ttUMMULITIC ELLIPSOID PROM MANZULLI TO BANDA. 117 



section, may be traced curving round the crushed and inverted fold 

 in this limestone and passing downwards so as to underlie it in the 

 way represented. 



The part of the Bahadur Khel valley near Totukhi lies high, 

 separating" the waters of the Teeree (Tin) valley 



Neighbourhood of To- r & J J 



tukhf tertiary sand- streams from those of the Kurshru Algud, and is 

 stones. 



rocky, the tertiary sandstones being set on edge 

 with a high dip to the south w^here not vertical. The rocks are as usual 

 gray sandstones and red clays of a higher place in the series than those 

 nearer the hills, and showing less of red or purple colour, besides which 

 the soft gray sandstones occasionally contain scattered pebbles of quart- 

 zite or conglomeratic strings. 



Exactly to the south of the village of Teeree (Tiri), and to the south"' 

 South of Teeree, in- by east, the sections are very instructive as to the 



structive sections. ^ relationg of the rockg# The Md curveg 



which these form may be seen from long distances on the northern 

 flanks of the range, and on closer inspection the conformity of the groups 

 at least down to the gypsum, which is generally more or less obscure, is 

 as clear as their arrangement is in other places complex. The section 

 seen is as shown in Fig. 24, the curves overarching a space of nearly a 

 mile in breadth : — 



■ 



Gypseous series. 3. Greenish clay. 4. Eed clay zone. 5. Nummulitic limestone. 6. Tertiary sandstone, &c. 

 8. Gray and purple sandstones. 



7. Reddish purple clays and sandstones with hone beds. 

 Clay bands numerous- 

 Feet. 

 6. Alveolina limestone .., ... ... ... 100 



4 <( 5. Shaly limestone ... ... ... ... 100 



4. Greenish and whitish marly clays chiefly ... ... 50 



3. Blood-red clays (thick here) ... ... ,..200? 



2. Green clays (a few feet). 



1, Gypsum and clays, very thick, unknown amount in continuation of the sand- 

 stone and gypseous series, 1 in Figure. 



By carrying this section southward over the hills, it would traverse 

 the continuation of the limestone and overlying sandstone of the 



( 221 ) 



