^32 PROCEEDINGS COTTESWOLD CLUB 1910 



Culver Hill, Amberley 



Thickness in feet inches 

 II. White Oolite i. Limestone, whitish, and apparently 



some marl, but inaccessible : seen . . 30 

 III. Clypeus-Grit 2. More conspicuous deposit of marl and 

 rubble ; Terebrattda globata, auctt. non 

 Sow., very common. [Holectypus de- 

 pressus (Leske), at Scar Hill. This is 

 the highest bed now visible at Scar Hill) i o 



3. Limestone, oolitic, thicker-bedded in 

 the lower portion, passing up into 

 whiter, thinner - bedded limestones ; 

 Ter. globata, auctt., non Sow., not un- 

 common in the massive beds : about 4 o 



4. Yellow, softish pisolitic marl and rubble ; 



Ter. globata, common, Clypeus Ploti, 

 Klein, Pleuromya Gold fussi (Lye), etc. 

 (At Scar Hill, i ft. 2 ins. thick, and 

 Ter. globata very common) . . . . o 10 



5. Limestones, yellowish-grey massive 



(three main beds), but in places, at the 

 top and bottom of the beds, rubbly. 

 The lower portion is less fossiliferous. 

 Clypeus Ploti, Klein, Holectypus de- 

 press us (Leske), etc. . . . . ..60 



6. Parting . . . . . . . . ..01 



Non-sequence. Beds IV. &• V. wanting. 



Limestone, shelly iron-speckled, coarsely 



oolitic, yellow and white - blotched ; 



oysters on the top, bored . . . , 04 



VI. Upper Trigonia- Ragstones, shelly, in two massive beds ; 



Grit crowded with Te^efcyfl/ff/a globata, a.\\ctt. 



andA'Av«c/jo»jW/aspp. and usual fossils 8 o 



Non-sequence Beds VII. to XIX. {incl.) 

 wanting. 



XX. Upper Freestone Limestones in two beds, very hard, con- 

 choidal fracture, top very even, water- 

 worn and oyster-strewn, bored , top- 

 most six inches of rock very shelly, 

 and Nerincea spp., corals frequent, 

 Astarte : Ttrebratula fimbria, Sow., 3 

 inches from the base . . . . ..30 



XXI. Oolite Marl Well-marked parting above band of yel- 



lower oolitic limestone' joined on to 

 the well-planed surface of Limestone o 4 

 that has, in the top-portions especially, 

 Nerincea, corals and lamellibranchs . . 14 

 XXII. Lower Freestone Limestones, well-oolitic, in massive beds : 



seen .. .. .. .. ..120 



The Bradfordensis-Beds here {i.e., Upper Freestone and 

 OoUte Marl), are again very fossihferous, and would doubtless 

 repay detailed working. 



I This adheres to the Upper Freestone at Scar Hill, where that deposit is 2 feet 10 inches thick, 

 and the Oolite Marl i foot 10 inches. 



