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AVONIAN

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Originally appearing in Volume V03, Page 67 of the 1911 Encyclopedia Britannica.
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AVONIAN , in See also:

geology, the name proposed by Dr A. See also:Vaughan in 1905 (Q.J.G.S. vol. lxi. p. 264) for the rocks of See also:Lower Carboniferous See also:age in the See also:Avon See also:gorge at See also:Bristol. The Avonian See also:stage appears to embrace precisely the same rocks and fossil-zones as the earlier designation " Dinantien " (see CARBONIFEROUS See also:SYSTEM) ; but its substages, being founded upon different See also:local conditions and a different See also:interpretation of the zonal fossils, do not correspond exactly with those of the See also:French and Belgian geologists. Substages. ZONES. Substages. Kidwellian .Dibunophyllum- Seminula Syringothyris Clevedonian Zaphrentis Tournaisien ,Cleistopora The upper Avonian (Kidwellian) is well See also:developed about See also:Kidwelly in See also:Carmarthenshire. The lower substage (Clevedonian) is well displayed near See also:Clevedon in See also:Somerset. See A. Vaughan, " The Carboniferous See also:Limestone See also:Series (Avonian) of the Avon Gorge," Proc. Bristol Naturalists' See also:Soc., 4th series, vol. i. pt.

2, 1906, pp. 74-168 (many plates) ; and T. F. Sibley, " On the Carboniferous Limestone (Avonian) of the Mendip See also:

area (Somerset)," Q.J.G.S. vol. ]Iii., 1906, pp. 324-380 (plates). (J. A.

End of Article: AVONIAN

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