Geosites are formations that constitute evidence of the geological-geomorphological history of the earth, are important in terms of science, education, culture, landscape and landscape, and should be preserved and left to future generations. While geosites are mostly formed as a result of natural events and processes, some of them may be human-made elements shaped by the influence of the geological-geomorphological features of the place. Rock communities, fossil beds, mineral deposits, important geological-geomorphological structures, volcanic shapes, meteor pits, landforms, old mineral deposits, mounds and tumuli can be given as examples of geosites. The areas in question may be of local, regional, national or even international importance.