part 11 PKOCEEDINGS OF THE GEOLOQICAL SOCIETY. Ixxxix 



boundaries of the sheets in areas not affected hv larger disturbances 

 of deep-seated origin. 



The results obtained by the joint magnetic and geological work- 

 in the two areas show that this method of investigation may be 

 used to extend our knowledge of the underground structure. It 

 appears also that an extension of the method to other parts of 

 the country would yield information of considerable scientific and 

 economic importance. 



A short discussion followed, and the thanks of the Fellows 

 present were accorded to Dr. Cox for his Lecture. 



Geological maps were exhibited by Dr. A. Hubert Cox, M.Sc, 

 F.G.S., in illustration of his Lecture. 



A model of a ' Sop ' of iron -ore worked at the Park Mines, 

 Dalton-in-Furness, was exhibited by the Director of the Geological 

 ! urvey, to whom it was presented by the Barrow Haematite Steel 

 Company. Mr. Bernard Smith, F.Gr.S., described the model, and 

 discussed the origin of the ore-body. The model was prepared by 

 Messrs. David & Herbert Lawn. 



May loth, 1918. 



Mr. G. W. Lamplugh, F.K.S., President. 

 in the Chair. 



Albert Stanley Harding, B.Sc, Brighton Villas, Abertillerv 

 (Monmouthshire), was elected a Fellow of the Society. 



The List of Donations to the Library was read. 



A Lecture on ' The Geology of the Italian Front ' was delivered 

 by Prof. Edmund Johnston Gaewood, M.A., Sc.D., F.R.S. 

 It was illustrated by lantern-slides, geological maps and sections, 

 and tables of strata. 



The President expressed to the Lecturer the thanks of the 

 Fellows present. 



A'OL. LXXIT. 



