The three methods of relative aging of rocks are:
- Superposition - In a sequence of undisturbed sedimentary rocks, the oldest layers are at the bottom and the youngest are at the top.
- Original Horizontality - Layers of sediment are originally deposited horizontally. If the layers are tilted or folded, this indicates they have been disturbed after their deposition.
- Cross-Cutting Relationships - Geologic features (like faults or igneous intrusions) that cut through other rocks are younger than the rocks they cut.
So, the correct answers are:
- Superposition
- Original Horizontality
- Cross-Cutting Relationships