relative age
When rocks break, they move along the surface in a process known as faulting. This movement can occur due to tectonic forces, causing the rocks to break and move along fractures known as faults.
These types of rocks are known as "fault rocks" or "fault gouge." The movement of rocks on opposite sides of a fault can create various structures such as slickensides, cataclasite, or mylonite, depending on the amount of movement and deformation that has occurred.
A normal fault may form when rocks are pulled apart. In a normal fault, the hanging wall drops down relative to the footwall due to tensional forces pulling the rocks apart.
Faults are the result of "brittle deformation". This means that they occur in rocks which are not molten. A rock has to be solid before it can be faulted, and hence the rock must have formed before the fault could form within it.
When compression pushes rocks together, faults form when the stress exceeds the strength of the rocks, causing them to break and push against each other. These fault zones can be areas of high seismic activity as the rocks continue to be pushed and undergo deformation.
the answer is procces of breaking down rock into smaller and smaller sediments
Index fossils
In order to be useful in determining the relative ages of rocks, an indicator must provide different indications for rocks of different ages, right? So how could something which doesn't change over time be useful?
they are useful by showing where the fossil is buried then on that certain layer, it will be studied to know the age.
the group of igneous rocks composed primarily of feldsper and quartz
a reverse fault
Reverse fault
They're useful for x-rays or looking at metals,or determining the age of rocks/fossils. (Hope it helped!😁)
Rocks on either side of a fault move along the surface of the fault.
A reverse fault may form when rocks are compressed.
This kind of fault is called a normal fault and is usually a sign of crustal extension.
When rocks break, they move along the surface in a process known as faulting. This movement can occur due to tectonic forces, causing the rocks to break and move along fractures known as faults.