PROCEEDINGS OE THE GEOLOGICAL SOCIETY. 



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2. "On the Drifts of the Yale of Clwyd, and their relation to the 

 Caves and Cave-deposits." By Prof. T. M c Kenny Hughes, M.A., 

 F.G.S. 



The following specimens were exhibited : — 



Implements and specimens from Drift- deposits, exhibited by 

 Prof. T. M c Kenny Hughes, M.A., F.G.S., in illustration of his 

 paper. 



Specimens of Metamorphic Rocks from the Malvern Hills, exhi- 

 bited by Prank Rutley, Esq., F.G.S. 



Specimens illustrating Metamorphism in Lizard Gabbros, exhi- 

 bited by J. J. H. Teal, Esq., M.A., P.G.S. 



December 1, 1886. 



Prof. J. W. Jttdd, F.R.S., President, in the Chair. 



Henry Howe Arnold-Bemrose, Esq., M.A., Lonsdale Place, Derby ; 

 Richard Assheton, Esq., B.A., Downham Hall, Clitheroe ; Francis 

 Arthur Bather, Esq., B.A., Redhouse, Roehampton, S.W. ; Rev. 

 Joseph Campbell, M.A., Parsonage, Glen Inncs, New England, 

 N. S. Wales ; John Wesley Carr, Esq., B.A., University College, 

 Nottingham ; Thomas J. G. Fleming, Esq., Limavady, co. Derry, 

 Ireland ; Thomas Forster, Esq., Umaria Colliery, Umaria, India ; 

 Edmund Johnstone Garwood, Esq., B.A., Villa Giuseppina, Caden- 

 abbia, Lago di Como, Italy ; George Samuel Griffiths, Esq., 22 Collins 

 Street West, Melbourne ; Dr. Frederick Henry Hatch, Ph.D., Aubry 

 Lodge, Wellesley Road, Gunnersbury, W. ; Robert Tuthill Litton, 

 Esq., Market Street, Melbourne ; Frederick William Martin, Esq., 

 37 Charlotte Road, Edgbaston, Birmingham ; Richard D. Oldham, 

 Esq., A.R.S.M., Geological Survey of India, Calcutta ; Forbes 

 Rickard, Esq., F.C.S., Ashcombe, Carlton Road, Putney, S.W. ; 

 Albert Charles Seward, Esq., B.A., St. John's College, Cambridge ; 

 Herbert William Yinter, Esq., M.A., Wesleyan College, Truro, 

 Cornwall ; and Charles D. Walcott, Esq., U.S. Geological Survey, 

 Washington, D.C., U.S. America, were elected Fellows of the 

 Society. 



The List of Donations to the Library was read. 



The President announced that he had received from Prof. Ulrich, 

 of Dunedin, N.Z., the announcement of a very interesting discovery 

 which he had recently made. In the interior of the South Island 

 of New Zealand there exists a range of mountains, composed of 

 olivine-enstatite rocks, in places converted into serpentine. The 

 sand of the rivers flowing from these rocks contains metallic particles 

 which, on analysis, prove to be an alloy of nickel and iron in the 



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