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Sometimes beds of rock can turn over the other way, so be very cautious when relatively dating rocks!
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One way to find the age of a xenolith or subsidence area surrounded by volcanic debris is to correlate its layers with the layers of wall or parent rocks.
Stratigraphy is the study of sedimentary rock layers.
An absolute age is one determined usually by mass-spectrometry where an isotope is measured and then an age can be calculated (a very very basic explanation).