what are the 5 principles of relative dating

There are a number of different types of intrusions, including stocks, laccoliths , batholiths , sills and dikes. Though relative dating can only determine the sequential order in which a series of events occurred, not when they occurred, it remains a useful technique. Third, we observe that the fault A cuts across and displaces rock layers B-F. See similar textbooks. Cross-cutting features can include folds, faults, and igneous intrusions. This matching process is called correlation, which has been an important process in constructing geological timescales. Because these features are the ones doing the cutting, we know that they are younger than the rocks that they cut into.

WHAT ARE THE 5 PRINCIPLES OF RELATIVE DATING / morphy.info

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