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  2. Lithostratigraphy - Wikipedia

    en.wikipedia.org/wiki/Lithostratigraphy

    The surface stratum resulting is called an unconformity. Four types of unconformity: Angular unconformity: younger sediment lies upon an eroded surface of tilted or folded older rocks. The older rock dips at a different angle from the younger. Disconformity: the contact between younger and older beds is marked by visible, irregular erosional ...

  3. Unconformity - Wikipedia

    en.wikipedia.org/wiki/Unconformity

    An unconformity is a buried erosional or non-depositional surface separating two rock masses or strata of different ages, indicating that sediment deposition was not continuous. In general, the older layer was exposed to erosion for an interval of time before deposition of the younger layer, but the term is used to describe any break in the ...

  4. Hutton's Unconformity - Wikipedia

    en.wikipedia.org/wiki/Hutton's_Unconformity

    Hutton's Unconformity is a name given to various notable geological sites in Scotland identified by the 18th-century Scottish geologist James Hutton as places where the junction between two types of rock formations can be seen. This geological phenomenon marks the location where rock formations created at different times and by different ...

  5. Torridon Group - Wikipedia

    en.wikipedia.org/wiki/Torridon_Group

    The sequence is made up of 22 m thick cycles, each with a basal erosion surface followed by dark grey shales with desiccation cracks, planar cross-bedded sandstones with wave rippled tops, overlain by trough cross-bedded micaceous sandstones. These cycles are thought to represent repeated progradation of deltas into a lake.

  6. Cross-cutting relationships - Wikipedia

    en.wikipedia.org/wiki/Cross-cutting_relationships

    Cross-cutting relationships can be used to determine the relative ages of rock strata and other structures. Explanations: A – folded rock strata cut by a thrust fault; B – large intrusion (cutting through A); C – erosional angular unconformity (cutting off A & B) on which rock strata were deposited; D – volcanic dike (cutting through A, B & C); E – even younger rock strata (overlying ...

  7. Uniformitarianism - Wikipedia

    en.wikipedia.org/wiki/Uniformitarianism

    Hutton's Unconformity at Jedburgh. Above: John Clerk of Eldin's 1787 illustration. Below: 2003 photograph. Uniformitarianism, also known as the Doctrine of Uniformity or the Uniformitarian Principle, [1] is the assumption that the same natural laws and processes that operate in our present-day scientific observations have always operated in the universe in the past and apply everywhere in the ...

  8. Geology of Missouri - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Missouri

    The Great Unconformity separates Proterozoic igneous rocks from the Lamotte Sandstone, the basal unit of the Sauk sequence which also includes the Bonneterre Dolomite, Davis Formation, Derby-Roe Run Dolomite, Potosi Dolomite and Eminence Dolomite from the Cambrian, and the Ordovician Gasconade Dolomite, Roubidoux Formation and Jefferson City ...

  9. Phosphor - Wikipedia

    en.wikipedia.org/wiki/Phosphor

    For displaying of a limited palette of colors, there are a few options. In beam penetration tubes, different color phosphors are layered and separated with dielectric material. The acceleration voltage is used to determine the energy of the electrons; lower-energy ones are absorbed in the top layer of the phosphor, while some of the higher ...