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KIMERIDGIAN , in geology, the basal division of the Upper Oolites in theSee also: Jurassic See also: system
.
The name is derived from the See also: hamlet of Kimeridge or Kimmeridge near the See also: coast of Dorset-See also: shire, See also: England
.
It appears to have been first suggested by T
.
See also: Webster in 1812; in 1818, in the See also: form Kimeridge See also: Clay, it was used by Buckland
.
From the See also: Dorsetshire coast, where it is splendidly exposed in the See also: fine cliffs from St See also: Alban's See also: Head to See also: Gad Cliff, it follows the See also: line of Jurassic outcrop through Wilt-shire, where there is a broad expanse between Westbury and See also: Devizes, as far as See also: Yorkshire, there it appears in the vale of Pickering and on the coast in See also: Filey See also: Bay
.
It generally occupied broad valleys, of which the vale of See also: Aylesbury may be taken as typical
.
See also: Good exposures occur at Seend, See also: Caine, See also: Swindon, Wootton Bassett, See also: Faringdon, See also: Abingdon, Culham, Shotover See also: Hill,
See also: Brill, See also: Ely and Market Kasen
.
Traces of the formation are found as far See also: north as the See also: east ccast of Cromarty and See also: Sutherland at Eathie and Helmsdale
.
In England the Kimeridgian is usually divisible into an Upper Series, 600-650 ft. in the See also: south, dark bituminous shales, paper
shales and See also: clays with layers and nodules of cement-stones and septaria
.
These beds See also: merge gradually into the overlying See also: Portlandian formation
.
The See also: 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 See also: common in the upper See also: part of the lower division, and the lower part of the Upper Kimeridgian
.
A large number of See also: ammonites are See also: peculiar to this formation, including Reineckia See also: 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
.
See also: 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, See also: Gillingham, Brill, Ely, Horncastle, and other places
.
The so-called "Kimeridge See also: 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 See also: continental geologists is usually made to contain the three sub-divisions of A
.
See also: Oppel and W
.
Waagen, Upper (Virgulian) with Exogyra virgula Kimeridgien See also: Middle (Pteroceran) with Pteroceras oceani
Lower (Astartian) with See also: Astarte supracorallina; but the upper portion of this continental Kimeridgian is See also: equivalent to some of the See also: British Portlandian; while most of the Astartian corresponds to the See also: 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 See also: northern See also: Europe, including See also: Russia
.
In See also: Swabia and some other parts of See also: Germany the curious ruiniform marble Felsenkalk occurs on this See also: horizon, and most of the Kimeridgien of See also: southern Europe, including the See also: Alps, is calcareous
..
Representatives of the formation occur in See also: Caucasia, See also: Algeria, See also: Abyssinia, See also: Madagascar; in South See also: America with volcanic rocks, and possibly in California (Maripan beds), See also: Alaska and See also: King
See also: Charles's
See also: Land
.
See " Jurassic Rocks of Britain," vols. v. and i., See also: Memoirs of the See also: Geological Survey (vol. v. contains references to literature up to 1895)
.
(J
.
A
.
H.)
KIl1JI, or QIMHI, the See also: family name of three Jewish grammarians and biblical scholars who worked at See also: Narbonne in the 12th century and the beginning of the 13th, and exercised See also: great influence on the study of the See also: Hebrew language
.
The name, as is shown by See also: manuscript testimony, was also pronounced Xamhi and further mention is made of the French surname See also: Petit
.
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