The concept that the oldest rock layers are at the bottom of a sequence with younger rock layers deposited on top of them. This can be considered a rule that applies in all situations, except where the rocks are extremely deformed.
A principle of geology that states that rock and sediment layers are arranged in times sequence, with older layers on the bottom and more recent layers on the top. Geological activity can disrupt this order.
when one geologic unit lies on top of another unit, the upper unit has the younger age.
This describes how layers are usually laid down according to their age: the oldest layer is found on the bottom, and the most recent layer is on top. So, if a layer is on top of another layer, it is probably more recent.
Where two or more beds of rock lie one above the other, the uppermost bed is normally the younger. This is known as the Principle of Superposition.