164 ADDITIONS TO THE LIBEAET. 



Desnoyers, J. Note supplementaire au memoire sur la craie et les 

 terrains tertiaires du Cotentin. 4to. Paris, 1826 ? Presented 

 by W. WhitaJcer, Esq., F.G.S. 



Deiualque, G. Un nouveau dosage du Fer des Eaux Minerales de 



Spa. 8vo. Liege, 1887. 



-. Quelques dosages du Fer des Eaux de Spa. 8vo. Liege, 



1888. 



Diller, J. S. Peridotite of Elliott County, Kentucky. 8vo. Wash- 

 ington, 1887. 



DrygalsTd, Einch von. Die Geoiddeformationen der Eiszeit. 8vo. 

 BerUn, 1887. 



Duncan, P. Martin. On a new Genus of Madreporaria {Glyphas- 

 trcea), with Eemarks on the Morphology of Glyphastrcea Forhesi, 

 Ed. & H., from the Tertiaries of Maryland, U.S. 8vo. London, 

 1887. 



DujQont, E. Origines et modes de formation des calcaires de la 

 Belgique. 8yo. Brussels, 1887. 



Encyclopaedia Britannica. 9th edition. Vol. xxiii. T-Ups. 4to. 

 Edinburgh, 1888. Purchased. 



Encyclopaedic Dictionary. Vol. vi. Part 2. Shipp-Tart. 4to. 

 London, 1887. Presented by the Bev. B. Hunter, LL.D., F.G.S. 



. Vol. vii. Part 1. Tas-Urb. 8vo. London, 1888. Presented 



by the Bev. B. Hunter, LL.D., t.G.S. 



Ernst, A. La Exposicion IN'acional de Venezuela en 1883. Obra 

 escrita de orden del illustre americano General Guzman Blanco. 

 Tomo 1. Texto. 4to. Caracas, 1886. 



Ettingshausen, C. von. Beitrage zur Kenntniss der fossilen Flora 

 Neuseelands. 4to. Vienna, 1887. 



Fairley, W. Wicked Fairies of the Mine. (Slip.) 



Favre, E., et H. Schardt. Eevue Geologique Suisse pour I'annee 

 1886. xvii. 8vo. Geneva, 1887. 



, . Revue Geologique Suisse pour I'annee 1887. xviii. 



8vo. Geneva, 1888. 



Fisher, 0. A Eeply to Objections raised by Mr. Charles Davison, 

 M.A., to the Argument on the Insufficiency of the Theory of the 

 Contraction of a Solid Earth to account for the Inequalities or 

 Elevations of the Surface. 8vo. London, 1887. 



. On the Mean Height of the Surface-Elevations, and other 



Quantitative Results of the Contraction of a Solid Globe through 

 Cooling ; regard being paid to the existence of a level of no 



