WATER DIVINING GREGORY 



339 



other 17y2 feet. The essential point of this test, however, was that 

 water was found where the dowser said there was none.* 



FT 



5)jrirj^ 



Antclifi. 



• Bacon. X Beyer. O Child. 



+ Taylor. T Tompkins. 



S Sutton. 



PiGDKE 12. — The Guildford test, April, 1913. Lines connecting some bores were rep- 

 resented as streams 



* Professor SoUas tells me that in regard to the site which the dowser predicted would 

 be dry " there was never any question of more or lesis water ; it was water or no water." 

 In both wells the water stood at the same level. In reference to the unequal depth of the 

 two wells Professor SoUas tells me that while pumping out one in order to measure the 

 rate of flow the sides caved in and it was abandoned. 



