158 MR. L. RICHARDSON OX THE [vol. lxxiv, 



6. Ten- Acres-Field Quarry, near South Ferrott. 



Thickness in feet inches. 



JSchlcenbachi... Microzoa-Beds. 6. Limestone: seen 2 



7. Marl and rubble 2 



Massive Beds. 8. Limestone, rather sparry ; 



Ctenostreon sp. 2 



? Truellei ? Truellei Bed. 9. Limestone; Belemnopsis 



bessina (A. d'Orbigny), Rli y nchonella aff. 

 parvula Deslongchamps, Rh. subtetra.lt edra 

 auctt., isocrinoid-ossicles, etc 1 2 



to the base of which is attached 



•Garantianx... Limestone, similar to its equivalent («) at the 



Misterton Lime- Works 4 



„~^~~ — — Non-sequence. Deposits of niortensis-con- 



cavi hemeraB (inclusive) wanting. 



Bradfordensis. Limestone, hard, bluish-grey and yellowish- 

 brown, well ironshot, with an ironstained 

 surface (to which oysters are attached) ; 

 Rhynchonella sp. 1 ; usually 4 



joined on to the surface of the bed below 



Murcliisonx Limestone; Nautilus sp., Pseudomelania hetero- 



cycla (Deslongchamps), Coslastarte sp., Ento- 



-Ancolioceras. Hum demissum (Phillips), Gryphxa cijgnoides 

 Whidborne, Lima inoceramoides Whidborne, 

 Pholadomya fidicula J. de C. Sowerby, Varia- 

 mussium pumilum (Lamarck). Rhytic-honella 

 aff. weigandi Haas & Petri, Pseudoglosso- 

 thyris simplex (J. Buckman), Terebratnla sp., 

 Zeilleria anglica (Oppel) (rare near the top), 

 Galeropygus agaric if ortnis (Wright), Berenicea 

 sp. (usually on the Limse) etc. 2 8 



■Scissi Sand-rock, with a very irregular surface. 



Well-Spring-Farm Quarry, Misterton (Somerset). — 

 In the field at (7) is an old quarry on the line of fault shown on the 

 Geological Survey map (Old Series, Sheet XVIII). In the quarry 

 ■are seen Top Limestones of the usual type, let down against grey 

 sandy Scissum Beds on the south side of the fault. 



The Top Limestones are seen in an old quarry at (8). 



Quarry near Misterton Church. — In the old quarry (9) 

 .■south of Misterton Church the Top Limestones are seen resting 

 on rock of (farantiance hemera (similar to its equivalent at the 

 Misterton Lime works), and this in turn on the ironstained sur- 

 face of the March isoiMn-AncoUoeeras Beds, to which is attached, 

 here and there, ironshot rock also similar to the corresponding 

 deposit at the Limeworks. No doubt this is the quarry where 

 -J. F. Walker found evidence in the form of ' a variety of JVald- 

 lirimia meriana [probably Aulacothyris cucullata S. Buckman], 

 associated with T. decipiens, 2 of the Scroff (Jwscce hemera). 



1 Mr. S. S. Buckman, to whom I submitted this specimen for examination, 

 informs me that he has • this peculiar broad triangular form, but larger and 

 with one plait, from the [Rhynchonella-] ringens Beds of Sherborne ("Dorset].' 



2 Proc. Dorset Nat. Hist. & Ant. F. C. vol. iii (1879) p. !»!. 



