HtSCELLAKEOXTS. d26 



Swiss lake-dwellings, and French and Swiss cave-deposits ; and sum- 

 marizes the history of West Yorkshire from the preglacial age to the 

 historic period. W. H. D. 



Judd) Prof. J. W. Palaeontology and the Doctrine of Descent. 

 Nature, vol. xv. pp. 275, 276. 



Refers to labours of Dr. Neumayr, of Vienna, in the lacustrine series, 

 2000 feet thick, forming the highest part of the Tertiaries of E. Europe, 

 probably Pliocene. C. E. D. 



Kane, Sir Robert. Anniversary Presidential Address. Joum, E. 



Geol. Soc. Ireland, ser. 2, vol. iv. pt. 3, pp. 104-111. 

 Gives a resume of the paper read before the Society in 1875. 



Xianbe, — . Standpunkt und Aufgaben der Geologie und Palaeonto- 

 logie in der Gegenwart. [Present State of Geology and Palaeonto- 

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Xaranx, Eugene. Nouveau systeme du monde, ou les premieres 

 forces de la Nature. [New World System, or the Primary Forces 

 of Nature.] Ed. 3. Paris, 



Leymerie, — . Note sur les Cartes agronomiques comparees aux 

 Cartes geologiques. [Agricultural and Geological Maps compared.] 

 Pp. 7. Toulouse. [1876 ?] 



Long, Wm. Stonehenge and its Barrows. Wiltsh. Arch. Nat. Hist. 



Mag. vol. xvi. no. 46, pp. 1-244. 

 The geological nature of the stones is discussed, pp. 59, 68-77. 



Lyell, Sir Charles. Principles of Geology, or the Modem Changes of 

 the Earth and its Inhabitants considered as illustrative of Geology. 

 Ed. 12. 2 vols. 8vo. London. 



Macturk, Jolrn. Physical Geography adapted to the requirements 

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 8vo. London and Glasgow. 



Chap, vi., Structure of the Earth (pp. 112-131), gives a general 

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Magitot, — . Sur I'homme tertiaire, etc. [Tertiary Man.] Bull. 



Soc. Anihrop. Paris, ser. 2, t. xi. p. 523. 

 Note of observations and experiments on the marks on fossil bone« 

 {Balcenotus) attributed to the hand of man. (See Capellini, p. 52.) 



Malet, H. P. The Sea-level. Geogr. Mag. dec. ii. vol. iii. pp. 216- 



218,247-250. 

 Combats the received explanation of strata being exposed above the 

 «ea-level, and maintains that the sea must have sunk. 



