STATE GEOLOGIST. 



That of the Indian Mill p >., in the immediate vicini 



p I carried to a tfepth of 4:> t f< el At 



214 feet, brine was foil id at 19°, in &he gypseous group, ami at 

 195 feet, n i ar the bottom of this group, at l7 . N 

 n ■ gained in boring the next L39 Heet 



Windsor's well is located three or Four mil I . 

 north. It his been carried to the depth of 466 feet The 

 >- rth of the briD — > have increased somewhat 



sandstone* beneath tin roup. At 391 



i i. the M . the Balometi 1 ( The 



Strength nf the overt) >w was 84°, at the 

 Ions per minute. 



Mr. Taylor's well '1 very near Scril nl I have 



\ ed no data relating to it. 



The manufacture ibner's, Wind- 



the Indian Creek wetls. S r erected a 



! . or rather two of diem, 19 feet apart Each bouse is 100 



fto - feet high, and 7 feet Wide. The brine ia first 



I vat holding 32.000 gallons, from which it is 



pumped by water power to the top of the brush bouse From 



I t Tails slowly through six tiers <»f brush, n sting on frames, 



lo the bottom. Thence it its again into the tank, to undergo 



rding to Mr. Scribner, one pae 

 Ihmugh the brush favorable weather strengthei 



brine fron i ■ ',-. During the process much of the iron is 



pitated. 



rat, the concentrated brine it d to two 



ttle i. ►use, each holding 8,000 gallons. Here a 

 link . Ided. I'. ; . 



iles. Al er boiling some time in tl 

 I bi m<- is 1 1 ansfei red to four \ 



t by 



I is prol ably gypsum. 



From here it - <1 into the back kettles, and the evapo- 



ration continued. As the salt falU 4own, it is skimmed into 



