CRANE. | Mineral Springs and Wells. 327 
Shawnee County. The Boon, Capital and Topeka wells lie 
within the Upper Carboniferous, which is the source of their 
supply. Phiilips’s spring also receives its waters from the Up- 
per Carboniferous strata. | 
Riley County. The Blasing well, at Manhattan, lies wholly 
within the Upper Carboniferous. 
Leavenworth County. The Kickapoo and Linwood springs 
both derive their waters from the Upper Carboniferous. 
Atchison County. The prospect-hole well, south of Atchison, 
penetrated the Lower Silurian, but receives its waters both from 
the Sub- and Lower Carboniferous strata. 
The Becker and A. B. C. Laundry wells have, as a source of 
their waters, the Upper Carboniferous. 
The Dixon, McDuff, Arrington and Parker springs obtain 
their waters from the Upper Carboniferous strata. 
Doniphan County. The Hagle springs lie wholly within the 
Upper Carboniferous strata. 
Brown County. The Sun and Sycamore springs both receive 
their supply from the Upper Carboniferous. 
Nemaha County. The Centralia gypsum well draws its supply 
from the Upper Carboniferous strata, but may be contaminated 
with the gypsum salts from the Permian strata to the westward. 
The Capioma well probably drains Upper Carboniferous 
strata. 
Wyandotte County. The Wyandotte gas well penetrates the 
Lower Carboniterous strata, from which it receives its supply. 
The Forest Lake well is Upper Carboniferous. 
Bonner and Forest Lake springs lie wholly within the Upper’ 
Carboniferous formation. 
PERMIAN. 
Sumner County. The Conway spring is situated on the out- 
crop of the Upper and Lower Permian, or the Red Beds and 
the Permian strata, receiving its waters largely from the former. 
Butler County. The Providence mineral well probably draws 
its waters from the Upper Carboniferous strata. 
