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  2. The Journal of Geology - Wikipedia

    en.wikipedia.org/wiki/The_Journal_of_Geology

    The Journal of Geology publishes research on geology, geophysics, geochemistry, sedimentology, geomorphology, petrology, plate tectonics, volcanology, structural geology, mineralogy, and planetary sciences. Its content ranges from planetary evolution to computer modeling of fossil development, making it relevant to geologists as well as other ...

  3. Stormberg Group - Wikipedia

    en.wikipedia.org/wiki/Stormberg_Group

    The Stormberg Group is one of the four geological groups that comprises the Karoo Supergroup in South Africa. It is the uppermost geological group representing the final phase of preserved sedimentation of the Karoo Basin. The Stormberg Group rocks are considered to range between Lower Triassic (Olenekian) to Lower Jurassic (Pliensbachian) in age.

  4. Pediplain - Wikipedia

    en.wikipedia.org/wiki/Pediplain

    Pediplain. In geology and geomorphology a pediplain (from the Latin pes, genitive case pedis, meaning "foot") is an extensive plain formed by the coalescence of pediments. [1] The processes through which pediplains forms is known as pediplanation. [2] The concepts of pediplain and pediplanation were first developed by geologist Lester Charles ...

  5. History of geology - Wikipedia

    en.wikipedia.org/wiki/History_of_geology

    Antiquity. In the year 540 BC, Xenophanes described fossil fish and shells found in deposits on mountains. Similar fossils were noted by Herodotus (about 490 BC). [2][3][4] Some of the first geological thoughts were about the origin of the Earth. Ancient Greece developed some primary geological concepts concerning the origin of the Earth.

  6. Goldich dissolution series - Wikipedia

    en.wikipedia.org/wiki/Goldich_dissolution_series

    Goldich dissolution series. The Goldich dissolution series is a method of predicting the relative stability or weathering rate of common igneous minerals on the Earth's surface, with minerals that form at higher temperatures and pressures less stable on the surface than minerals that form at lower temperatures and pressures. Discontinuous.

  7. Hemipelagic sediment - Wikipedia

    en.wikipedia.org/wiki/Hemipelagic_sediment

    Hemipelagic sediment, or hemipelagite, is a type of marine sediment that consists of clay and silt-sized grains that are terrigenous and some biogenic material derived from the landmass nearest the deposits or from organisms living in the water. [1][2] Hemipelagic sediments are deposited on continental shelves and continental rises, and differ ...

  8. Analogue modelling (geology) - Wikipedia

    en.wikipedia.org/wiki/Analogue_modelling_(geology)

    Analogue modelling (geology) Pure shear sandbox model of thrust fault formation. Analogue modelling is a laboratory experimental method using uncomplicated physical models (such as a sandbox) with certain simple scales of time and length to model geological scenarios and simulate geodynamic evolutions. [ 1][ 2] There are numerous limitations ...

  9. Geological Magazine - Wikipedia

    en.wikipedia.org/wiki/Geological_Magazine

    ISSN. 0016-7568. Links. Journal homepage. Cambridge University Press page. The Geological Magazine is a peer-reviewed scientific journal established in 1864, covering the earth sciences. It publishes original scientific research papers on geological topics. The journal is published bimonthly by Cambridge University Press .