Ft. In. 
106 Mr. Cumberland on the Strata near Bristol. 
No. 
are the beds whose basset edges are covered by the mag- 
nesian limestone in horizontal strata, before noticed ; 
some small fragments of which may be observed from 
the spot overlapping the highest bed in view in a thin 
lamina. Fragments also may be found below, that have 
fallen in parts. 
From the boundary stone ( N. 9. C.B.) to another 
(BDC. 1810,) 30 paces further on, we may reckon a 
few broken off beds, underpinning and supporting those 
above mentioned, as belonging to this series ; after which 
we commence again where we left off, at the greatest 
quarry that is now working actively ; these beds are 
150. Bed of red limestone . . . 
151. Two others 
that are covered by rubble, stones, and grass, forming a 
little mound. Then other small beds, under another 
swelling mound, covered with rubble and turf. 
152. The first one a compact red - 
153. Second ^ - 
154*. Third | 
155. Fourth 
156. Fifth 
157. Sixth 
158. Seventh 
15 
15 
I 
3 
3 
3 
6 
6 
6 
Here begins the Great Quarry at boundary stone 
(B.D.C. 1810.J which ends with the same marked 
boundary stone, measuring between them 480 paces from 
working to working, and we shall consider it as the 
Fifth Series. This Great Quarry, now working, 
159. Commences with a bulky head of grey limestone, containing 
very rarely the large anomia, but no other shells or encri- 
nital remains. The further end has some beds of coral- 
loids, that are very abundant and very much expanded. 
This bulky head dips at the usual angle, and is the lower- 
