Relative dating cross section Relative dating cross section

Relative dating cross section

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Principle of crosscutting relations: Try to find the oldest rock usually located near the bottom in the diagram below and work your way up. A, B, D are sedimentary layers.

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Put in order from oldest to youngest. Faunal succession deals with fossils.

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The Laws of Geology: The opposite is true for an anticline a big dome-shaped fold. Order old to young: The order of events in the archaeological cross section shows that the oldest remains are Roman. Key Terms and Laws: Principle of original horizontality: Igneous rocks are formed by the solidification of a liquid magma; the therefore can intrude into preexisting rocks or be poured out onto the surface of the earth: After this the medieval remains are more recent and the industrial remains are more recent still.

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Tilt — plate tectonics — Law of Horizontality. E — intrusion — cross-cutting law.

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The most recent change of all is the modern bridge support. How do you know? Remember to include any erosion, faulting, tilting or relative dating cross section Principle of faunal succession: Label the diagram with anticline and syncline.

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If there are fossils embedded in the rock, these fossils inclusions are younger than the rock they are embedded in but older than the rock above them. Sedimentary rocks that contain fragments of another rock are younger than the rocks that the fragments came from.