DAU 179 



19. On the Quantity and Quality of the Gases emitted from the 

 Bath Waters — Phil. Trans. CXXIV. p. 1. 



20. On the Volcanic Strata exposed by a Section made on the site 

 of the new Thermal Spring discovered near the Town of Torre 

 deir Annunziata, in the Bay of Naples ; with some Remarks on the 

 Gases evolved by this and other Springs connected with the Vol- 



canos of Campania. — Proc. Geol. Soc. II. 177 Phil. Mag. ser. 



3, VII. p. 316.— Edinb. New. Phil. Journ. XIX. p. 221. 



21. On a Saline Spring near Oxford. — Trans. Geol. Soc. II. ser. 2, 

 V. 263.— Proc. Geol. Soc. II. p. 204.. 



22. Reply to Prof. Bischofs Objections to the Chemical Theory 



of Volcanos Edinb. New Phil. Journ. XXVI. p. 291 ; XXVII. 



p. 158. 



23. Report on the State of our Knowledge with respect to Mineral 

 and Thermal Waters. — Rep. Brit. Assoc. 1836, p. 1. 



24. On the Geology and Thermal Springs of North America. — 

 Rep. Brit. Assoc. 1838, Sect. p. 91. 



25. On the Quantity of Salt in Sea-water, as determined by the 

 examination of specimens collected on a voyage from Southamp- 

 ton to New York Ed. New Phil. Journ. XXXV. p. 65. 



26. On the Site of the Ancient City of the Aurunci, and on the 

 Volcanic Phsenomena which it exhibits ; with some Remarks on 

 Craters of Elevation, on the Distinctions between Plutonic and 

 Volcanic Rocks, and on the Theories of Volcanic Action which 

 are at present most in repute. — Trans. Ashmol. Soc. II. 1846. — 

 Edinb. New Phil. Journ. XLI. p. 213. 



Dadbeny (C. G. B.) and Widdrington (Capt.). 



1. On the Occurrence of Phosphorite in Estremadura. — Journ. 

 Geol. Soc. I. p. 52. — Journ. Agric. Soc. Engl. V. p. 406. 



Daubree (A.). 



1. Note sur ]e PhSnomene erratique du Nord de I'Europe, et sur 

 les Mouvemens r6cens du Sol Scandinave. — Compt. Rend. XVI. 

 p. 328.— Z. u. Br. 1844, p. 113. 



Daubuisson ; vide Aubuisson. 



Dauderstadius (C. Chr.). 



I. Dissertatio de Phcenice. Lips. 1665, 4°. — Bohm. Bibl. II. 2, 

 p. 533. 



n2 



