RECORDS OF MEETINGS. 
345 
examined. At the base was a purplish boulder-clay, sandy in 
texture, and enclosing many shell fragments and small boulders. 
This was overlaid by beds of fine silt, bent into folds, and filling 
hollows in the till. Over this came an upper till rich in chalk 
fragments. 
July lOtli. — A wagonette was taken to Weybourne, where 
the shelly sand known as the Weybourne Crag was examined. 
The contorted Cromer Drift was well seen in fine sections, and 
the Forest Bed Series was exposed at the base of the cliff and 
on tlie shore at several points. 
llie General Meetiwj was held at the Tucker's Royal Hotel, 
Cromer, under the chairmanship of Mr. Godfrey Bingley. 
The following new members were elected : — 
Mr. Robert B. Beverley, Wakefield. 
Mr. Richard Balderstone Cragg, Skipton. 
Mr. William Ackroyd, Leeds. 
Mr. Peter Whalley, Colne. 
The Secretary exhibited a chart of the Coal Measures of 
North Staffordshire, with their characteristic fossils, prepared 
by Dr. Wheelton Hind, and presented by him. 
The Society not having any room wliere it could be usefully 
displaj^ed, it was resolved to offer the chart to Prof. Kendall to 
be Imng in the Lecture Room at the Yorkshire College. Prof. 
Kendall suitably acknowledged the gift. 
A paper was read by Mr. F. W. Harmer, F.G.S., on " The 
Pleistocene Deposits of East Anglia." 
A discussion followed, in which Messrs. P. F. Kendall, 
W. L. Carter, C. W. FennelL and Rev. C. T. Pratt took part. 
The meeting closed with hearty votes of thanks to the Chair- 
man and to the leader of the Excursions and reader of the paper. 
Mr. Bingley and Mr. Harmer responded, 
July 11th. — The train was taken to Xorwdch, and the head- 
quarters was fixed at the Royal Hotel. 
The deposits in the neighbourhood of Norwich were examined, 
including the Chalk, XorT\ach Crag, and glacial beds. Many 
important erratics were found which had not been previously 
recognised so far south, e.g., rhomb-porphyry, Shap granite, 
and rocks from the Cheviots and the Lowlands of Scotland. 
