432 HIND : CARBONIFKROUS ROCKS OF THE PENNINE SYSTEM. 
The quarry at the dip mark, north of the word Bollards, 
shows the following sequence : — 
Crinoid limestone, 3 in. 
Black shale, 4 in. 
Finely stratified limestone, 9 in. 
Gypsum, 1 in. 
Black shale, 3 in. 
Platy limestone, 3 in. 
Crinoidal limestone, 2 in. 
Black shales, 2 ft. 3 in. with Prodiicfus longispinus. 
Crinoidal limestone, 5 in. 
Earthy limestone, 2 ft. 
Solid limestone, 15 ft. Base not seen. 
The following fossils were obtained : — 
Produdus mesolobus. 
„ plicatilis. 
„ punctafus. 
„ semireticulatus. 
Spirifera trigonalis. 
At Pythorns, a little more than a | mile further east, the con- 
glomerate bed of Brockthorns is again seen crammed with rolled 
fossil debris about 3 ft. thick. This is covered in by a few inches 
of shales, while below is fairly massive but well-bedded limestone, with 
bands of apparent brecciation. 
The following fossils were obtained : — 
Zaphrentis. 
Crinoids. 
Phillipsia sp. 
Produdus giganteus. 
,, pundatus. 
Spirifera lineata. 
„ glabra. 
Or this resupinata. 
Michelini. 
Spines of Palcechinus. 
Euomphalus Dionysii /• 
