464 



PROCEEDINGS OF THE GEOLOGICAL SOCIETY. 



179. 



180. 

 181. 

 182. 

 183. 



184. 

 185. 

 186. 

 187. 

 188. 

 189. 



190. 

 191. 

 192. 

 193. 

 194. 

 195. 

 196. 

 197. 

 198. 

 199. 

 200. 

 201. 



202. 

 203. 

 204. 

 205. 

 206. 

 207. 

 208. 

 209. 



210. 

 211. 

 212. 

 213. 

 214. 

 215. 

 216. 

 217. 

 218. 

 219. 

 220. 



ft. in. 



Brought forward . . . 235 3 



Stone 5 



Clay 6 



Stone 4 



Clay 1 10 



Stone 7 



Clay 3 9 



Stone 4^ 



Clay 4 



Stone 6 



Clay 11 



Stone, Ammonites jpla- 



norbis 6 



Clay 2 



Stone 6 



Clay 2 



Stone 9 



Blue clay 3 4 



Stone 7i 



Blue clay 2 4 



Stone 5 



Clay 3 



Stone 4^ 



Blue clay 1 4 



Stone, Ammonites fla- 



norbis.EindLGryphcBa in- 



curva more abundant ... 4 



Clay 9 



Stone 6 



Clay 2 



Stone 8 



Clay 1 



Stone 8 



Ditto 6 



Blue clay, Ammonites 



angulatus 4 



Stone 8 



Clay 1 10 



Stone 4 



Clay 1 9 



Stone 7 



Bluemarl 2 



Stone 3 



Marl 1 



Stone 6 



Marl 1 



Stone 5 



Carried forward 277 2^ 



ft. in. 

 Brought forward 277 2\ 



221. Marl 1 



222. Stone 2^ 



223. Marl 1 



224. Stone 4 



225. Marl 2^ 



226. Stone 5 



227. Marl 9 



228. Stone U 



229. Marl 8 



230. Stone 6 



231. Marl 1 



232. Stone 6 



233. Marl 1 



234. Stone 3 



235. Bluemarl 11 



236. Stone 6i 



237. Marl 7 



238. Stone 9 



239. Bluemarl 7 6 



240. Stone 6 



241. Marl 3 



242. Stone 3 



243. Marl 2 9 



244. Stone 10 



245. Marl 2 6 



246. Stone 6 



247. Bluemarl 20 



248. Stone 5 



249. Marl 7^ 



250. Stone 5^ 



251. Marl 7i 



252. Stone 9 



253. Thick beds, blue marl, 



about 30 



254. Stone 6 



255. Marl 2 



256. Stone 4 



257. Marl 1 



258. Stone 6 



259. Marl 2 



260. Stone 3 



375 4 



Beds still continuing, but 

 dipping under line of 

 railway, thickness un- 

 known. 



In this important section we have a clear passage upwards, with- 

 out any break, from the upper beds of the Keuper, though the Ehae- 

 tic and White Lias series into the Lower Lias. The " White Lias " 

 is here almost identical in thickness with the section (given in my 

 former paper) at Steven's Hill, Long Sutton, about four miles distant ; 

 hut whilst the limestone beds are thicker, there has been a corre- 

 sponding decrease in the intervening beds of marl. There are large 



