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BRITISH FOSSILIFEROUS LOCALITIES 
Jurassic, Inferior Oolite (resting on Upper Lias, Ham Hill Stone). Brachio- 
pods ( Homoeorhynchia cynocephala , etc.) are common and an occasional ammonite 
occurs, 
Kellaway, G. A. and Wilson, V. 1941, p. 180. 
Geol. Surv. O.S. 18 ; Ord. New Pop. 155. 
Weston-in-Gordano, 3 miles N.E. of Clevedon. Nightingale and Black 
Rock Quarries, N.E. and E. of the village. 
Carboniferous Limestone (Z and C zones), with corals and brachiopods. 
Reynolds, S. H. and Greenly, E. 1924, pp. 448, 450, with geol. map. 
Geol. Surv. O.S. 35 ; Ord. New Pop. 155. 
Weston-super-Mare. Spring Cove, 200 yds. N. of the pier. 
Carboniferous Limestone (C t subzone). A bed composed almost entirely 
of the coral Caninia subibicina crops out in the cliff by path to shore. 
Vaughan, A. 1905, p. 552. 
Geol. Surv. O.S. 20 ; Ord. New Pop. 165. 
Wheddon Cross, 5| miles S.W. of Dunster. Middle Devonian, Ilfracombe 
Beds, with a varied coral fauna and some crinoids, brachiopods, etc. 
Hicks, H. 1896, p. 364. 
Geol. Surv. O.S. 20 ; Ord. New Pop. 164. 
Winford, 6 miles S.W. of Bristol. Small quarry \ mile S. of Winford, ora 
Crown Hill, on W. side of lane about 300 yds. N. of Crown Inn. 
Carboniferous, “ Millstone Grit ” with plentiful, but badly-preserved, 
goniatites. 
Geol. Surv. O.S. 19 \ Ord. New Pop. 165. 
Withycombe, 4 miles W. of Williton. Old quarries near Sandhill Farm, 
$ mile S.E. of Withycombe. 
Middle Devonian, Ilfracombe Beds, with a rich coral fauna. 
Perceval, S. G. 1866. 
Geol. Surv. O.S. 20 ; Ord. New Pop. 164. 
Wiveliscombe, 9£ miles W.N.W. of Taunton. Quarries near Oakhamptora 
House, If miles N. of Wiveliscombe. 
Upper Devonian, Morte Slates, with brachiopods, lamellibranchs and 
trilobites. 
Ussher, W. A. E. 1908, p. 27. 
Geol. Surv. N.S. 295 ; Ord. New Pop. 164. 
Wriragton, 10 miles S.W. of Bristol. Quarries 300 yds. N.E. of Wringtora 
at S. end of Prestow Wood opposite Branches Cross. 
Carboniferous Limestone (D 2 subzone). A rich fauna of clisiophyllid and 
other corals and rare echinoderms (blastoids). 
Geol. Surv. O.S. 19 ; Ord. New Pop. 165. 
STAFFORDSHIRE 
Biddulph, 3 miles S.S.E. of Congleton (Cheshire). Spoil-heap from 
disused colliery at Woodhouse Lane, about 300 yds. S.E. of Wood house Farm 
and 700 yds. N.E. of the Oxhay, on lane to Biddulph Moor. 
Carboniferous, Coal Measures ( lenisulcata zone, marine band Ira roof of 
Crabtree Coal), with solid goniatites ( Gastrioceras listen ). 
Geol. Surv. N.S. 110 ; Ord. New Pop. 110. 
Brindley Ford, 3 miles N.N.E. of Tuns tali. Right bank of R. Trent in 
Lion’s Paw Wood, 170 yds. W.N.W. of Lion’s Paw Farm and 760 yds. N.N.E. 
of Judgefields. 
Carboniferous, Millstone Grit (G zone), with abundant goniatites (Gastric 
c&ras cancellation) and lamellibranchs . 
Geol. Surv. N.S. 110 and 123 $ Ord. New Pop. 110. 
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