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The Caithness Flagstone Group is a Devonian lithostratigraphic group (a sequence of rock strata) in northern Scotland. The name is derived from the traditional county of Caithness where the strata are well exposed, especially in coastal cliffs.
Rocks formations and the Dedo de Deus (God's Finger) peak in the background, Serra dos Órgãos National Park, Rio de Janeiro state, Brazil Raouché or Pigeons' Rock in Beirut, Lebanon Druid Arch, Canyonlands National Park, Utah, US View of Meteora, Greece Rock formations in Ongamira Valley, Sierras de Córdoba, Argentina Belogradchik Rocks, Balkan Mountains, Bulgaria "Jaws", an erosional fin ...
The group outcrops near Whitehaven on the Cumbrian coast and beneath the Vale of Eden. It comprises the St Bees Evaporite and the overlying St Bees Shale Formation which are between 0 and 100m and 0 and 215m thick respectively. [1] The lower formation sits atop the mixed lithology breccia known as Brockram. [2]
Significant coastal limestone quarries were also active at Lydstep and Caldey. [10] Slate was quarried at Caersalem Quarry at Porthgain and exported via the village harbour. Many older buildings and field walls have been constructed from locally sourced stone from riverbeds and hillsides.
The Coastal Plain includes the Sandhills or Carolina Sandhills, a 10–35 mi (16–56 km) wide region within the Atlantic Coastal Plain province. [9] Rocks in the exposed Coastal Plain region of Georgia range from the Late Cretaceous Tuscaloosa Formation to modern Holocene sediments actively forming along the Atlantic coast.
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The Franciscan Complex or Franciscan Assemblage is a geologic term for a late Mesozoic terrane of heterogeneous rocks found throughout the California Coast Ranges, and particularly on the San Francisco Peninsula.
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