How are cross cutting relationships used in relative dating

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How does the law of crosscutting relationships help scientists determine the relative age of rocks?

Cross-cutting relationships Save Cross-cutting relations can be used to determine the relative ages of rock strata and other geological structures. Cross-cutting relationships is a principle of geology that states that the geologic feature which cuts another is the younger of the two features. It is a relative dating technique in geology. It was first developed by Danish geological pioneer Nicholas Steno in Dissertationis prodromus and later formulated by James Hutton in Theory of the Earth and embellished upon by Charles Lyell in Principles of Geology Types There are several basic types of cross cutting relationships: Structural relationships may be faults or fractures cutting through an older rock. Intrusional relationships occur when an igneous pluton or dike is intruded into pre-existing rocks. Stratigraphic relationships may be an erosional surface or unconformity cuts across older rock layers, geological structures, or other geological features. Sedimentological relationships occur where currents have eroded or scoured older sediment in a local area to produce, for example, a channel filled with sand. Paleontological relationships occur where animal activity or plant growth produces truncation.

Nov 7, Answer: Because the fault that strikes through layers of rock must be younger than the rocks it strikes through. So, let's imagine for a second that you have a 3-layered cake.

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April Koch April teaches high school science and holds a master's degree in education. Discover how geologists study the layers in sedimentary rock to establish relative age. Learn how inclusions and unconformities can tell us stories about the geologic past. We'll even visit the Grand Canyon to solve the mystery of the Great Unconformity!

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Cross-cutting relationships

There are several basic types of cross cutting relationships: Structural relationships may be faults or fractures cutting through an older rock. Intrusional relationships occur when an igneous pluton or dike is intruded into pre-existing rocks. Stratigraphic relationships may be an erosional surface or unconformity cuts across older rock layers, geological structures, or other geological features.

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