The Quarterly journal of the Geological Society of London . Upper Freestone ale: Horizontal, \ inch = 1 mile. of deposit. The line marked Horizon of Terebratulaiany localities, the species is found so plentifully. It>mbe in conformity with the Kimsbury Castle section. Quart. Journ. Geol. Soc. Vol. LI. TABLE VI.—STRATIGRAPHICAL DIAGRAM. 1 III 2 h |. Scale: Veitical, 1 inch = 10 feet (1 era. = 4 feet). b Upper Freestoi Scale: Horizontal, J inch = 1 milo. Jfate. Tlio upper boundary of the Upper Trigonia-gvil is not intended to denote any particular tliicknp f deposit. The line marked Horizon o
The Quarterly journal of the Geological Society of London . Upper Freestone ale: Horizontal, \ inch = 1 mile. of deposit. The line marked Horizon of Terebratulaiany localities, the species is found so plentifully. It>mbe in conformity with the Kimsbury Castle section. Quart. Journ. Geol. Soc. Vol. LI. TABLE VI.—STRATIGRAPHICAL DIAGRAM. 1 III 2 h |. Scale: Veitical, 1 inch = 10 feet (1 era. = 4 feet). b Upper Freestoi Scale: Horizontal, J inch = 1 milo. Jfate. Tlio upper boundary of the Upper Trigonia-gvil is not intended to denote any particular tliicknp f deposit. The line marked Horizon of Ten-hrahila Buckmani is inlended \ fdmw the position of tin- mnrl-ti.:d, beluw tin- uand-bed, wherein, at inmiy Ln-nlities, tlie species is found ko plentifully. Itshould be dotted at Buckholt Wood, and from Wistlej to past Hilcot. It is mavked at Sheepscoinbe in conformity with the Kimsbury Castle section. Yol. 51.] OF THE MID-COTTESWOLDS. 431 Table VI. (plain lines) shows a rapid rise in the thickness of the intervening beds from Mount Surat to Stroud Hill. The thicknessis maintained to Sheepscombe, and then a decline commences, whichbecomes very rapid between Buckholt and Cranham Woods. Next,after passing Birdlip, there is a rapid rise, the line for which travelsnearly straight from Tuffleys to Ravensgate, the only deviation froms
Size: 2392px × 1045px
Photo credit: © The Reading Room / Alamy / Afripics
License: Licensed
Model Released: No
Keywords: ., bookcentury1800, bookdecade1840, bookidquarte, booksubjectgeology
