The Quarterly journal of the Geological Society of London . in Proc. Cotteswold Nat. Field-Club, vol. ix. pt. ii. (1887)p. 1142; and the Frith section may be advantageously comparedtherewith. It will be seen that at the Frith there is 19 feet 9 inchesof strata in the Oolite Marl series above the Rh. , 1 It might arise from divergence; and this term proposed does not commitus to the means whereby the result is obtained, it only describes the effectproduced. 2 Of Bed 21 of that section 9 lbs. yielded 563 specimens, excluding micro-morphs ; they were mostly brachiopoda. Many
The Quarterly journal of the Geological Society of London . in Proc. Cotteswold Nat. Field-Club, vol. ix. pt. ii. (1887)p. 1142; and the Frith section may be advantageously comparedtherewith. It will be seen that at the Frith there is 19 feet 9 inchesof strata in the Oolite Marl series above the Rh. , 1 It might arise from divergence; and this term proposed does not commitus to the means whereby the result is obtained, it only describes the effectproduced. 2 Of Bed 21 of that section 9 lbs. yielded 563 specimens, excluding micro-morphs ; they were mostly brachiopoda. Many were crushed. Vol. •] OF THE MID-COXTESWOLDS. 459 and that there is practically nothing below it; while at NotgroveStation there is 18 feet 1 inch of rock above this horizon, and14 feet 9 inches below it. This at any rate explains why Notgroveis the more prolific below. Table VIII. Diagrammatic Table to show the sequence in the acmes of develop-ment of various species of brachiopoda—the greatest divergence in thelines indicating the acme in each 3 q Base ofO. M. atthe Frith. Base ofO. M. at NotgroveStation.
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Keywords: ., bookcentury1800, bookdecade1840, bookidquarte, booksubjectgeology
