101 



T. Wiggins & Son's boring, made in 1887 



2 ft i; Soil 



1 ft. : Yellow clay 



Sand and gravel 



Water rises to within 7 ft of 

 the surface in the tube 



35 ft 



2 ft 



68 ft. 



2 ft. 

 110 ft. 



but not so much 

 gravel as at old bore-hole 



Greatest supply of water here 



Bookleaf loam 



Lower boulder clay, some parts contain- 

 ing more stones than others. All 

 the stones water- worn. 



Small quantity of water about middle of 

 clay bed 



Bed marl, very dry. No sign of water 

 here 



Left off boring. 



The Auction Mart Co's. boring at the New Inn, made in 1899: 



Light spring at 8 ft. (apparent- 

 ly much contaminated 



31 ft 



56 ft. 



Light spring 1 ft. 



64 ft. 



Light spring 



110 ft 



A powerful* spring 140 ft. 



Blue sandy loam 



Blue Cluy, mixed with small stones 



Sandy bed 

 Blue clay 



Gravel bed f AnalysisJ 



Hard blue clay, mixed with small stones 



Red marl stone, or red shale 



[Analysis] 



*This spring rises in tbe pipe to 3 ft. above surface level, and 

 has continued running from a tap night and day since November 

 16, 1899, on which date it was found. 



Analyst's Report on Water obtained at a depth of 61 feet : — 



Borough Hall, Stockton-on-Tees, 



July 31 si! 1899. 

 I hereby certify that the following are the results of an analy- 

 sis of the sample of water received on the 26th instant, from Mr. 

 G. W. Weatherill, High Street, Stokesley :— 



Gi ains per Gallon 



Description of sample 



Drawn .. ... 



Appearance in 2 ft tube 



Smell when heated to 100 degrees F. 

 Chlorine in Chlorides 



Phosphoric acid in phosphates 



Nitrogen in Nitrates and Nitrites 



Ammonia ... 



Albuminoid Ammonia 



Total solid matter dried at 212 degrees P 

 Microscopical examination of deposit 



from spring (64 ft), 

 on the 26th instant 

 Pale straw and milky 

 Earthy 



Trace 

 Slight trace 



10-80 



Mineral matter, etc. 



•04760 

 •00700 

 233-24 



