They are formed from hardened lava which comes up from the ground and hardens inside the rock, which happens of course after the other rocks have already formed.
Extrusions, intrusions, and faults are key features used in relative dating of rocks. When lava extrudes onto the surface and solidifies, it creates a layer of igneous rock that is younger than the rocks beneath it. Intrusions, which occur when molten rock pushes into existing rock layers, are also younger than the surrounding rocks they invade. Faults are fractures where rocks have moved; they are younger than the rocks they cut through, indicating that the rocks were already present before the fault occurred.
The youngest rock layer in a geological sequence is typically the one that has not been disturbed by faults or intrusions. When a fault occurs, it displaces the rock layers, indicating that the fault is younger than the rocks it cuts through. Similarly, an igneous intrusion forms when magma penetrates existing rock layers, making it younger than the surrounding sedimentary rocks. Thus, both faults and igneous intrusions are younger than the rock layers they affect.
Faults are younger than the rocks they cut through, as they are formed after the rock units. The offset layers or rocks along a fault help geologists determine the relative age relationship between the fault and the surrounding rocks.
Geologic features such as faults and igneous intrusions that are younger than the rocks they cut through are referred to as "younger features" in the context of relative dating. This concept is based on the law of cross-cutting relationships, which states that if a geological feature cuts through another, it must be younger than the feature it disrupts. This principle helps geologists determine the relative ages of various rock formations and geological events.
Faults are always younger than the rocks they cut. They cannot be older that the rocks they are cutting, because the rocks would not be there.
Faults, intrusions, and extrusions are all geologic features related to the movement of the Earth's crust. Faults are fractures along which rocks have moved, intrusions are igneous rocks that have been forced into pre-existing rocks, and extrusions are igneous rocks that have been extruded onto the Earth's surface. They all involve the movement and displacement of rocks, contributing to the shaping of the Earth's crust.
sill
Crosscutting includes fractures (cracks in rocks), faults (fractures where movement has occurred), or masses of magma that cut across preexisting rocks before cooling. Any crosscutting feature must be younger than the rock or sediment it cuts across.
If the situation is as simple as the one you have stated, it isn't difficult. Meanwhile, many faults displace laterally, either in compression or tension so that it can appear that younger rocks overlie older ones. See the law of super-position. Compressive faults generally force younger rocks below older, but not always. See subduction zones. Then see ophiolite suites.
How could the rock be faulted if it came after the faulting? It wouldn't be there to fault. So therefore, what ever the fault cuts through, it must be younger than it in order for it to be able to cut the rock in the first place.
The youngest rocks would be igneous, those created by cooling magma. Impossible to find a fossil there.
igneous rocks