The rock layers that a fault passes through had to have already existed for them to break and create a fault.
This is analogous to the door panel of your car had to have already existed for it to bend and create a dent.
Not necessarily. Rock layers along a strike-slip fault may be offset if they are dipping.
thrust or reverse fault,
Every layer of rock, as one moves up from the core, is younger than the one below it. This means that the layers of rock above and below the coal are different ages, with the one above younger and the one below older.
One is not necessarily older than the other. It depends on the context. A fault running through any rock must be younger than that rock.
The answer is: Relative dating
Younger than all three sediments.
What is the relative age of a fault that cuts across three horizontal sedimentary rock layers?A. The fault is older than the middle layer. B.The fault is younger than all the layers it cuts across.C. The fault is the same age as the top layer. D. The fault is older than all the layers it cuts across == ==
Usually along a fault the rock layers are broken and displaced in some manner so that the rock layers are not continuous across the fault.
Fault
after the fault
they are younger and extrusions are older. they are younger because the surrounding rock layers had to have been there first in order for it to appear. :)
Not necessarily. Rock layers along a strike-slip fault may be offset if they are dipping.
A crosscutting feature is always younger than the rock layers it cuts through because the feature always forms after the rock layers have been formed, making the rock layers older.
thrust or reverse fault,
Principle stating that older rock layers are beneath younger rock layers.
Principle stating that older rock layers are beneath younger rock layers.
The type of rock layers found on one side of the fault will either be repeated higher or lower on the other side of the fault. This proves that one side of a fault has moved (slipped).