Full text: Remote sensing for resources development and environmental management (Volume 2)

722 
4.2 Aj abg< 
L E G-E N D 
GE OMORPHOLOGICAL UNIT 
Alluvial Plain ( Old) 
Ciond Basin 
+>V 
4.v>; 
i-+p 
Sandy/Loess Plain 
(Disssc t«d) 
Sandy/Loet* Plain 
(Undissected) 
Infermontare Valley Pill 
(Unditreded) 
Intermontane Valley Fill 
(Dissected) 
•Pediment 
Buried Pediment 
Structural 6 
Denudational Hills 
lithQLogy/material 
Alluvium 
(Récent to Quaternary) 
DO 
Loe«s 
(Recent to Quaternary) 
DO 
DO 
DO 
Quartzite, Phylite & Slate 
(Precambrian) 
Alluvium & Loess 
(Recent to Quaternary) 
Quartzite, Phylite a Slate 
(Precambrian) 
SYMBOLS USED 
m 
river/stream 
PALEOCHANNEL 
WATER LOGGED 
■3 AREA 
pTTvTI SALT AFFECTED 
№J/V\ AREA 
I—¿"J SETTLEMENT 
Figure 1. Geohydromorphological map (Based on Aerial Photographs 8. Landsat Imagery). 
The Ajabgi 
carbonacic 
quartzite, 
quartzitic 
than Aiwa: 
porosity £ 
but seconc 
found due 
litates hi 
watertabli 
rocks yie^ 
10 cubic n 
4.3 Quatei 
Recent to 
and loess 
permeabili 
They form 
brackish v 
sits are c 
ranging fi 
The yield 
but genera 
of Yamuna 
than othei 
5 GROUNDWA 
GEOMORPH 
5.1 Struct 
Structural 
form a run 
water occu 
ractures a 
high relie 
zone and v 
been dug i 
characteri 
Firozpur J 
zite is no 
8 metres, 
zone of th 
is also no 
might be r 
cted in fr 
has been r 
5.2 Pedime 
Owing to h 
limited we 
runoff zon 
recharge s 
The good q 
unit. 
5.3 Buried 
This unit 
with nomin 
beneath. I 
found unde: 
thicknes s 
from place 
varies froi 
water rang' 
5.4 Interm' 
This unit i 
The unit i: 
it does no 
in present
	        
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