Vol. 58.| PROCEEDINGS OF THE GEOLOGICAL SOCIETY. Ixxxi 
April 16th, 1902. 
Prof. Caartes LapwortH, LL.D., F.R.S., President, in the Chair. 
James Grundy, Esq., Inspector of Mines for the Government of 
India, 27 Chowringhee Road, Calcutta; and Frank Parkin, Esq., 
The Limes, 5 Sherwood Rise, Nottingham, were elected Fellows 
of the Society. 
The List of Donations to the Library was read. 
The following communications were read :— 
1. ‘The Carlisle Earthquakes of July 9th & 11th, 1901. By 
Charles Davison, Sc.D., F.G.S. 
2, ‘The Inverness Earthquake of September 18th, 1901, and its 
Accessory Shocks.” By Charles Davison, Sc.D., F.GS. 
3. ‘The Wood’s Point Dyke, Victoria (Australia).’ By Frederic 
Philip Mennell, Esq., F.G.S. 
A Photograph of a Ruined House was exhibited, in illustration 
of Dr. C. Davison’s paper on the results of the 1901 earthquake at 
Inverness. 
April 30th, 1902. 
Prof. Cuartes Lapwortu, LL.D., F.R.S., President, in the Chair. 
John Dampier Green, Esq., Johannesburg (Transvaal) ; Everard 
Heneage, Esq., Marlborough Club, London; Edwin Sloper, Esq., 
26 Wolseley Road, Crouch End, N.; and George Frederick Herbert 
Smith, Hsq., British Museum (Natural History), Cromwell Road, 
S.W., were elected Fellows ; and Prof. Thomas Chrowder Chamber- 
lin, of Chicago ; Dr. Thorvaldr Thoroddsen, of Reykjavik (Iceland) ; 
and Prof. Samuel Wendell Williston, of the University of Kansas, 
Lawrence (Kan.), were elected Foreign Correspondents of the 
Society. 
The List of Donations to the Library was read. 
Mr. J. KE. Marr exhibited some specimens from a Metamorphosed 
Metalliferous Vein several inches wide, which he had discovered in 
the basic andesites near the Shap Granite, in a quarry close to the 
high road, north of the spot where it crosses Longfell Gill. 
The minerals of the vein include quartz, calcite, garnet, epidote, 
hornblende, galena, iron-pyrites, and copper-pyrites. Some of the 
garnets are about an inch in diameter. he epidote and the horn- 
blende tend to form distinct bands on the margin of the vein. The 
other metamorphic phenomena recall those describod by the exhibitor 
and Mr. Alfred Harker, in the case of large vesicles occurring in the 
same rocks. 
