488 List of the Works of Sir B. I. MurcMson, Bart., F.R.S. 



Geologists. — Proc. Geol. Soc. iv. p. 174; Phil. Mag. ser. 3, xxiv. p. 72; Z. u. Br. 

 N. Jahi-b. 1844, p. 623. 



46. The " Permian System " as applied to Germany, with collateral observations 

 on similar Deposits in other countries ; showing that Rothe-todte-liegende, Kupfer- 

 schiefer, Zechstein, and the lower Limestone constitute the Upper Member of the 

 Palaeozoic Eocks. — Eep. Brit. Assoc. 1843, Sect. p. 52. 



47. On the important Additions recently made to the Fossil contents of the 

 Tertiary and Alluvial Basin of the Middle Ehine. — Eep. Brit. Assoc. 1843, Sect. p. 55. 



48. Anniversary Addresses to the Eoyal Geographical Society of London. — Journ. 

 Eoy. Geogr. Soc. xiv. ; xv., 1844. 



49. Observations on the Ural Mountains to accompany a new Map of the Southern 

 portion of that Chain. — Journ. Eoy. Geogr. Soc. xiii. p. 269. 



50. On the Palaeozoic Deposits of Scandinavia and the Baltic Provinces of Eussia, 

 and their relations to Azoic or more ancient Crystalline Eocks ; with an Account of 

 some great features of Dislocation and Metamorphism along their northern frontiers. 

 — Proc. Geol. Soc. iv. p. 601 ; Journ. Geol. Soc. i. p. 467; Eep. Brit. Assoc. 1844, 

 Sect. p. 53; Verhand. Kais. Min. Gesellsch. Petersb. 1844. 



51. Fragments of a Geologist. — Quart. Eev. Ixxiii. p. 324. 



52. On the Palaeozoic Deposits of the Basin of Christiania. — Forhand. Skand. 

 Naturf. Mote, Christiania, 1845. 



53. On the Superficial Detritus of Sweden, and on the Probable Causes which 

 have affected the Surface of the Eocks in the Central and Southern portions of that 

 Kingdom. — Journ. Geol. Soc, ii. p. 350. 



54. Outline of the Geology of the Neighbourhood of Cheltenham. 8vo. Chelten- 

 ham, 1834. — -Ed. 2., augmented by /. Buchnan and E. E. Strickland. 8vo. London, 

 1845. 



55. On the Silurian Eocks of Cornwall, with Opinions on the Gold of Australia. 

 — Trans. E. Geol. Soc, Cornwall ; Ann. and Mag. Nat. Hist. xix. p. 326. 



56. On the Silurian and associated Eocks in Dalecarlia, and on the succession from 

 Lower to Upper Silurian in Smoland, Oeland, and Gothland, and in Scania. — Journ. 

 Geol. Soc. iii. p. 1. 



57. Address to the British Association for the Advancement of Science (Southamp- 

 ton). — Eep. Brit. Assoc, 1846. 



58. — Additional Eemarks on the Deposit of (Eningen, in Switzerland. — Journ. 

 Geol. Soc. iii. p. 54. 



59. On the Meaning originally attached to the term " Cambrian System," and on 

 the evidences since obtained of its being geologically synonymous with the previously 

 established term "Lower Silurian." — Journ. Geol. Soc. iii. p. 165; Edin. N. Phil. 

 Journ. xliii. p. 147. 



60. Introduction to a Second Memoir of Capt. Vicary on the Geology of parts 

 of Sinde.- — Journ. Geol. Soc. iii. p. 331. 



61. On the Distribution of Gold Ore in the Crust and on the Surface of the Earth. 

 —Eep. Brit. Assoc. 1849, Sect. p. 60. 



62. On "the Silurian Eocks of Bohemia," with Remarks on the Devonian Eocks 

 of Moravia. — Edinb. New. Phil. Journ. xliv. p. 66. 



63. On the Geological Structure of the Alps, Apennines, and Carpathians, more 

 especially to prove a transition from Secondary to Tertiary Eocks, and the develop- 

 ment of Eocene Deposits in Southern Europe. — Journ. Geol. Soc v. p. 157. 



64. On the Distribution of the Superficial Detritus of the Alps, as compared with 

 that of Northern Europe. — Journ. Geol. Soc, vi. p. 65 ; Edinb. New. Phil. Journ., 

 xlviii. p. 256. 



65. On the Earlier Volcanic Eocks of the Papal States, and the adjacent parts of 

 Italy.— Journ. Geol. Soc. vi. p. 281. 



66. On the Vents of Hot Vapour in Tuscany, and their relation to Ancient Lines 

 of Fracture and Eruption. — Journ. Geol. Soc. vi. p. 361. 



67. Geologia della Alpi, degli Apennine e dei Carpazi. Traduzione dall' Inglese, 

 ed Appendice suUa Toscana dei Professori Faolo Savi e G. Meneghini. Firenze, 1 850. 



68. The Slaty Eocks of the Sichon, or Northern end of the Chain of the Forez in 

 Central France, shown to be of Carboniferous age. — Journ. Geol. Soc. vii. p. 13. 



69. On the Discovery of Palaeozoic Fossils in the crystalline Chain of the Forez 

 in France, and on Lines of Dislocation between the Lower and Upper Carboniferous 

 Deposits of France and Germany.— Eep. Brit. Assoc, 1850, Sect. p. 96. 



