upward and over the other with a steep dip angle. This type of fault occurs in compressional tectonic settings where the forces push the rocks together, causing one block to thrust over the other.
A reverse fault occurs when a portion of rock moves upwards while the other portion moves downwards, forming a dip in the rock layers. This type of fault is typically associated with compressional forces in the Earth's crust.
The answer would be upward
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~
In a lateral fault, the hanging wall moves horizontally in relation to the footwall. This type of fault occurs when the blocks of rock on either side of the fault move horizontally past each other. The hanging wall moves in the direction of the fault line, while the footwall remains relatively stationary.
The answer is a dip-slip fault, When a portion of rock moves upward leaving the other in place with a dip this is known as a dip-slip fault.
The answer is a dip-slip fault, When a portion of rock moves upward leaving the other in place with a dip this is known as a dip-slip fault.
A reverse fault occurs when a portion of rock moves upward and over the other with a steep dip angle. This type of fault occurs in compressional tectonic settings where the forces push the rocks together, causing one block to thrust over the other.
A reverse fault forms when a hanging wall moves upward due to compressional forces. This type of fault occurs in areas where the crust is being pushed together, causing the hanging wall to move up and the footwall to move down.
A reverse fault occurs when a portion of rock moves upwards while the other portion moves downwards, forming a dip in the rock layers. This type of fault is typically associated with compressional forces in the Earth's crust.
In a normal fault, the hanging wall moves downward relative to the footwall, creating extensional forces. In a reverse fault, the hanging wall moves upward relative to the footwall, generating compressional forces.
When the hanging wall moves upward relative to the footwall, it creates a reverse fault, also known as a thrust fault if the angle is shallow. This type of fault typically occurs in regions experiencing compressional forces, causing the crust to shorten and fold. Reverse faults are common in mountainous regions where tectonic plates converge.
The hanging wall moves up relative to the foot wall. These happen when tectonic forces push rocks together. It is caused by compression.
The hanging wall is the block of rock located above the fault plane. It moves downward in a normal fault and upward in a reverse fault during faulting events. It is named "hanging" because in underground mining, it appears to hang over the miners' heads.
upward
it moves downwards
The type of fault that occurs when one portion of rock slides over the top of another is called a reverse fault. In a reverse fault, the hanging wall moves upward relative to the footwall, typically due to compressional forces. This type of faulting is commonly associated with convergent plate boundaries where tectonic plates collide.