Sequence between Doulting and Cheylinch. 



(Quarry — disused — on the west side of the 

 Doulting-Cheylinch Eoad.) 



Thickness in feet inches. 



Fullers' Earth Clay, pale-grey and yellow ; ' Terebratula 



globata,' Acanthothyris midfordensis, sp. 

 nov., ? Alectryonia (fragment), Ostrea 

 Knorri, Voltz, Serpula volubilis, Mini- 

 ster, 8. plicatilis, Minister, Goniomya 

 angulifera (Sow.), Belemnites (Belem- 



nopsis) bessinus, d'Orb. 2 6 



II. Anabacia- Limestone, white, oolitic ; seen 1 



Limestones. 



Doulting Quarry. 



(Quarry — in work— on the east side of the 

 Doulting-Cheylinch Road.) 



Subsoil, clayey at the top 1 5 



II. Anabacia- Limestone, white, oolitic, sparry, some- 



Limestones. what rubbly in the upper portion, 



(About 5 or 6 feet.) but flaggy and more regularly- bedded 

 below. Fossils abundant in a zone 

 1 foot thick, commencing at 20 inches 

 above the Doulting Stone ; Tere- 

 bratula (probably ' T. globata ') , Pecten 

 (Syncyclonema) demissus, Phillips, 

 Trigonia costata (Sow.), Ostrea, Litho- 

 phagus inclusus, Anabacia complanata, 

 Strophodus magnns, Agassiz. Called 



by the quarrymen ' Ridding' 5 



III. Doulting Stone, a. ' Hard.' Suitable for rough masonry, 

 (44 feet.) but generally burned. Freestone, 

 coarse, pale-yellow and greyish, rarely 

 oolitic, with much calcite crystallizing 

 out in the cavities ; Pteria digitata (Des- 

 longchamps), Limea duplicata (Sow.), 

 Homomya cf. crasskcscula, Morris & 

 Lycett, Strophodus magnns, Agassiz, 

 Serpula cf. Umax. Top-bed bored by 

 Lithophagi ; it has oysters adhering, 

 waterworn; 3^ to 4 feet 3 6 



b. Doulting Freestone. Freestone, 

 pale-brown and grey, highly calci- 

 ferous, often without partings ; 14 to 

 16 feet 16 



c\ Limestone, yellowish-grey, compact, 

 splintery, obscurely oolitic, with dark- 

 yellow staining along the cracks. The 

 top-portion is bored, oyster- strewn, 

 and contains pebbles of a greenish 

 rock. By the quarrymen this stone is 

 called the ' Ragstone,' and therefrom 

 Mr. S. S. Buck man records ' Bhyn- 

 chonella subtetrahedra ' and ' Trigonia 

 costata''; seen 1 



\c". Limestone, not exposed, but in rail- 

 way-cutting 6 6 



d. Limestone, not exposed, but in rail- 

 way-cutting 16 



,^ U w ^..^.^-..(Non-sequence: Upper Coral-Bed. 



and Dundry Freestone absent.) 



VI. Upper Trigonia- The ' Conglomerate-Bed ' 1 4 



Grit. 



