Vol. 68.] ANNIVERSARY MEETING — LTELL FUND. xlvij 



your chief interest in the Cambridgeshire boulders was aroused by 

 the numerous rock-types which are thus to be found scattered 

 over a country not otherwise rich in problems of the more solid 

 geology, were it not for your contribution on the Cambridge 

 district to * Geology in the Field.' You have not neglected other 

 sides of the Science, for your paper on the Dogger of Blea Wyke 

 and that on the Ingletonian Series are important contributions to 

 our detailed knowledge of the position and character of these strata. 

 Your latest paper has dealt with your observations in South Africa, 

 and involves, not only an important elucidation of the tectonics of 

 the area, but, if its conclusions are accepted by South African 

 geologists, a new reading of the relations of the strata there. It 

 is my pleasant duty to hand to you the Balance of the Proceeds of 

 the Lyell Eund. 



