Özet:

Nevşehir and its nearby surroundings are largely composed of volcanic shapes and units in different lithologies. The volcanic rally has also influenced the urban development, the use of land and the formation of the capadocyan peribacas, one of Turkey’s most important tourist areas. In order to investigate the impact of volcanic structures and litological units on both the city and the formation of peribacus, a series of studies have been carried out in the field and geomorphological evolution model has been developed according to the rule of numeric maps, geomorphological maps, diagrams, volcanic reversion (inversion). The most important aspects that attract attention in the geomorphological development of the Nevşehir environment are the path of polysicity (multi-stage) development that occurs with both tectonic and volcanic effects and the topographic disruption events that occur due to different exhaustion. Therefore, a wealth of rally in the city and its nearby surroundings appears (volcanic domes, volcanic plates, volcanic coins, trap, volcanic turning stairs, foil stairs, foil mirrors, moses, witness mountains, peribacas, etc.). As an active morphology, redness in the field today is more influential due to the influence of the arms and the fluvial infection process. This process has also led to the formation of badlands topography, which occurs in the form of selective intersection with the erosion of the threshold with the influence of litological factors, and quite rich, but also a wide variety of peribacas.