364 
HUGHES : INGLEBOROUGH. 
the outcrop. It makes no feature where it should cross Moughton 
Lane, or where it passes under the base of the Mountain Lime- 
stone east of Norber, from which we should infer that it probably 
thins out in this direction also, and is merely a lenticular bed 
of small extent. It is made up of rolled and angular fragments 
up to eight or ten inches in diameter, derived largely from 
the Green Slate Series, the fine felspatliic mudstones and finer 
and coarser grits, conglomerates, and breccias of that series 
being all represented in tlie conglomerate. There were also 
fragments of a rock very similar to some of the beds in the under- 
s. 
a. Striped sandy shale not much cleaved. 
h. Conglomerate not well seen in the line of this section. 
c. Cleaved shale with subordinate calcareous hand. 
d. Felspathic ash-like beds and yellow porcellanous rock with subordinate 
black bands, one very conspicuous. These are probably the beds 
seen under the bridge. 
e. Slate strongW cleaved 70° S.S.W. 
/. Felspathic, speckly, ash-like beds exposed at the gate for a horizontal 
distance of about 8 feet. 
(J. Very tough, granular, crystalline rock, with small sago-like grains of 
transparent quartz, about 10 inches seen. 
Ji. Limestone, with a knobbly, irregular surface, about 2 feet seen. 
The strike of e,f, g, h is clear, but not the dip; indeed, it may be that 
between this and the barn we have crossed the axis of the fold, and that 
we are already on the southern limb of the anticlinal. 
lying Bala. The matrix was very calcareous, often a coarse 
crystalline limestone, in which two species of coral Favosites 
alveolaris and Favosites (stenopora) fibrosa were not uncommon. 
In the included fragments Professor Harkness informed me that 
a trinucleus had been found, but I have been unable to verify 
this statement, or, indeed, to find any derived fossils. 
The first thing to be done is to make a collection of «very 
kind of fragment and every variety of matrix in this conglomerate, 
