CRANE. | Mineral Springs and Wells. 325 
the Sub-Carboniferous, or from a point near the contact of the 
Sub-Carboniferous and Lower Silurian. 
Bourbon County. The two Bourbon county wells discussed 
in this report are located at Fort Scott. These wells are known 
as the artesian and sulfo-magnesian. They both tap the 
Lower Silurian, from which they draw their waters. 
Iinn County. The La Cygne iron spring is located in and 
draws its water from the Lower Carboniferous. 
Neosho County. The St. Paul well, although located in the 
Lower Carboniferous, derives its waters from the Sub- Carbonifer- 
ous or Lower Silurian, possibly both. 
UPPER CARBONIFEROUS. 
Labette County. The Mound Valley well probably drains Lower 
Carboniferous strata. 
The Parsons mineral well is situated about on the outcrop of 
the Upper and Lower Carboniferous strata, but, being shallow, 
may le wholly within the Upper Carboniferous. 
Montgomery County. The Independence bromo-magnesian 
well passes through both Upper and Lower Carboniferous and 
derives its supply from either the Sub-Carbononiferous or Lower 
Silurian. 
The Coffeyville alll hes wholly within the Upper Carbonifer- 
ous strata. 
The Coffeyville artesian well taps the Lower Silurian, from 
which it derives its waters. 
The Parkhurst spring has its source in the Upper Carboniferous 
strata. 
Chautauqua County. Chautauqua springs lie within and re- 
ceive their waters from the Upper Carboniferous. 
Wilson County. The Fredonia well extends to the Lower 
Silurian and probably gets its water from the same. 
The Coyville well draws its supply from the Upper or {ohare 
Carboniferous. 
The Delaware springs, at Stella, ie wholly within the Upper 
Carboniferous. 
