INDEX. 



307 



Commencement of speckled sandstone 

 Composition of salt marl 



■= of magnesian sandstone 



■ of potash salt . 



Conditions of production of salt 

 Conglomerate bands in siluiian 



near Mari 



zone, Siwalik . 



Conglomerates 



Connexion of Salt Eange with outer 



Himalaya 

 Copper shales 



Cost of carriage of salt in 1837 

 Country each side of Bakrala ridge . 



above Makrach 



—^ west of Khewi'a 



' on each side of range 



east of Kund ghat . 



Cretaceous formation 



■ passage beds to west 



western beds, fossils 



■ distribution, where seen . 



at Chichali Pass, 



Crushing and dislocation, eastern 



Page, 



90 



71 



88 



80 



82 



87 

 266 

 125 



27 



2 

 91 



6 

 122 

 214 

 219 



42 

 214 

 103 

 103 

 104 

 104 

 276 



145 



plateau 



Crystalline boulder beds, 87, 104, 117, 258 

 Crj'stals, pseudomorphic, after salt . 98 



Dandot cliffs 



plateau 



• coal 



. 164 

 . 41 

 . 166 



D'Archiac and Haime on Salt 



Eange fossils . . .15 



Davidson, Mr., ditto . .15, 20, 21 



de Koniuck Salt Eange fossils . 22 



Devonian, so-called . . .12 



Diagram of Salt Eange series . 69 



Difference of carboniferous sections . 94 



Page. 



Difference of Salt Eange nummuli- 

 tic from that of other nummulitic 

 areas .... 107 



Disappearance of range at Indus . 40 

 Diljaba Mountain . . . 123 



Discovery of carboniferous ammon- 

 ites . . . .05 

 Disintegration south of range . 59 

 Disparity between Salt Eange and 



Himalayan series . . .64 



Distance of volcanic sources from 



area of salt marl . . .83 



Distribution of cretaceous . . 104 



of salt mai'l . • 72 



Disturbance . ' -52, 102, 192 



north of Jalalpur . 131 



Dolomite in gypsum . • 74 

 i in salt marl • 133, 231, 277 

 Doubtfully two zones of haematite . 210 

 Drainage, Sardi glen . • 193 

 of Salt Eange . 43, 45 



E 



Early acquaintance with importance 

 of Salt Eange 



conditions of accumulation of 



salt marl . 

 Eastern part of range 



plateau 



termination of Mount Tilla 



■ cretaceous . 



■ limestone of Kahiin plateau 



Economic resources 

 Effect of rain (foot-note) 

 Elevation of Korana hills 

 — '■ of Salt Eange 



Elphinstone's Caubul 

 Eocene 



Epitome of Eastern Salt Eange 

 geology at Mount Tilla . 



i 307 



280 



52 



40 



124 



103 



170 



283 



143 



14 



32, 56, 57 

 4 

 69, 105 



130 



