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:j^ii 



CONTENTS. 



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ililrej 189,-— coaftofBerwlcklliire, § 190,— Cullenla 



§ 192, — Ardencaple in Dumb artonfli ire. 



BaniFshir 



Arran, &.c. 



193 



Pembrokefhire, § 194 



Jed. 



burgh, § i95,-~Ingleburgh in Yorkiliire, § 196, 

 Cumberland, § 197. Inflexion of the llrata, § 198. 

 Remarkable inflances in the Alps and Pyrenees, 



§ 199 



20c 



on Benlav/ers in Perthfliire, § 201, 



coaft of Berwicklliire, /3. — Plymouth, § 202. Stra- 

 ta fuffering fuch inflexions have been foft and duc- 



tile, § 



§ 

 § 



Genera] property of thefe inflexions, 



Uniform 



primary 



^ 



Inferences as to the nature of the elevating 



theories. Cry. 



§ 2.07 



mp 



Hallization, ib- Marks of undulae in the fchiftus 



9'- 



Elevation of the llrata a lironghold of the 



209. Elevation of the llrata 

 enables us to fee far into the interior of the earth, 

 § 210. 



Huttonian theory, § 



Note xiii. 



Metallic Veins. Page 239 



eclmens of native iron, § 211, 212. Margraaf 



§ 



§ 



Increafe 



of the 



fufi 



ume 



mens of gold 



§ 



filver fli 



215. Speci- 

 11 quartz, an 



argument in favour of the Huttonian theory, § 



218. 



Proof in favour of the fame from chalce- 



dony including 



f 



M 



m above or from either fide, § 



§ 



Suppofed fadl that 



f 



§ 



No 



mari£s of horizontal depofition in veins •, their coating 



differs 



