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  2. Elugelab - Wikipedia

    en.wikipedia.org/wiki/Elugelab

    The detonation produced a crater 1.9 km (6,200 ft) in diameter and 50 m (160 ft) deep where Elugelab had once been; [9] the blast and water waves from the explosion (some waves up to 6.1 m or 20 ft high) stripped the test islands clean of vegetation, as observed by a helicopter survey within 60 minutes after the test, by which time the mushroom ...

  3. Cleveland Shale - Wikipedia

    en.wikipedia.org/wiki/Cleveland_Shale

    The Cleveland Shale is a shale geologic formation in Ohio in the United States. The Cleveland Shale underlies much of northeast Ohio in beds of varying thickness. In northeast Ohio, the member does not appear east of the Grand River. [7] Measurements taken in northeast Ohio show the Cleveland Shale to be 7 feet (2.1 m) [7] to 100 feet (30 m ...

  4. Delay-action bomb - Wikipedia

    en.wikipedia.org/wiki/Delay-action_bomb

    A delay-action bomb is an aerial bomb designed to explode some time after impact, with the bomb's fuzes set to delay the explosion for times ranging from very brief to several weeks. Short delays are used to allow the bomb to penetrate before exploding: "a delay action bomb striking the roof of a tall building will penetrate through several ...

  5. List of Global Boundary Stratotype Sections and Points

    en.wikipedia.org/wiki/List_of_Global_Boundary...

    This is a list of Global Boundary Stratotype Sections and Points.Since 1977, Global Boundary Stratotype Sections and Points (abbreviated GSSPs) are internationally agreed upon reference points on stratigraphic sections of rock which define the lower boundaries of stages on the geologic time scale.

  6. Volcanic bomb - Wikipedia

    en.wikipedia.org/wiki/Volcanic_bomb

    A volcanic bomb or lava bomb is a mass of partially molten rock larger than 64 mm (2.5 inches) in diameter, formed when a volcano ejects viscous fragments of lava during an eruption. Because volcanic bombs cool after they leave the volcano, they are extrusive igneous rocks. Volcanic bombs can be thrown many kilometres from an erupting vent, and ...

  7. Nappe - Wikipedia

    en.wikipedia.org/wiki/Nappe

    In geology, a nappe or thrust sheet is a large sheetlike body of rock that has been moved more than 2 km (1.2 mi) [1] or 5 km (3.1 mi) [2] [3] above a thrust fault from its original position. Nappes form in compressional tectonic settings like continental collision zones or on the overriding plate in active subduction zones.

  8. Chagrin Shale - Wikipedia

    en.wikipedia.org/wiki/Chagrin_Shale

    Schematic showing the graded relationship of the Cleveland Member and Huron Member of the Ohio Shale to the Chagrin Shale. In Ohio, the Chagrin Shale underlies the Cleveland Shale [2] and overlies the Huron Shale. [3] It is a member of the Ohio Shale. [2] [2] [3] [7] The Chagrin Shale grades into and between the Cleveland and Huron Shales. [2] [2]

  9. Geological Survey of Ireland - Wikipedia

    en.wikipedia.org/wiki/Geological_Survey_of_Ireland

    Geological Survey Ireland produces maps, reports and databases, and acts as a knowledge centre and project partner in a number of aspects of Irish geology. [3] The organisation managed the Irish National Seabed Survey (INSS, 1999–2005), which on completion was the world's largest civilian marine mapping programme. The INSS mapped all of ...