114 
ft. ins. 
I 4-Soft pasty Oolitic Marly debris, small Rhynchonelle (scarce) Zee 
5—Sandy stone wes one “ng Oa 
6—Soft Marly parting oe x 0 6 
7—Sandy stone, (two bands) with “Marl ‘saat ae ae Neal 
8—Loose, soft, white, blue, or yellow Marl 2H AS, 
9—Sandy stone Onna 
10—Marly parting ... a 0 3 
11—Loose shattered sort of eccaienis, mmiige fede a the es 5. (0 
12—Band of hard stone... oa ae ae oes ee 0 4 
J 13—Blue clayey Marl aS nae ams aa “O fet 3 10 
14—Band hard stone 0 56 
15—Yellow clay 0 8 
16—Yellow clay, often fake ing like ‘Upper sae Ryneh 
subobsoleta bed. Tereb. fimbri (Whe oe 1 8 
17—Coral bed, according to Mr Witchell, with Lima Pontos 
Trigonice, Corals, &c. fi 3182 
18—Hard white rock, (variable) abana eink of a Pebatans sate 
of bedding. Rhynch. sp. Rh. Lycetti, scarce... 3 29 
19—Shaly pasty rock, 7. curvifions abundant. W. Leckey 
scarce. Rhynchonellee yak aoe 2m 
Same Cutting, South side. 
20—Hard stone, Tereb. submazillata abundant . Sis 2 O 
21—Whitish pasty rock, becoming clayey on exposure, very 
fossiliferous. Wald. Leckenbyi, Rh. Lycetti, Wald. 
Witchelli, Tereb. posgromenaie, Tereb. Lees ae 
Whitakeri ... 1 10 
22—Hardish Oolitic ee: pale pink tinge, esr flat on the top. 
Visible... 0.5 08 
This cutting is extremely interesting, not only on account 
of the rich fauna that it contains, but for many other matters. 
Just beyond the bridge a fault, which crosses the line obliquely, 
(N. W. to 8. E.) brings down the upper beds of the Inferior 
Oolite, viz., the Clypeus Grit, Trigonia Grit, and Notgrove 
Freestone level with the Oolite Marl. A few yards further on 
eastwards these beds are all bent downwards at about 45 
degrees, and another fault brings the Fullers Earth down to 
the same level. 
The Oolite Marl which is shown in this cutting attains a 
very great degree of development. The bottom bed, No. 22, 
may very probably be the top of the Lower Freestone, which 
can be observed on either side of the Station in the fields. 
