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Strata dating

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Relative dating

Many things on our planet, such as the formation of mountains, or the draining of lakes by rivers, take millions of years. The creation of life on earth and the extinction of life on earth has happened many times over. Scientists have documented at least 5 mass extinctions. Geological Dating -Determining rock strata by geological composition -Using depth to determine relative age -Predicting natural events by strata 2 What is Geological Dating? It is how scientists can determine the relative age of rocks and fossils. They do this by looking at the strata layers of the rock.

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Deposition —The accumulation of sediments after transport by wind, water, ice, or gravity. Facies —A body of sedimentary rock with distinctive characteristics. Fossil correlation —The matching of sedimentary strata based on fossils present in the strata. Lateral continuity —The principle that sedimentary strata are three-dimensional features that extend horizontally in all directions and that eventually terminate against the margin of other strata. Physical correlation —The matching of sedimentary strata based on the physical characteristics of rocks that make up the strata. Radiometric dating —A process by which the age of a rock can be determined by studying the relative concentrations of a radioactive isotope and the products formed by its decay. Superposition —The principle that a layer of rocks is older than any other layer that lies above it and younger than any other layer that lies below it.

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Similar presentations More Presentation on theme: Relative Dating Determining relative ages of rocks or strata compared to another rock or strata.

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Correlation (Geology) - Absolute Vs. Relative Ages Of Strata

Geology[ edit ] The regular order of the occurrence of fossils in rock layers was discovered around by William Smith. While digging the Somerset Coal Canal in southwest England, he found that fossils were always in the same order in the rock layers. As he continued his job as a surveyor , he found the same patterns across England. He also found that certain animals were in only certain layers and that they were in the same layers all across England. Due to that discovery, Smith was able to recognize the order that the rocks were formed.

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