) 



The groundwater hydrology of Region 6 is similar to Region 5. Bedrock 

 wells yield an average of 10 gpm from a water table which averages 10.6 

 feet below the ground level (Prescott 1974). The ice-contact deposits are 

 all favorable groundwater aquifers, delivering more than 50 gpm. They also 

 act as recharge areas for bedrock groundwater. There are few areas which 

 exhibit favorable bedrock yields, but there is too little data to confirm 

 the absence of bedrock aquifer zones (Caswell and Lanctot 1975). Since most 

 wells in this region are dug wells, there is a potential for well water salt 

 contamination by aerial pesticides which travel rapidly through gravel 

 deposits (Caswell 1978). 



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