98 PAPERS, ETC. 
In another quarry of much the same character on 
the road leading to Bicknoller, south of St. Audries, the 
anticlinal of these beds has been discovered within a few 
days by Mr. J. D. Pring, of Taunton, and we are now 
enabled to complete a section of the whole range, the 
publication of which, in the present volume, has been 
superintended by that gentleman, to whom I anı also in- 
debted for other valuable information. 
The sandstones in this quarry are of a reddish grey 
colour, and very hard. The two dips may be clearly 
observed, viz., the northern at an angle of 20 deg. north- 
west, and the southern at about 10 deg. south-east. North 
of Doddington, the sandstones are of a purer gray colour, 
having a mixture of red only at certain points. Mr. Pring 
notes the discovery of the cast of a Terebratula in the 
hard grey sandstone of this part, and having on the same 
specimen traces of the fine lined corals of the Fenestella 
family, and Encrinital catss. Save this one solitary speci- 
men, the whole of this part has proved to be non-fossilifer- 
ous, and further evidence is certainly required before we 
can pronounce it to be otherwise. By Doddington we en- 
ter on the middle part. The beds now vary from those 
we have been examining by being more flag-like with dove 
and greenish coloured slates between. On the north-east 
of Crowceombe, near Fire Beacon, we find, in a quarry, 
beds composed of greenish and purple tinged sandstones, 
much cleaved, and the dip imperfect and southerly. It has 
a talcose appearance, and bears no trace of fossil remains. 
Clay slate lies between these beds, and which looks very 
much like soapstone, though it is not in the least steatitic, 
but contains a large proportion of silica and alumina, and 
a small trace of magnesia. Passing on to the northern 
escarpment of Will’s-neck hill, is a hard, light, greenish 
