Relative Dating of Rock Layers
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This technique uses principles of stratigraphy (rock strata) and the study of fossils (palaeontology) to determine the relative ages of rocks and sediments.
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relative dating absolute dating Chapter 17 Chapter 17 principle of superposition principle of original horizontality Chapter 17 Chapter 17 principle of lateral continuity principle of cross‐cutting relationships Chapter 17 Chapter 17 principle of inclusions principle of fossil succession Chapter 17 Chapter 17 unconformity disconformity Chapter 17 Chapter 17 angular unconformity nonconformity Chapter 17 Chapter 17 correlation guide fossil Chapter 17 Chapter A principle holding that rock layers extend outward in all directions until they terminate. A principle holding that an igneous intrusion or fault must be younger than the rocks it intrudes or cuts across.