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CARADOC See also:SERIES , in See also:geology, the name introduced by R. I. See also:Murchison in 1839 for the See also:sandstone series of Caer Caradoc in See also:Shropshire, See also:England. The limits of Murchison's Caradoc series have since been somewhat modified, and through the labours of C. See also:Lapworth the several members of the series have been precisely defined by means of graptolitic zones. These zones are identical with those found in the rocks of the same See also:age in See also:North See also:Wales, the See also:Bala series (q.v.), and the terms Bala or Caradoc series are used indifferently by geologists when referring to the uppermost substage of the Ordovician See also:System. The Ordovician rocks of the Caradoc See also:district have been sub-divided into the following beds, in descending See also:order: the Trinucleus shales, See also:Acton See also:Scott beds, Longville flags, Chatwell and Soudley sandstones, Harnage shales and See also:Hoar Edge grits and See also:limestone. In the Corndon district in the same See also:county the Caradoc series is represented by the Marrington See also:group of ashes and shales and the See also:Spy See also:Wood group beneath them; these two See also:groups of strata are sometimes spoken of as the Chirbury series. In the Breidden district are the barren Criggeon shales with ashes and flows of See also:andesite. In the See also:Lake district the Coniston limestone series represents the Upper Caradocian, the See also:lower portion being taken up by See also:part of the See also:great Borrowdale volcanic series of rocks. The Coniston limestone series contains the following subdivisions: Ashgill group (Ashgill shales and Staurocephalus limestone). Kiesley limestone. Sleddale group (Applethwaite beds = Upper Coniston limestone See also:conglomerate; Yarlside See also:rhyolite; stye end beds=Lower Coniston limestone. See also:Roman See also:Fell group (See also:Corona beds). The Dufton shales and Drygill shales are equivalents of the Sleddale group. Rocks of Caradoc age are well See also:developed in See also:southern See also:Scotland; in the See also:Girvan district they have been described as the Ardmillan series with the Drummock group and Barren Flagstone group in the upper portion, and the Whitehouse, Ardwell and Balclatchie groups in the lower part. Similarly, two divisions, known as the Upper and Lower See also:CARALES Hartfell series, are recognized in the southern and central See also:area, in See also:Peeblesshire, See also:Ayrshire and See also:Dumfriesshire. In See also:Ireland the Caradoc or Bala series is represented by the See also:lime-stones of Portraine near See also:Dublin and of the See also:Chair of See also:Kildare; by the See also:Ballymoney series of See also:Wexford and Carnalea shales of Co. Down. In the Lough See also:Mask district beds of this age are found, as in Wales, interstratified with volcanic lavas and tuffs. Other localities are known in counties See also:Tyrone, See also:Meath and See also:Louth, also in Lambay See also:Island. See ORDOVICIAN SYSTEM; also C. Lapworth, See also:Ann. and Mag. Nat. Hist., 5th series, vol. vi., 188o; Geol. Mag., 1889; C. Lapworth and W. W. See also:Watts, Proc. Geol. Assoc., xiii., 1894; J. E. Marr, Geol. Mag., 1892; J. E. Marr and T. See also:Roberts, Q. J. G. S., 1885; B. N. See also:Peach and J. See also:Horne, " See also:Silurian Rocks of Great See also:Britain," vol. T., 1899 (Mem. Geol. Survey). (J. A. Additional information and CommentsThere are no comments yet for this article.
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