HIND : CARBONIFEROUS ROCKS OF THE PENNINE SYSTEM. 433 
Two miles still further east is the quarry at Teenly Rock, which 
shows fine well-bedded limestone, the beds being nearly horizontal. 
Towards the base of the quarry is a bed of oolitic hmestone. Fossils 
are not plentiful here, but a tj^ical Carboniferous Limestone fauna 
occurs : — 
Produdus giganteus. 
„ semireticulatus. 
„ plicatUis. 
„ yunctatus. 
Spirifera glabra. 
„ lineata. 
Athyris planosulcata. 
Orthotetes crenistria. 
Orthis resupinata. 
Conocardium aliforme. 
Crinoidal fragments. 
Between Teen ley and Py thorns thin limestone and shales are 
seen in the stream at Becks Brow Bottom, and a sulphuretted 
hydrogen spring, indicating a roll and temporary disappearance of 
the limestone from the surface. 
East of the Ribble is a patch of country bounded on the north 
and east by the Hellifield and Skipton line. Numerous dip marks 
and quarries are shown, nearly all of which show the upper beds 
of the massif of limestone. The country has a rolling domed contour 
which we have found to be characteristic of limestone rather than 
shale areas, and is moreover covered by stone walls, and is treeless 
and waterless. Massive bedded limestone is seen in a quarry just 
beyond Bell Busk station, and another quarry rather less than J 
mile west of Bell Busk viaduct. This shows 18 ft. or more of thick 
massively bedded limestone with no shales, and yielded the following 
fossils : — 
Chonetes papilionacea. 
Spirifera lineata. 
Sijringopora geniculata. 
Cyathophyllum Stutchhuryi. 
Crinoids. 
L 
