194 Mr. Verchére on the Geology of Kashmir, [No. 38, 
2. Pale limestone, weathering glaring white ; filled with geodes, lined with 
small spar-crystals. No fossils. Dips 8. 80°, ... S00 ».. LOO ft. 
3. Thin-bedded, shaly, striped limestone, ... Preaie i2) Lhe 
Fault. It rons E.—W. and is about 10 feet wide at the ibe It is filled with 
rocks similar to No. 3, folded in all directions. 
4, Limestone like 3; vertical, a0 pot ae wo eloptbe 
5. Pale limestone; with geodes, like 2. Traces of fossils were observed, 
but much altered and not recognizable, es 200 ee LOOM iE: 
6. Pale blue, shaly limestone; dips N. 80°, ... 200 (ate aeietbs 
7. like 5; dips N. 80°, ... Pe 66d a0 eee OON tbe 
Fault; it rons H.—W. 
Sapp S alae) a8 7, ees 00 See eee eeay Oaths 
9. Argillaceous, thin-bedded, pale grey estou breaking in flat thin pieces, 
like pottery, A 000 600 ae) OU MEL. 
10. Sandy Teens: thewel oa dik 400 ven ecee Opstitre 
- 11. Conglomerate limestone, varying from a coarse sandy Hmestone to 
a perfect conglomerate, the pebbles being rounded, pieces of limestone im- 
bedded in a soft calcareous paste. It contains many sections of the Aviculo- 
pectens and other large bivalves peculiar to the Weean bed. Portions of the 
bed are white and altered, ... eee m0 odo eee LOO ft. 
12. Sandy, micaceous, limestone; dark grey, ee opens 
13. White limestone; no fossils, ... ee a Ps Omtbe 
14. Argillaceous limestone, blue and pale; weathering lustreless 
and velvety, 03 cae 300 300 pa soe) | eObehte 
15. Conglomeratic limestone lke 11, 500 vee .. 650 ft. 
16, Brecciated and sandy limestone; sometimes a coarse calcareous sand~ 
stone, 306 vee ooo 300 doc 50 soo) ttt, 
17. Ash-blue, pale, muddy limestone; weathering lustreless, ... 25 ft. 
18. Brecciated and sandy limestone, Rid Bet cece Latte 
19, Ash-blue, pale and muddy ; weathering lustreless,............ 25 ft. 
All these beds dip 8. with an angle diminishing gradually from 80° to 35° 
20, This bed is the top of a well defined anticlinal. The rock is a yellowish- 
grey limestone, with rolled pieces of limestone imbedded. It is sandy, some- 
times quite a sandstone, oftener a sandy impure limestone. It contains a great 
many remains of fossils. The southern branch of the unticlinal dips 8. 35°; 
the northern branch dips N. N. W. 25°. There is therefore a squeezing of the 
strata at the western end of the strike, and a divergence or opening of the 
fault at the eastern end, Thickness about 30 feet, 
Then we get a repetition of the beds seen before, as follows: 
21. Ash-blue, lustreless muddy limestone, ... a Bey i itt 
22. Brecciated and sandy limestone, ine Ay a lt 
93. Ash-blue limestone, .,. sae oe aes wa 2 aethe 
24, Brecciated limestone,,.,, nes 990 na cee, Out 
