The Quarterly journal of the Geological Society of London . carinafiini ?Hucclecote ?(Stout Acantli.) 1205. iBeanic.:[ turn ;Ac. spp. ;Liparnc. 1. cheltiense X7 Cbarlton Kings; Radstock: 120 rt. Liparoc. {Lip. hepf- Dumbleton, etc. Dundry. augnlare) {L. cheltiense) {Lip. zieteni 1 The numbers refer to beds in Geol. Whitby 2nd ed. Mem. Geol. Surv. 1915,p. 69; the strata are about 155 feet thick, Bed 7 being 35 feet. - Specimens collected by my father, and personal observations. ?^ Mr. J. W. Tutchers information. i W. D. Lang, Proc. Geol. Assoc, vol. xxv (1914) p. 293 ;
The Quarterly journal of the Geological Society of London . carinafiini ?Hucclecote ?(Stout Acantli.) 1205. iBeanic.:[ turn ;Ac. spp. ;Liparnc. 1. cheltiense X7 Cbarlton Kings; Radstock: 120 rt. Liparoc. {Lip. hepf- Dumbleton, etc. Dundry. augnlare) {L. cheltiense) {Lip. zieteni 1 The numbers refer to beds in Geol. Whitby 2nd ed. Mem. Geol. Surv. 1915,p. 69; the strata are about 155 feet thick, Bed 7 being 35 feet. - Specimens collected by my father, and personal observations. ?^ Mr. J. W. Tutchers information. i W. D. Lang, Proc. Geol. Assoc, vol. xxv (1914) p. 293 ; the numbers are thoseof his beds. In regard to this and the following tables, my best thanks are dueto Mr. Lang for the great pains that be has taken to supply me with information,sending MS. notes of later researches and sul)mitting specimens—my in square brackets. Since this paper was read he has published some of theseMS. notes—The i6ea--Zone Proc. Geol. Assoc, vol. xxviii (1917) p. 31. [X Fauna present, position surmised.]. NVIHSIAlOa NVID3IMH The accompanyingdiagram (fig. A) showsthe famial sequences,and non-sequences, inthe Domerian andHwiccian of the areasunder account is takenof the thicknesses ofstrata; it is only afauna! record; but itbecomes a stratigra-phical illustration ofthe position of affairswhen the concludingstrata of the Domerianw^ere deposited. The datum-line is7 Domerian {spina-tuni) proved in allareas. The movement ofthe Men dip axis ofNorth Somerset isquite obvious. Itsinfluence apparentlyextended to Grlouces-•tershire. On the Dor-set Coast, though theDomerian strata areespecially thick, thereare two more non-sequences, due possiblyto movement of the^Ve^anouth last of these, thepre - spinci f um one,which presumably co-incides mth the lackof the IcBvU zone ofRaasay, is particularlyinteresting. The baseof spinafum has BlueLias pebbles, the dateof which it would beinteresting to deter-mine. If, as
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Keywords: ., bookcentury1800, bookdecade1840, booksubjectgeology, bookyear1845
