Vol. 58.]  PROCERDINGS OF THE GEOLOGICAL SOCIETY. Vv 
The following specimens were exhibited, in addition to those 
mentioned on pp. lll—iv :— 
Specimens and Lantern-slides of Malvern Fossils, exhibited by 
Prof. Theodore Groom, M.A., D.Sc., F.G.8., and C. A. Matley, Esq., 
eoc., 1 G.S., 10 illustration ‘of the former’s paper and the latter’s 
appendix. 
December 18th, 1901. 
J. J. H. Teatz, Esq., M.A., V.P.R.S., President, in the Chair. 
John T. Bebbington, Esq., 28 Coningsby Road, Anfield, Liverpool ; 
Henry T. Leighton, Esq., 37 Arch Street, Rugeley (Staffordshire) ; 
Alexander Gordon Milne Thomson, Esq., Maybank, Maryfield, 
Dundee; and Thomas Leonard Walker, M.A., Ph.D., Professor of 
Mineralogy & Petrology in the University of Toronto (Canada), 
were elected Fellows; and Dr. Alexander Petrovich Karpinsky, of 
St. Petersburg, and Prof. Alfred Lacroix, of Paris, were elected 
Foreign Members of the Society. 
The List of Donations to the Library was read. 
Prof. H. G. Srerey drew attention to a Skull of Equus fossilis from 
Keswick, exhibited by Mr. J. Postneruwaire, F.G.8., and said that 
it belonged to a species of horse, but the skull appeared to be 
broader and flatter in front of the orbits than in Hquus caballus ; 
and it gave evidence on the upper surface of being an aged specimen, 
an inference which was supported by the palatal conditions. The 
teeth are worn down, so as to approximate to the condition of aged 
teeth of Hqguus fossilis, as sometimes found in river-valley gravels; 
but he was not aware that these teeth had previously been met 
with in association with this form of skull. He understood that 
the specimen had been found near the surface beneath an ancient 
building at Keswick, and that there was no evidence as to its 
geological antiquity. 
Mr. PosrLetuwatrTe said that the skull which the previous vapeaker 
had described was found beneath the floor of one of the rooms of a 
farmhouse known as‘ Birketfield,’ the property of Mr. J. M. Moorsom, 
about 6 miles east of Keswick. The house, which is of considerable 
age, was being altered and repaired, and it was in taking up one of 
the floors, for the purpose of relaying, that the skull was found. 
The surface-deposit on the farm is Glacial Drift. 
Prof. W. W. Warts called attention to the exhibited set of Twenty- 
two Photographs, the first of three sets to be published as typical 
examples of Geological Photographs by the British Association 
Committee on Geological Photographs. 
VoL. LVIII. b 
