BaILey. | 
Mineral Waters. 
181 
Stotler Well, Lyon County. 
The water of a well at Stotler has the following composition : 
Grams per liter. 
IONS. RADICALS. 
Sodiuma(Na apa whee aes: .0970 | Sodium oxid (NaeO)............ .1308 
IPotassiamy (khan esa. oe: .0554 | Potassium oxid (K2O).......... .0668 
Callciumy (Calter. age a S21 Som le alciumyoxi da (Ca®) pre 2987 
Maenesiumy (Mio) essere a: ae. .0560 | Magnesium oxid (MgO)......... .0934 
1H) Royo) (() aN)) Seas eo Aad ee O52} || Gro OrdiGl (IAN). occcceccogbo0cc .0453 
Chilontny(Cl)ieeenae ee. ess 4 OGD. | Clarina (M)occccccaccceoecoc0es .0169 
Sulfuric acid ion (SO4)......... .9476 | Sulfuric anhydrid (SOsz)........ . 1897 
Phosphoric acid ion (POs)...... .0006 | Phosphoric anhydrid (P:O;)..... .0004 
Silicic acid ion (SiOs)........... .0420 | Silica (Si@o)......... ales aN eae .0332 
Carbonic anhydrid ... not determined 
Analysis by G. H. Failyer and J. T. Willard. 
Sun Springs, Brown County. 
These springs are located three miles southwest of the town 
of Morrill, Brown county, on the St. Joseph & Grand Island 
railway. This is a high, rolling country, and is well watered. 
These springs are in the valley of Mulberry creek, a stream that 
runs east and then north, and at last finds its way into the 
Nemaha. 
IMPROVEMENTS. 
This property was developed in 1898. The new hotel is just 
in the edge of the timber, a little to the north of the grove in 
which the springs are situated. A bath-house has also been 
erected, with baths for giving hot and cold baths, and a dam 
thrown across the valley makes a lake, which gives facilities 
for boating. There are a large number of springs within a 
radius of an eighth of a mile, and water is found in abundance 
wherever a small excavation is made in the ground. The soil 
seems to be peculiar in that it is very springy, and at a short 
distance below the surface is full of large nodules, consisting of 
clay and iron minerals. 
The principal spring is No. 1, a few rods southwest of 
the hotel. This is improved by being built up and cemented 
to a point about three feet above the surface. It is eight feet 
in diameter and eight feet deep, and a stream nearly filling a 
58. Trans. Kan, Acad. Sci., vol. X, p. 64. 
