"Crickley Member"@en . . . "Pale grey to yellowish brown limestones; lower part dominated by medium- to coarse-grained ooidal shell-fragmental grainstone ('Lower Limestone'), passing up into rubbly, poorly sorted, shelly, shell-detrital, moderately to highly pisoidal grainstones and packstones ('Pea Grit') with thin marl beds. South of Painswick, the succession is apparently replaced by ooidal grainstones comprising the Frocester Hill Oolite and Selsey Hill Oolite of Mudge, D C, 1978a, but the relationship between these strata and the type Crickley Member is uncertain."@en . "Lower Limestone and Pea Grit [Obsolete: use CRKY]"@en . "Frocester Hill Oolite and Selsey Hill Oolite [Obsolete: use CRKY, CLCL]"@en . "Crickley Limestone and Crickley Oncolite [Obsolete: use CRKY]"@en . . "Upward transition from ferruginous, bioturbated, sandy, muddy shell-detrital limestone (Leckhampton Member) into limestones as described in lithology."@en . . "Upward gradation from pisoidal limestones as described in lithology, into ooidal grainstones (Cleeve Cloud Member) in mid and north Cotswolds; a non-sequence marked by a hardground in southern Cotswolds (Mudge, D C, 1978a)."@en . . . "CRKY"@en . "Crickley Member"@en . "Limestone with subsidiary calcareous mudstone. Stratified bedrock. Occurs onshore. Deposited during the Aalenian Age (Jurassic Period) (174.7-170.9 Ma BP)."@en . . . . "Typically about 7m. Type section (Crickley Hill); c.15.7m, probably the maximum (Ager, D V, 1969)."@en . "174.7"^^ . . "170.9"^^ . "stable"@en . . "Pea Grit Series [Obsolete: use CRKY]"@en . .