262 COSMOS. 



made by Sir James Hall more than half a century ago, anJ 

 by the attentive study of granitic veins, which has contributed 

 go largely to the establishment of modern geognosy. Some- 

 times the erupted rock has not transformed the compact into 

 granular limestone to any great depth from the point of con- 

 tact. Thus, for instance, we meet with a slight transforma- 

 tion a penumbra as at Belfast, in Ireland, where the ba- 

 saltic veins traverse the chalk, and, as in the compact cal- 

 careous beds, which have been partially inflected by the con- 

 tact of syenitic granite, at the Bridge of Boscampo and the 

 Cascade of Conzocoli, in the Tyrol (rendered celebrated by 

 the mention made of it by Count Mazari Peucati).* Another 

 mode of transformation occurs where all the strata of the com- 

 pact limestone have been changed into granular limestone by 

 the action of granite, and syenitic or dioritic porphyry.! 



I would here wish to make special mention of Parian and 

 Carrara marbles, which have acquired such celebrity from the 

 noble works of art into which they have been converted, and 

 which have too long been considered in our geognostic collec 

 tions as the main types of primitive limestone. The action 

 of granite has been manifested sometimes by immediate con- 

 tact, as in the Pyrenees,$ and sometimes, as in the main land 

 of Greece, and in the insular groups in the ./Egean Sea, through 

 the intermediate layers of gneiss or mica slate. Both cases 

 presuppose a simultaneous but heterogeneous process of trans 



* Humboldt, Leltre a M. Brocliant de Villiers, in the Annales de 

 Chimie et de Physique, t. xxiii., p. 261 ; Leop. von Bucli, Geog. Bricfe 

 uber das siidliche Tyrol, s. 101, 105, und 273. 



t On the transformation of compact into granular limestone by the 

 action of granite, in the Pyrenees at the Montagues de Rancie, pee 

 Dufrenoy, in the Mimoires G6ologiques, t. ii., p. 440 ; and on similai 

 changes in the Montagnes de COisans, see Elie de Beaumont, in the 

 Mem. Geolog., t. ii.. p. 379-415; on a similar effect produced by ihe 

 action of dioritic and pyroxenic porphyry (the ophite described by Elie 

 de Beaumont, in the Gcologie de la France, t. i., p. 72), between Tolosa 

 and St. Sebastian, see Dufrenoy, in theAfcm. Geolog., t. ii., p. 130 ; and 

 by syenite in the Isle of Skye, where the fossils in the altered limestone 

 may still be distinguished, see Von Dechen, in his Geognotie, p. 573. 

 In the transformation of chalk by contact with basalt, the transposition 

 of the most minute particles in the processes of crystallization and 

 granulation is the more remarkable, because the excellent microscopic 

 investigations of Ehrenberg have shown that the particles of chalk pre. 

 viously existed in the form of closed rings. See Poggend., Annalcn dci 

 Phytik, bd. xxxix., s. 105; and on the rings of aragonite deposited 

 from solution, see Gustav Rose in vol. xlii., p. 354, of the same journal. 



t Beds of granular limestone in the granite at Port d'Oo and in thu 

 Mont de Labourrl. See Charpentier, Constitution Geolngiqnc des Pyr6 

 ners, p. 14-J, 116 



