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  2. Geological history of Earth - Wikipedia

    en.wikipedia.org/wiki/Geological_history_of_Earth

    The geological history of the Earth follows the major geological events in Earth's past based on the geological time scale, a system of chronological measurement based on the study of the planet's rock layers ( stratigraphy ). Earth formed about 4.54 billion years ago by accretion from the solar nebula, a disk-shaped mass of dust and gas left ...

  3. Historical geology - Wikipedia

    en.wikipedia.org/wiki/Historical_geology

    Historical geology. Historical geology or palaeogeology is a discipline that uses the principles and methods of geology to reconstruct the geological history of Earth. [ 1] Historical geology examines the vastness of geologic time, measured in billions of years, and investigates changes in the Earth, gradual and sudden, over this deep time.

  4. History of geology - Wikipedia

    en.wikipedia.org/wiki/History_of_geology

    In 1741 the best-known institution in the field of natural history, the National Museum of Natural History in France, created the first teaching position designated specifically for geology. [19] This was an important step in further promoting knowledge of geology as a science and in recognizing the value of widely disseminating such knowledge.

  5. John Renton - Wikipedia

    en.wikipedia.org/wiki/John_Renton

    John J. "Jack" Renton (1933 – February 28, 2020) [1] was a professor of geology at West Virginia University, known for the quality of the teaching in his introductory geology courses [2] and in the video version of the course, Nature of Earth. [3] In 2001 he received the WVU Eberly College of Arts & Sciences Outstanding Teacher Award, the WVU ...

  6. Principles of Geology - Wikipedia

    en.wikipedia.org/wiki/Principles_of_Geology

    The first rule is that geologic change comes from slow and continual procedures that have been happening over a long period of time. [ 8 ] This rule is the basic ideal of Uniformitarianism and is easy to understand why this was a rule. The second rule is that all the forces that affect the geology of the Earth comes from the Earth. [ 8 ]

  7. Geochronology - Wikipedia

    en.wikipedia.org/wiki/Geochronology

    Geochronology. An artistic depiction of the major events in the history of Earth. Geochronology is the science of determining the age of rocks, fossils, and sediments using signatures inherent in the rocks themselves. Absolute geochronology can be accomplished through radioactive isotopes, whereas relative geochronology is provided by tools ...

  8. History of Earth - Wikipedia

    en.wikipedia.org/wiki/History_of_Earth

    The history of the Earth can be organized chronologically according to the geologic time scale, which is split into intervals based on stratigraphic analysis. [2] [21] The following five timelines show the geologic time scale to scale. The first shows the entire time from the formation of the Earth to the present, but this gives little space ...

  9. William Smith (geologist) - Wikipedia

    en.wikipedia.org/wiki/William_Smith_(geologist)

    The Geological Society of London presents an annual lecture in his honour. In 2005, a William Smith 'facsimile' was created at the Natural History Museum as a notable gallery character to patrol its displays; others were Carl Linnaeus, Mary Anning, and Dorothea Bate. [35] His work was an important foundation for the work of Charles Darwin.

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