Artesian Mineral Water of the Raotince Site, Tetovo

Abstract

A number of mineral springs occur on the west and east peripheral part of the Polog valley. Their appearance is connected with the Western Polog fault that stretches west to the brim of the valley NE–SW direction and east direction of Polog fault stretches in NW–SE. Тhis paper presents the results of detailed hydrogeological investigations of mineral water at the site Raotince Tetovo. Based on data obtained on two operational investigative boreholes at the site in Raotince of the pleistocene limnic sediments at a depth of 38–67 m is founded artesian aquifer with low mineralized water.