Springhead „School fountain“

(Google translate) School fountain according balneologic classification, hypothermal thermo stone source comprising a substantial content of calcium, magnesium hydrogen carbonate, aluminum oxide, iron oxide and silicon dioxide. (Stankovic, S., 2009..) Wellhead School fountain behind for the old school, Niska Banja, where she and encourages title. Rate of 2.5 liters per second, and a water temperature of 17 ° -19 ° C.

 

Springhead „School fountain“

(Google translate) School fountain according balneologic classification, hypothermal thermo stone source comprising a substantial content of calcium, magnesium hydrogen carbonate, aluminum oxide, iron oxide and silicon dioxide. (Stankovic, S., 2009..) Wellhead School fountain behind for the old school, Niska Banja, where she and encourages title. Rate of 2.5 liters per second, and a water temperature of 17 ° -19 ° C.

Due to non-uniform inflow of the water from the spring 1958. Suva bath was carried out to bring the water of the spring to the main springs and in that the composition is embedded temporary divider for mixing the water with these two overflow for excess water. This allows the temperature matching between the water 39 ° C which is the main source to the water and the temperature of the spa Dry ranging between 12 ° and 37 ° C. Over three drain separators enables the supply water bath with three temperature. Many years of comparative meteorološkihm and hydrological observation it was noted that the thermal component of the cure and water constant according to temperature and yield, and that the traffic occurring due to varying the cool karst components, whose amounts are dependent on the atmospheric precipitation in the catchment (collecting) the Suva mountains and Koritnjak.

School fountain is one of the thermo-mineral sources Niške Spa appearing in the southern periphery of the basin under the peaks Niške Koritnjak (808 m), the far western of Suva mountain. They are rasednoj zones, limited the north side kretacejskih limestone KOVANLUK. These are interspersed with numerous limestone dijaklaza filled with white calcite veins. In the very Niškoj Spa on the terrace nišavskoj zastrveni bigra have thick, with an average thickness of the layers about 10 m, but in places up to 20 m.

Coordinates:

Latitude: 43.296083

Longitude: 22.008299