elxxxvi Journal of the Asiatic Society of Bengal. [NS., XIV, 
— European mountain ranges, but —— = 7 been a 
ertainty in India, are diffic eee to ac as the direct result of 
Geapental thrusts on account of the ecient fonliles docu st crushing 
and corrugation which the dis iced rocks have been subjected to. 
The frequ 
stratum has oe the notion that their elevation was originally due 
entirely to an upward plateav-le bulging of the surface, and that the 
horizontal Piste soniont is due to a sliding down the slupe of the upraised 
ea, as the direct effect of gravitation, in a manner comparable to the 
movement of a landslip or of a glacie 
Tin ores in Ome J. Cogetn Brown. 
The 
wolfram at vt high price seooailins or ANE mineral have led to its 
itati fi r 
. — won by dredging in one valley ; other promising areas are ref 
and the association of the ore is briefly discussed. 
On the distinct sedimentary origin of some quartzites of 
Mysore.—By V. S. Sampastva IyER 
cara describes the occurrence, near gees ra egg 
of high] she 
nya A ao the markings on typical specimens of ripple-mar q 2 
eir Diecatecs are very similar to ‘t ose of Ti 
nes arked _Guartite of Baroda _or to those of typical quartzites © eo 
sediments preserving their t 1 ‘ tures do occur 5 
ypical textures bd struc 
Mysore, though the e exposure noted at present i mall one. The paper 
Ae illustrated by specimens, photos, fnescapn die sek map. ca 
Note on some Dinosaurian remains recently discovered | ee 
the Lameta beds at Jubbulpore.—By C. A. Ma ie 
The author recently discovered a number of Mapes bones, some ~ : 
of very large size, in beds of the Lameta formation at Jubbulpore. 
oss pe hill ee 
tonite were found at two horizons on the western slop af : 
as Bara Simla, on the estate of the Gun Carr rriage Factory. piece 
Presented to the Geological Survey of India oa are n0 
studied iby Mr. G. de P. Cotter and the author : 
argest remains occurred as ssatsoned bones in @ a rod onl 
4 
one amphicoel ous), a right humerus 54 inches long, an incom anothet 
(2) 48 inches in n length, leas (?) 28 inches aie & portion . gigantic 
radius, some ribs and a n umber of “Mewes ents. They belong to ® prove 
herbivorous dinosaur, probably 50 feet or more in length, and are ‘bed 
rag a assigned to Titanosaurus indicus genus and s er te fem 
f y Lydekker on the evidence of two veedancas and an incomple 
ound in this ne eee asuy about half a century ago. disco corer 
A Portion of the skeleton of another and smaller reptile be hese 
" mbedded 1 — 
t 50 yards tion 
sandstone at the base of the lower limestone men : ressures | 
and re 
study © 
matrix from the more delicate bones before 
