To face p. 408.] 



[Quart. Journ. Geol. Soc. Vol. LXIII, Nov. 1907. 



Table II. — Koad-Cutting, Midfokd, hear Bath. 



Fullers' Earth Bluisl 



( I. Rubbly Beds 



(6 inches.) 

 I II. Anabacia- 



LlMESTONES. 



(11 feet.) 



Thickness in feet inches 

 l-grey clay, with some masses of impure limestone; Terebratula globoid, auctt., 



h<nill,nthi/,-is niuljnnlnish, sp. nov., Urnithc/la <■<„/,, ,n > usis (E. Deslongchanips), 



Belemnites (BelerAnopsis) bessinus, d'Orb., Belemnites 2 spp., Ammonites (Zig- 

 lagtceras) procerus, Seebaeh, Ostrea acuminata, Sow., 0. Knorri, Voltz, Goniomya 



,n„l„l,jn;i (Sow.), Pie,,,;,,,,,/,, sp., //// ///-<•/,„/ v ■//„ N„„7///, Walk,.,-, ( ') IVsft, £„/,s- 



f/o/t( (Morris & Lycett), Sutira (east) 

 a. Limestone, rubbly, with crowds of Terebratula globata, auctt /./„„/ fidmaMaj 



gibbosa, Sow., (i.)Volsella ouneata (Sow.): to 8 indies 



a. Limestone, white, oolitic ; the top-bed brownish, shelly, bored by annelids and 



Lithophagi, and oyster-covered ; Serpula sp ' 



6. Limestone, regular bed, but only well seen in the centre of the section ": "Anabaeia 



,1,,,,,,/a 



III. DoULTING StONU . 



(11 feet 9 inches.) 



feet.) 



Illetl 



c. Limestone, oolitic, less massive than the underlying beds; WW, 

 (Defrauce) *..* .' 



a. Limestone, very massive, with frequent nests of Terebratula globata 

 of Trigonite very common in tho upper portion of the bed'; Anabaeic 



h. Limestone, less massive, with ' Terebratula globata' (rare), and cavities 

 have been. The top-bed is bored, and oysters arc attached to the up 



C. Limestones, massive, with imprints of Trigonim. Top-surface waterwo 



by Lithophagi; Anabaeia at the top ....' 



IV. Ul'l'ER Cokal-Bed a. Limestones, whitish, rubbly, mixed with greyish marl ; Isaslrcea spp. lye 

 Spiriferina (!) oolitica, Moore, Zellaum lhtrhls,,,,;, Moore, Z. „„! 

 Thecidella granulosa, Moore, Th. Forbesi, Moore, 77/. triangularis, d'Orb., Cranu 

 Saundersi, Moore, Crania sn., CristMurut >;>i itlata, Lam., Marginulina custata 



•e shells 



d bored 



" uit), 



M< 



VI. Ui'i-EH Trigoma- 

 Gjut. 

 (5 feet.) 



Batsoh., Spiitllma 

 Jones, Cytheteis B] 

 Lycett, (?)TiHrbo (i 

 Spirorbismidfordm 



(Non-sequence'.) 



a. Ragstones, brown, fn 



helvetica, I 

 . Cutheridia 



& Zwingli, Vatellina sp., Bairdia Hilda, 

 i sp., Emarginula sp., Trochotoma depressiuscula, 

 , Amberleya Eudlestoni, sp. nov. (text-fig. 6, p. 434), 



(text-fig. 7, p. 435), Neuropora sp., and sponges ... 



ishol, shelly ; the top-portion is sli 



,i\w in 



>pei 



itly bored, and there 



„(Sehlolh.). These 



s), Irigonia 

 duplicates, 

 .), Hhyncho* 



are a few oj 



ragstones are better bedded than those be 

 h. Ragstone, similar to Via, but more shelly; some 



bottom-part is pebbly. Ctenostreon pectiniforme 



costata (Sow.), Ostrea 2 spp., (?J Volsella cuneat 



Sow. (cast of), Belemnites (fragments), Acanthothi 



nella ha mpen'ensis, S. Buckman 



-(No n-sequeuce.) 

 a. Limestone, hard, grey, arenaceous, non-oolitic. Tlie top-portion is occasionally 



bored by Lifhojilini/i, and the deeper irregularities have received some of the 



pebbly material such as occurs at the base of the overlying deposit, to which it is 



generally joined on : to 8 inches 



h. Sands, yellow, micaceous. 



| dispansi-StrucJcmanni. . 



g.S Section exposed in Greenway Lane and Lyncombo cutting, near Bath (Somerset k 



Dorset Railway). (S. S. Buckman, Quart. Journ. Geol. Soc. vol. xlv, 1889, p. 448.) 

 3 o 



c. Yellow, micaceous sands, not well exposed : about 05 



Yellow sands, with about a dozen lines of 'sand-burrs.' From fallen 'sand-burrs,' 



Grammoceras fallaciosum [Pseudogrammooeras cf, Struekmanni\ was obtained ... 35 



(striatuli Yellowish-brown stone, with very numerous lighter-coloured oolitic grains, which fall 



out and leave the stone pitted, (irtniintocrnis strut tula m 



This is firmly cemented without a break on to 



bifrontis Yellowish stone, with the oolitic granules less numerous, and therefore appearing of a 



closer texture. Iiililuccrus hi/runs, Davtt/locvras Hu/amlrci ', D. crusstini, Wuhlheimut 



[ Cincta] Li/cvtti, Vhi/iichunella sp 



This is firmly cemented without a break on to 



•?' l/alci/cri a. Close-grained, smooth-feeling, greyish-blue stone, without any trace or grains as in 



the bed above. Harpoceras falcifcrum 



| h. Greyish-blue clay 



1^ c. Close-grained, greyish, mottled stone 



Ui'pbjr Liassic Clay d. Greyish-blue clay. 



