GEOLOGICAL AND HYDROGEOLOGICAL INVESTIGATION OF KÖŞKKÖY THERMAL SPRING, HÜYÜK-KONYA

Abstract

In the study area, Paleozoic and Tertiary aged rock units outcrop. Paleozoic aged rock units which form the basement, are peliticschists, sericitschists, chloriteschists, quartzschists, quartzites and marbles. Pliocene aged rock units, which are lacustrine sediments, conglomerates, sandstones, siltstones, claystones and sandy limestones overlie this basement with angle disconformity. The meteoric water, circulated in the region is heated by the effect of geothermic gradient and emerges near the small town of Köşk, forms the Köşk thermal. Recharge of the thermal water is 3,66 l/s in 20.08.1997 and 3,46 l/s in 21.09.1997. Temperature of the water is 35 oC which measured by using max-thermometer in the emerging point of (well) the water. According to do thermal measurements and the results of chemical analyses the water can be defined as "Ca, Mg, SO4 thermal and mineralized water" by the IUGS standarts. AB/2 = 700 m Rezistivite Deep Electric Drilling has been done to increase the recharge and temperature of the Köşk thermal water at seven points in 7-8 Septemper, 1997. In the light of this geophysical investigations and with the support of geological and hydrogeological conditions, it can be expected that the temperature and recharge of the thermal water would be increased. On the basis of geophysic resiztivite data, to increase of water recharge and its temperature it is suggested that the best drilling sites are between 2 and 3 well-points which are located between fault and high-resiztivite chalkschists-quartzite within schists.

Keywords

• Köşkköy, Kaplıca, Jeotermik gradyan, Debi, Rezistivite