346 
RECORDS OF MEETINGS. 
July IStli. — The party went by train to Lowestoft and 
examined the chffs from Kessingland to Lowestoft and Gorton. 
The glacial deposits proved of great interest, and the identity 
of the contents of the Chalky Boulder- clay at Pakefield and in 
Mid-Norfolk was established. The interception of the beach 
material, travelling from the north, by the harbour works at 
Lowestoft had clearly a disastrous effect on the coast to the 
south of the town, which had been almost entirely denuded of 
the protecting gravel. 
July 14th. — The party visited sections on the Great Eastern 
Railway and studied the constituents of the Chalky Boulder-clay 
at Fornsett. Here the clay was composed largely of Kimeridge 
shale mingled with chalk. The shale was much less ground 
than at Lowestoft. The most noteworthy boulders were of 
chalk and flint, resembUng those of Lincolnshire and Yorkshire 
with some Spilsby Sandstone and Red Chalk. A few igneous 
rocks were found, including chiefly dolerites. In a great gravel 
pit at Wymondham two specimens of rhomb-porphyry were 
found. At Hethersett, near Cringleford, Chalky Boulder-clay 
was seen to be destitute of the Kimeridge Clay fragments which 
characterise it further south. 
The party were entertained to tea by Mr. and Mrs. Harmer, 
at Oakland House, and the host's fine collection of fossils was 
examined. Hearty thanks were accorded to Mr. and Mrs. 
Harmer for their kindness. 
Meeting of the Underground Waters Committee, Leeds, 
3rd September, 1903. 
Chairman : — Prof. P. F. Kendall. 
Present: — Messrs. W. Ackroyd, F. Swann, A. R. Dwerryhouse, 
S. W. Cuttriss, C. W. Fennell, J. H. Howarth, J. J. Wilkinson, 
G. Bingley, and Revs. E. Jones and W. L. Carter (Secretary). 
The minutes of the previous Committee Meeting were read 
and confirmed. 
Letters of regret for absence were read from Messrs. W. 
Morrison and W. Simpson. 
