. Memoirs of the Geological Survey of India . sandstones and clays may have once reposed above the highest beds ofthe range. The disturbance, though great, seems not to have been limited to the ordinary anticlinal and synclinal curves, but dislocation also, as one result Disparity of opposite of tension, apparently took place. In the centre sides of contortion. of fae main fold 0f the ridge where the rocks might be supposed to have had least room for alteration or motion, a certain dis-parity of the bed of the gypseous series and those close above the latteron each side of the axis may be obse
. Memoirs of the Geological Survey of India . sandstones and clays may have once reposed above the highest beds ofthe range. The disturbance, though great, seems not to have been limited to the ordinary anticlinal and synclinal curves, but dislocation also, as one result Disparity of opposite of tension, apparently took place. In the centre sides of contortion. of fae main fold 0f the ridge where the rocks might be supposed to have had least room for alteration or motion, a certain dis-parity of the bed of the gypseous series and those close above the latteron each side of the axis may be observed (similar in a general way tothat noticed regarding the sections north of Ismail Khel), so that bothsides of the anticlinal within the hard nummulitic limestone are not closecounterparts of each other. It may be supposed that the curve of thebeds now incomplete was sufficiently extended to have admitted of somelateral changes during deposition, sandstones and clays predominating at( 208 ) Wynne. 7V*#w -IrvcLu* Salt Fl*ci. IV Fault FatxJU. •7^. 16 Cvirvs in TST-mrumulitic Limestone n«Ra£ot*in£i Sir.
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