434 HIND : CARBONIFEROUS ROCKS OF THE PENNINE SYSTEM. 
The Cold Coniston limestone mapped as isolated beds, regarded 
in connection with the beds exposed in the hill 200 yards west, are 
evidently more extensive. 
This limestone occurs in a series of domes or knolls, one of which 
is bisected by the Skipton-Settle road at Fogga. 
The upper part of this limestone is massive, not well bedded, 
whitish in colour, but the lower beds are more regularly stratified. 
A fairly extensive fauna, typical of the Carboniferous Limestone, 
occurs here. 
Two hundred yards west is another quarry on the south side 
of the road in the side of a large well-rounded rolling hill. The beds 
are well marked, and dip at 30° N.N.E., and thus would, if pro- 
duced, pass below the limestones of Fogga. 
About 30 ft. of beds are exposed. . 
The following fossils were obtained :— 
Productus semireticulatus. 
Spirifera glabra, 
Rhynchonella pleurodon. 
Large Corals. 
Cyatkophyllum Stutchhuryii 
Zaphrentis cylindrica. 
Three-quarters of a mile further west, and a little north, another 
exposure is found in a wood at Old Rock plantation, on the 1 inch 
maps 
Here several feet of well-bedded limestones covered by black 
shales are seen dipping N.W. at 15°. 
On the rolling ground south of the road are the following sections. 
A little more than J mile S.S.W., at the word quarry on the 1 inch 
map is the following section: — 
Hard blue limestone. 1 ft. 
Hard nodular shale with crinoids, Zaphrentis, and frag- 
ments of shells. 12 ft. 
Well-bedded limestone. 
Half a mile south-east, between the woods Camp and Hall Field, 
are two exposures in the same beds, showing massive well-bedded 
grey limestone overlaid by calcareous shales* 
