Minutes of Proceedings. xxxiii 



The American Anthropologist, Vol. X., Parts 1, 2, 3. Washington, 



1897. 

 Proceedings American Philos. Soc, Vol. XXXV., No. 152. 



Philadelphia, 1896. 

 Bulletin Minnesota Academy of Natural Sciences, Vol. IV., No. 1, 



Part 1, 1896. 

 Bulletin de la Societe Imperiale des Naturalistes de Moscou, 1896, 



No. 3. Moscow, 1897. 

 Das Meteoreisen von Forsyth Co., Georgia, von Prof. Dr. E. 



Cohen. Sitzungsber. d. k. p. Akad. d. Wiss., 1897. 

 Uber ein neues Meteoreisen von Locust Grove, Henry Co., Nord 



Carolina, von Prof. Dr. E. Cohen. Ibid. 

 The Proceedings and Transactions of the Nova Scotian Institute 



of Science, Vol. IX., Part 2. Halifax, 1896. 

 Bulletin de la Societe des Sciences Naturelles de L'Ouest de la 



France, Vol. VI., Parts 1, 2, 3, 1896. 

 Annales de la Faculte des Sciences de Marseille, Vol. IV., Part 



4, 1895, and Vol. V., Parts 3, 4, no date. . 

 Bulletin of the Johns Hopkins Hospital, Vol. VIII., No. 72. 



Baltimore, 1897. 

 Two numbers of the Illustrated Christian World. (Dr. Holub's 



contribution.) 

 Boletin Mensual del Observatorio Meteorologico Central de 



Mexico, 1897. 

 Eeport of Her Majesty's Astronomer at the Cape of Good Hope 



for the year 1896. London, 1897. 

 Proceedings of the Scottish Microscopical Society, Vol. II., No. 1, 



1896. 

 The Scottish Geographical Magazine, Vol. XIII., No. 4. Edin- 

 burgh, 1897. 

 Bulletin de l'Academie Imperiale des Sciences de St. Petersburg, 



Vol. VI., No. 2, 1897. 



Mr. A. W. Eogers, Assistant Geologist to the Geological Com- 

 mission, read a paper on " Geological Surveying in South 

 Africa," of which the following is an abstract : 



A geological map shows as far as possible the nature of the rock 

 to be found at the surface, and also at moderate depths below the 

 surface, at any point in the country. Owing to the recurrence of the 

 requisite conditions, particular varieties of sedimentary and igneous 

 rocks have been formed, or brought to the relative positions in which 

 we now find them, at different times during the past history of the 

 earth ; therefore the colours representing rock masses on our maps 

 have in most cases reference to the age of the rock represented. 



