Online Encyclopedia

KIMERIDGIAN

Online Encyclopedia
Originally appearing in Volume V15, Page 800 of the 1911 Encyclopedia Britannica.
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KIMERIDGIAN  , in

geology, the basal division of the Upper Oolites in the
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Jurassic
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system . The name is derived from the
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hamlet of Kimeridge or Kimmeridge near the coast of Dorset-
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shire, England . It appears to have been first suggested by T . Webster in 1812; in 1818, in the form Kimeridge Clay, it was used by Buckland . From the Dorsetshire coast, where it is splendidly exposed in the
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fine cliffs from St
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Alban's Head to
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Gad Cliff, it follows the
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line of Jurassic outcrop through Wilt-shire, where there is a broad expanse between Westbury and
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Devizes, as far as
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Yorkshire, there it appears in the vale of Pickering and on the coast in
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Filey
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Bay . It generally occupied broad valleys, of which the vale of
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Aylesbury may be taken as typical . Good exposures occur at Seend, Caine,
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Swindon, Wootton Bassett,
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Faringdon,
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Abingdon, Culham, Shotover Hill,
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Brill, Ely and Market Kasen . Traces of the formation are found as far north as the east ccast of Cromarty and Sutherland at Eathie and Helmsdale . In England the Kimeridgian is usually divisible into an Upper Series, 600-650 ft. in the south, dark bituminous shales, paper shales and clays with layers and nodules of cement-stones and septaria . These beds
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merge gradually into the overlying
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Portlandian formation . The
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Lower Series, with a maximum thickness of 40o ft., consists of clays and dark shales with septaria, cement-stones and calcareous " doggers." These lithological characters are very persistent . The Upper Kimeridgian is distinguished as the zone of Perisphinctes biplex, with the sub-zone of Discina latissima in the higher portions .

Cardioceras alternans is the zonal ammonite characteristic of the lower division, with the sub-zone of Ostrea deltoidea in the lower portion . Exogyra virgula is

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common in the upper
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part of the lower division, and the lower part of the Upper Kimeridgian . A large number of
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ammonites are
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peculiar to this formation, including Reineckia
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eudoxus, R . Thurmanni, Aspidoceras longispinus, &c . Large dinosaurian reptiles are abundant, Cetiosaurus, Gigantosaurus, Megalosaurus, also plesiosaurs and ichthyosaurs; crocodilian and chelonian remains are also found . Protocardia striatula, Thracia depressa, Belemnites abreviatus, B . Blainvillei, Lingula ovalis, Rhynchonella inconstans and Exogyra nana are characteristic fossils .
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Alum has been obtained from the Kimeridge Clay, and the cement-stones have been employed in Purbeck; coprolites are found in small quantities . Bricks, tiles, flower-pots, &c., are made from the clay at Swindon,
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Gillingham, Brill, Ely, Horncastle, and other places . The so-called "Kimeridge
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coal" is a highly bituminous shale cap-able of being used as fuel, which has been worked on the cliff at Little Kimeridge . The " Kimeridgien " of
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continental geologists is usually made to contain the three sub-divisions of A . Oppel and W .

Waagen, Upper (Virgulian) with Exogyra virgula Kimeridgien
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Middle (Pteroceran) with Pteroceras oceani Lower (Astartian) with
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Astarte supracorallina; but the upper portion of this continental Kimeridgian is
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equivalent to some of the
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British Portlandian; while most of the Astartian corresponds to the Corallian . A. de Lapparent now recognizes only the Virgulian and Pteroceran in the Kimeridgien . Clays and marls with occasional limestones and sandstones represent the Kimeridgien of most of
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northern
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Europe, including Russia . In Swabia and some other parts of Germany the curious ruiniform marble Felsenkalk occurs on this horizon, and most of the Kimeridgien of
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southern Europe, including the
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Alps, is calcareous .. Representatives of the formation occur in Caucasia, Algeria, Abyssinia,
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Madagascar; in South
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America with volcanic rocks, and possibly in California (Maripan beds),
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Alaska and King Charles's
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Land . See " Jurassic Rocks of Britain," vols. v. and i.,
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Memoirs of the
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Geological Survey (vol. v. contains references to literature up to 1895) . (J . A . H.) KIl1JI, or QIMHI, the
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family name of three Jewish grammarians and biblical scholars who worked at
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Narbonne in the 12th century and the beginning of the 13th, and exercised
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great influence on the study of the
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Hebrew language . The name, as is shown by
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manuscript testimony, was also pronounced Xamhi and further mention is made of the French surname Petit .

End of Article: KIMERIDGIAN
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