The utility of stratigraphy for dating purposes is based on the fact that

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Learning Geology. Subscribe To Posts Atom. Comments Atom. Types of stratigrpahy There are several types of stratigraphy that are described below. Geochronology, the science of absolute dating of rocks and determining the time sequence of geological events in Earth's history, particularly by radiometric dating, developed largely at the turn of the 20th Century and during its first three decades with the advent of atomic and nuclear physics and quantum theory e.
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Stratigraphy

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Stratigraphy: Earth's Geological, Archaeological Layers

This makes geology partially philosophical science since we never know the extent and real dimension of time. In this case our own place in time is just a flick among series of evolutionary events. However, as humans we are always ready to place ourselves as central or influential figures. Then we get a slap in the face from Mother Nature, but unfortunately we never learn. Geologists analyze geologic time in two different ways: in terms of relative geologic age , and in terms of absolute or numeric geologic age.
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Rubidium–strontium dating

The rubidium-strontium dating method is a radiometric dating technique used by scientists to determine the age of rocks and minerals from the quantities they contain of specific isotopes of rubidium 87 Rb and strontium 87 Sr, 86 Sr. Development of this process was aided by German chemists Otto Hahn and Fritz Strassmann , who later went on to discover nuclear fission in December The utility of the rubidium — strontium isotope system results from the fact that 87 Rb one of two naturally occurring isotopes of rubidium decays to 87 Sr with a half-life of In addition, Rb is a highly incompatible element that, during partial melting of the mantle, prefers to join the magmatic melt rather than remain in mantle minerals.
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The problem : By the mid 19th century it was obvious that Earth was much older than years, but how old? This problem attracted the attention of capable scholars but ultimately depended on serendipitous discoveries. Early attempts : Initially, three lines of evidence were pursued: Hutton attempted to estimate age based on the application of observed rates of sedimentation to the known thickness of the sedimentary rock column, achieving an approximation of 36 million years.
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