FAR 389 



Farcy (Ch.). 



1. Aperpu philosophique des Connaissances huraaines au 19^siecle. 

 Paris, 1827, 18°.— Fericss. Bull. XVI. p. 208. 



Farcy (Fr. Ch.). 

 1. Recherches historiques sur I'Aigle. 4°. Paris, 1826. 



Farey (J.). 



1. On the Stratification of England— Phil. Mag. XXV. p. 44. 



2. On the Dislocations of the Strata of the Earth. — Phil. Mag. 

 XXVIir. p. 120. 



3. On the Stratitication of Matlock in Derbyshire. — Phil. Mag. 

 XXXI. p. 36. 



4. Observations on a late paper by Dr. TV. Richardson respecting 

 the Basaltic district in the North of Ireland, and on the geolo- 

 gical facts thence deducible.— Phil. Mag. XXXIII. pp. 257, 385. 



5. Geological Observations on the Excavation of Valleys, and local 

 Denudations of the Strata of the Earth in particular districts, 

 etc.— Phil. Mag. XXXIII. p. 442 ; XXXIV. p. 49. 



6. Geological Remarks and Queries on MM. Cuvier and Bron- 

 gniart's Memoir on the Mineral Geography of the environs of 

 Paris.— Phil. Mag. XXXV. p. 113. 



7. On the supposed Freshwater origin of the Gypsum Strata in the 

 environs of Paris ; on the Geological Characters and Relations 

 of the Alum Shales on the Northern Coasts of Yorkshire ; and 

 on the Orbicular Blocks of Sienite on Mount Sorrel Hill, in Lei- 

 cestershire.— Phil. Mag. XXXV. p. 256. 



8. A List of about 700 Hills and Eminences in and near to Derby- 

 shire, with the Stratum which occupies the top of each, and 

 other particulars.— Phil. Mag. XXXVIL p. 161. 



9. Geological Observations on Unstratified Mountains, and on the 

 Use and Abuse of Geological Theories. — Phil. Mag. XXXVII. 

 p. 440._ 



10. On the great Derbvshire Denudation. — Phil. Trans. CI. p. 242. 

 —Phil. Mag. XXXIX. p. 26. 



11. Geological Remarks and Queries on Dr. CamphelVs Map and 

 Account of the Stratification of Lancashire. — Phil. Mag. 

 XXXVIIL p. 336. 



12. Geological Observations on the county of Antrim, and others 

 in the North-east part of Ireland.— Phil. Mag. XXXIX. pp. 266, 

 353. 



