The principle of superposition can be used to determine the relative age of these rock layers. This geological principle states that in any undisturbed sequence of rocks, the oldest layers will be at the bottom and the youngest layers will be at the top.
The principle of superposition can be used to determine
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the actual age of these rock layers
the relative densitites of these rock layers
the actual temperatures of these rock layers
the relative age of these rock layers
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