Full text: Resource and environmental monitoring (A)

  
IAPRS & SIS, Vol.34, Part 7, *Resource and Environmental Monitoring", Hyderabad, India, 2002 
  
places clothed with tropical dry deciduous forest. The average 
yield of groundwater in this area is very poor i.e.< 50 lpm. 
4. SUMMARY AND CONCLUSION 
The study has revealed that satellite remote sensing technique is 
most beneficial advanced scientific tool for 
hydrogeomorphological studies and delineation of groundwater 
prospect zones through which challenging task of groundwater 
resources can be explored properly. Remote sensing inputs 
coupled with hydrological data are important components for 
the evaluation of suitable sites for groundwater development in 
the Purna River basin of Parbhani district. Geologically, the 
area is occupied by Deccan Basalts of late Cretaceous to early 
Eocene period. As the primary porosity is limited to gas 
cavities (vesicles), the groundwater in the area is therefore 
concentrated the zone of secondary porosity developed in the 
rocks due to fractures, joints and amount of weathering. 
Hydrogeomorphologically, the Purna River basin is divided 
into areas occupied by younger alluvial plain, older alluvial 
plain, valley fill, pediments, highly dissected plateau 
moderately dissected plateau and denudational hills. By 
studying the hydrogeomorphological conditions of the basin, it 
is possible to decipher the groundwater potentiality. It is 
moderate to good, in most part of the basin while the alluvial 
plains, the fractured zones in the dissected plateaus and the 
valley fills are very good potential zones. The weathered 
pediments with fractures and denudational hills are having 
moderate to poor groundwater potentiality. 
Dug wells are recommended in the alluvial units, valley fill 
deposits and weathered pediments. The highly dissected and 
moderately dissected plateaus are suitable for bore wells. Most 
of the dug wells in the pediments and in dissected plateau dry 
up during pre monsoon period hence bore wells and dug-cum 
bore wells are recommended for these areas. 
ACKNOWLEDGEMENT 
The author is grateful to Dr. R.D. Kaplay, School of Earth 
Sciences, Swami Ramanand Teerth Marathwada University, 
Nanded, Maharashtra, India for his keen interest and consistent 
guidance during the present work. 
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