Dating igneous rocks

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Ringing rocks are used in idiophonic musical instruments called lithophones. Several early scientists became interested in the ringing rocks; however, none were able to formulate a credible theory on the ringing ability of the rocks or the formation of the boulder fields. Edgar T. Wherry — , mineralogist and botanist , became interested in the ringing rocks while teaching at Lehigh University. Wherry theorized that the ringing was due to the texture of the diabase rocks and that they were supported by other rocks.
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Igneous petrology - Wikipedia

Originally fossils only provided us with relative ages because, although early paleontologists understood biological succession, they did not know the absolute ages of the different organisms. It was only in the early part of the 20th century, when isotopic dating methods were first applied, that it became possible to discover the absolute ages of the rocks containing fossils. In most cases, we cannot use isotopic techniques to directly date fossils or the sedimentary rocks they are found in, but we can constrain their ages by dating igneous rocks that cut across sedimentary rocks, or volcanic ash layers that lie within sedimentary layers. Isotopic dating of rocks, or the minerals in them, is based on the fact that we know the decay rates of certain unstable isotopes of elements and that these rates have been constant over geological time. One of the isotope pairs widely used in geology is the decay of 40 K to 40 Ar potassium to argon
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Fossil and Radioisotope Dating

The complex of data recorded in fossils worldwide—known as the fossil record —is the primary source of information about the history of life on Earth. Only a small fraction of ancient organisms are preserved as fossils, and usually only organisms that have a solid and resistant skeleton are readily preserved. Most major groups of invertebrate animals have a calcareous skeleton or shell e. Other forms have shells of calcium phosphate which also occurs in the bones of vertebrates , or silicon dioxide.
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The rock components of the crust are slowly but constantly being changed from one form to another and the processes involved are summarized in the rock cycle Figure 3. The rock cycle is still active on Earth because our core is hot enough to keep the mantle moving, our atmosphere is relatively thick, and we have liquid water. On some other planets or their satellites, such as the Moon, the rock cycle is virtually dead because the core is no longer hot enough to drive mantle convection and there is no atmosphere or liquid water. Magma can either cool slowly within the crust over centuries to millions of years — forming intrusive igneous rock, or erupt onto the surface and cool quickly within seconds to years — forming extrusive igneous rock. Intrusive igneous rock typically crystallizes at depths of hundreds of metres to tens of kilometres below the surface.
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