. The Quarterly journal of the Geological Society of London. this district is the position of theNeseran Beds, already ascertained from Mr. Walfords researches. They linkup the marine Fullers Earth strata of the south-west with the tipperEstuarine deposits of Yorkshire, and thus enable the date to be fixed for theYorkshire beds. The Authors use of the term Concinna Beds is inadvisable. Bhyncho-oiella concinna is a species of the Cornbrash. Various more or less concinva-like lUrynchonellm are found in earlier rocks, but to give them the name of the-Cornbrash species is misleading. There is a so
. The Quarterly journal of the Geological Society of London. this district is the position of theNeseran Beds, already ascertained from Mr. Walfords researches. They linkup the marine Fullers Earth strata of the south-west with the tipperEstuarine deposits of Yorkshire, and thus enable the date to be fixed for theYorkshire beds. The Authors use of the term Concinna Beds is inadvisable. Bhyncho-oiella concinna is a species of the Cornbrash. Various more or less concinva-like lUrynchonellm are found in earlier rocks, but to give them the name of the-Cornbrash species is misleading. There is a somewhat large inconstant]formBhynchonella which occurs in, and is characteristic of, certain Fullers Earthdeposits of the Ardley Cutting. So far as I know, it does not occur in otherdistricts; but it should not be called Eli. concinna. 1 [This paper, under the title of Some New Oolitic Strata in North Oxford-shire, was afterwards privately printed : Buckingham, 1906.] Quart. Journ. Geol. Soc. Vol. LXIX, UPPER GREEN HILL QUARRY, Eastern ies Subsoil & rubbly limestonesvery fossiltferous. XiSiEfiaffiDLl limestoneLine of rolled nodules. Sandy marl, (A) False-bedded Limestones and \ ,<..,- . i\ ? ^^^SP Marls (Beds )) Fl6. 2. LOWER GREEN HILL QUARRY.
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Keywords: ., bookcentury1800, bookdecade1840, booksubjectgeology, bookyear1845
