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THE WEST OF ENGLAND AND EAST OF WALES. 455 
this declined, the phenomena of the various glacial periods would be 
produced. He thought boulder-clays and boulders had been re-sorted 
again and again by the sea. 
Mr. Dr Rance said that in the Lake-district the striz radiate 
from the watershed. Hence pebbles derived from the Solway, 
found in the midland Glacial deposits, could only have come by 
floating ice; and, further, with these there was evidence, in the 
Middle Sands, that currents flowed to the 8.8.E. The striz were 
older than the deposits on them. 
Mr. J. F. Camppett expressed his satisfaction at the numerous 
facts brought forward by Mr. Mackintosh, and instanced the Straits 
of Belleisle in almost the same latitude, where the existing state 
of facts explained very well phenomena described by Mr. Mackintosh. 
Mr. Mackrytosu replied that in the peninsula of Wirral the 
striz converged. In Anglesey the strive were parallel. For replies 
to some of the speakers he referred to his paper. 
