GEOLOGICAL 
OUT" LINE 
y MOZUFFERABAD 
OP THE 
Jtfaipjer 
Scale. 8 Miles = I, In ch 
Kalian 
map (lLec''i’E« VeL.lX^ along fh.e Meridian of 74 'EL 
(This T°i‘ ns "with Hie Jarrm 
epatta. 
fNa.wasb.ur *t 
DsTD EX 
ABBOTTABAD'}' 
Chile ai 
K\fbbuf 
rbela 
AtUxvixxrrv 
uinl 
Sup erficial 
Gundun 
'W'rL 
lntij h ni} 
But'ookote/ 
Kill abut 
. OU, gr-oive-L 
. Upper* . 
.(c*m.y ?o **W' cr.tsj’ ^ 
. Lower' ■ 
Kotiiaft 
iRusc&d ;ili 
Siwalik 
/Li'mlLr 
PESHAWUR 
Mtu-r'ea be.cLr 
'EERO OR 
D evwul 
Nummulitic 
Me. sozoic 
Tr'iajf. J VUTaurs lc Cf+t-cu>e,ovis 
Ccu'bonLfer'eisUS' 
Palasozoic 
// AKlivrubad 
/ / , /'O' / / / // 
//Me ©"toll. Sit// 
mWM/// 
ILLS 
Crystalline 
A nAlclirtAxJL 
SjT tmlAn^xl 
. F (xaaJU^s . 
oor 
Mutuhfu; 
NOTE- Th« Nummuilic limestone salt and gypsum 
west of die River Indus trrm probably* a. , 
lateral development cf the upper rvutvimulttie Gt'oup 
’ooro 
Hniki. Sir 
,tul Pa-’ 
ShaiW h 
lALidaN- 
mdokt 
Mun dalieyr S if 
irtota 
Ayyu WjpiND'i 
F uttel 
liungo 
Me er Kh.vra.yle e S ir 
To revurree 
Gopm^uf 
a m 
•vgoorlole Sir 
Kb a !. R 
Jharnl 
L achee 
S®53W»»>' 
vboga. 
sa&SSXS: x\- : 
futCOSsk 
;vxi 1 VV\.u 
B llHurvd. KhoyJ 
r.ftKK.“..?\,S-S. 
mass, 
^Tnftr ett. 
■L.-.f 
C^AOWOOK 
0 I'mcli Gliob 
Ki*HVrK»t 
CURH.fc E&H Kl 
tdon Fort 
Iv. of Hulun 
G-oTS liana 
Httfhcmlorv 
amgully* Sir 
WilRPOfVR 
L-ukki 
Mu oil a 
.bo rum 
i >V)uoillual 
BUNNOO 0 PatKi 
mnamee 
Ri ndo o KHeyl 
oxnelij 
ilaba&h’ 
Toiag'ujig 
•Shuriv nh 
J MELUM 
Do o rtieux' 
Chakowul 
^Dttod KYxeyl 
Mooveed 
j»ur nee Alum^frr 
Kummur 
Soolteui Kh oyi 
Syadpoor 
>V /” Kohtr 
MoncVi 
Kalar Kaliar 
TurecTCheyl 
Jourah 
Jala Li 
