SEC. 3.] WAGUR, E. KUTCH. 1^1 



at Futtyghudj consisting of coarse felspathic white and variously 

 banded sandstone and grit with some mud beds^ 



North-west side of tract. 



and a parting of greenish yellow marl. The hill 

 is traversed by intrusions and dykes of gray trap^ and much of the 

 country in the neighbourhood is occupied by sandy plains, where the 

 rocks are seen rising above these to the east and north. They consist 

 of coarse, open, gravelly sandstone, some of the beds hardened by 

 infiltration of iron, assuming a black color on exposure. They are cut up 



by trap dykes, and by the very frequently observed 



Ramps. 



silicious veins resembling the ' gangiie' or ' Jwrse' 

 of a lode, sometimes termed by the Cornish miners ' ramps' 



About Doosulpoor, and to the east and west, nearly the same 

 varieties of hard fine grained calcareous and some- 



Doosulpoor. , „ ,1 - TTi 1 ii 1 



what flaggy beds as occur in Bela nave norttieriy 

 inclinations towards the Runn. 



Between Rev, or Row, and Rahpoor, is an outlying patch of the 

 sub-nummulitie beds appearing from beneath the 

 alluvium to the north, the Jurassic rocks of the 

 adjacent country being red ferruginous and light colored sandstones inter- 

 stratified with gray shales ; these undulate over the country, and the 

 sandstones contain a few Ammonites and other fossils. 



From Rahpoor to Oomia, and around the former town, ferruginous 



sandstones and earthy shales, strong yellow sand- 



Rabpoor to Oomia. ^^^^^^ ^^^ ^^^ ^^^ light-colored flags and hffima- 



titic beds, undulate or dip north at 5° to 7°, and are crossed by a long 

 dyke of purple lava-trap. Hence to Adeysur, the rocks have more the 

 aspect of those belonging to the upper Jurassic group and are much 

 intersected by dykes and ' ramps,' particularly in the vicinity of the 

 latter town. Hereabouts the beds slope generally towards the alluvium, 

 which is bordered by an intervening band of the lateritic and white 

 sub-nummulitic rocks. 



( 121 ) 



