Water spring are vital to all human activities. The integration of hydrological, geological, hydrogeological and ecological characteristics of resource ecosystems provides a much needed tool for recognizing the characteristics and their distribution. The objective of this study was to identify springs in the study area, in order to evaluate their hydrogeological characteristics and parameters. Eight springs have been identified in the Golesh Massif area. They are mainly of lithological contact. Water flow ranging from 0.03 to 5 l/s, the temperature, pH and total hardness in the water of spring Curreli range within 11.1 to 15.7 °C, 5.51 to 8.03 °C and 18.8 to 21.67 °dH, respectively. Their recharge mainly depends on the amount of precipitations that falls in the area.
Kosovo is distinguished by a particularly high degree of seismic activity as a result of its location in the alpine-Mediterranean seismic area. The thickness of the seismic zone in the Earth’s crust is a crucial element in seismotectonics, as it affects the design of fault systems, relative fault activity, earthquake size and distribution within a fault system, and the long-term accumulation of tectonic deformation. Kosovo’s large depressions and high relief make it challenging geomorphologically. The country of Kosovo is divided into numerous chunks along the fault lines because of the inclinations of these prevalent motions. Normal faults, along which differentiations on the order of 2000 m occurred during the neotectonics period, identify the contacts between these blocks. Understanding Kosovo’s seismotectonic characteristics requires an exact analysis of hypocenter parameters when historical earthquakes that have struck the country are reassessed for magnitude. This study deals with the seismicity and tectonics of the territorial space of the Republic of Kosovo.
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