C PROCEEDINGS OF THE GEOLOGICAL SOCIETY. [Aug. I903, 



April 8th, 1903. 



J. J. Harris Teall, Esq., M.A., F.R.S., Vice-President, 

 in the Chair. 



Wynne Edwin Baxter, Esq., J.P., D.L., 170 Church Street, Stoke 

 Newington, N., and The Granvilles, Stroud (Gloucestershire) ; and 

 W. E. Garnett Botfield, Esq., J.P., The Hut, Bishop's Castle 

 (Shropshire), were elected Eellows of the Society. 



The List of Donations to the Library was read. 



Prof. W. W. Watts drew attention to the exhibit on the table of 

 the new series of Platinotype Photographs about to be issued by the 

 Geological Photographs Committee of the British Association. 



The following communications were read : — 



1. ' On the Probable Source of some of the Pebbles of the 

 Triassic Pebble-Beds of South Devon and of the Midland Counties.' 

 By Octavius Albert Shrubsole, Esq., F.G.S. 



2. ' Note on the Occurrence of Keisley-Limestone Pebbles in the 

 Bed Sandstone-Bocks of Peel (Isle of Man).' By E. Leonard Gill, 

 Esq., B.Sc. (Communicated by Prof. W. Boyd Dawkins, D.Sc, 

 E.R.S., E.S.A., E.G.S.) 



In addition to the photographs mentioned above, the following 

 specimens were exhibited : — 



Bock-Specimens (Pebbles) and Microscope-Slides, exhibited by 

 0. A. Shrubsole, Esq., F.G.S., in illustration of his paper. 



April 29th, 1903. 



J. J. Harris Teall, Esq., M.A., E.B.S., Vice-President, 

 in the Chair. 



Norman Melville Kirkcaldy, Esq., C.E., Dunedin (New Zealand) ; 

 and Bernard Stracey, Esq., M.B., Sutton Bonnington, near Lough- 

 borough, were elected Fellows ; and Prof. Carl Klein, of Berlin, 

 was elected a Foreign Correspondent of the Society. 



The List of Donations to the Library was read. 



Prof. Bonney, in exhibiting three specimens found by Prof. Collie, 

 F.R.S., on Desolation- Valley Glacier, east of the watershed of the 

 Bocky Mountains and a little south of the Canadian Pacific Railway, 

 pointed out that one, a slab of white quartzite, was covered by 

 horizontal worm-burrows, often about one-third of an inch in 



