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Relative age dating geologic cross sections

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Here is an example: The Davin Shale appears oldest, followed by the Hutt Ashstone, the Cabin Limestone, Lower Coal Seam, Raven Sandstone, Blackman Shale, then Fossil Bed Limestone.

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This was followed by deposition of Loren Shale and finally the Jackson Sandstone.This film investigates the variety of stories surrounding the New Testament account of the crucifixion, death, resurrection and ascension of Jesus, by interviewing historians, theologians and historical researchers.This exploration of the latest theories about what really happened to Jesus 2000 years ago uncovers some surprising possibilities.Prior to the discovery of radiometric dating in the early 20th century, which provided a means of absolute dating, archaeologists and geologists used relative dating to determine ages of materials.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.Another period of structural deformation occurred, tilting the beds and finally the formation of the current erosional surface.

The Permian through Jurassic stratigraphy of the Colorado Plateau area of southeastern Utah is a great example of Original Horizontality and the Law of Superposition, two important ideas used in relative dating.

In order to determine the relative ages use the four fundamental principles of relative age dating that were explained to you on the concepts page.

Always start with the oldest rock and work toward the present.

Once you've figured out the relative ages, type your answers in the white blocks, then go to the bottom of the page and click on the button marked "Submit Answers for Correction." A box will open which will tell you the answers you missed.

Click OK and it will give you the number correct, the number left blank, and the number wrong.

For example in the diagram below, the sedimentary units are in sequence, P, K, M, S, and X. A body of magma (INTRUSION R) has intruded or cut through all of the previous layers. Now that you've followed the steps involved to determine the relative ages of the rock layers in the above cross section, try your hand at putting the rock layers in sequence yourself.