188 WYNNE : TRANS-INDUS SALT REGION, KOHAT DISTRICT. 



formed of debris, but it is instead a portion of the solid roek of the 

 escarpment smoothly worn, and even at its junction with the vertical 

 cliff simulating the arrangement of detrital materials, as seen in the 

 figure (Fig. 55), of the upper tertiary sandstone cliff near Hussunshood 

 (Hassanshiid) . 



The rocks are here so frequently seen, that any large stratum of 

 conglomerate would probably show itself, so that the numbers of smooth, 

 rounded, hard boulders and pebbles about may either be supposed to 

 have come from one of the thick conglomerate zones of the northern 

 side of the Sheen (Shin) Ghur range (as shown in Colonel J. T. Walker's 

 section map No. 3, Northern Trans-Indus Frontier Survey) continued 

 to the Lukkur Ghur, or to have remained the most indestructible parts 

 of former conglomerates which had once existed over this ground. 



( 292 ) 



