Authors
Abstract
Electrical resistivity, observations well and lithological data are used for the
groundwater investigation in the piedmont zone Ratmau –Pathri Rao watershed in
Haridawre Districted of Uttaranchal India, The analysis of the resistivity data in the
light of known lithology indicates that two aquifer (shallow and deep) are generally
present in the area
The resistivity of aquifers are generally varies in wide range. This is due to the
presence of different size of ranges of grains condition consisting of fine sand and
gravel (pebble) in the Tarai zone which further grade to coarser material (Boulder in
the Bhabhar zone)
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