AI Summary & Key Takeaways
AI InsightFrom these conclusions we try to evaluate the underground water reserves and losses of the Fethiye Plain.
📌 3 Key Takeaways
Abstract
The surface under investigation in the Fethiye plain is about 450 km². The main geological formations are: various kinds of limestones, green rocks, such as serpentine, and alluviums. The main tectonic and morphologic characteristics are the numerous faults, karsts and flood cones. The yearly rainfall average is 1000 to 1200 mm, the temperature average is 19°, and the yearly evaporation average is 1200 mm. From the minimum yields of the small rivers of the area, measured during the dry period, the minimum infiltration rate of the geological formations has been estimated and compared with similar results in other countries. From these conclusions we try to evaluate the underground water reserves and losses of the Fethiye Plain.
Özet
Fethiye ovası etüd sahası 450 km² kadardır. Raslanan formasyonlar başlıca çeşitli kalkerler ve yeşil sahrelerle alüvyoner formasyonlardan ibarettir. Araziye tektonik bakımdan fay stili hâkim bulunmaktadır. Morfolojik yönden karstik hâdiselerle sel konileri dikkati çekmektedir.