Some of the important geosites of Geopak that must be seen.
It is one of the most important volcanic forms formed in the third phase of Kula volcanism (Divlit Tepe Volcanics). In terms of formation and shape features, it is in the type of cinder cone or scour cone.
It is one of the most important volcanic forms formed in the 3rd phase of the Kula Volcanism (Divlit Tepe Volcanics). In terms of formation and shape features, it is in the type of cinder cone or scoria cone.
Kula, 18. yüzyıl Osmanlı kent mimarisinin Türkiye’deki en iyi korunan alanlarından biridir. Kula evleri, yalnızca mimari tarzı değil aynı zamanda Osmanlı kentlerinde günlük sosyal yaşamın genel bir görüntüsünü yansıtmaktadır.
In the Kula-Salihli UNESCO Global Geopark, the Fairy Chimneys were formed due to the joint effect of raindrop erosion, surface erosion and tunnel / piping developed within the soft layer.
The volcanic rocks you see here were formed as a result of the spreading of the lava that emerged as a result of the activation of Toytepe Volcano, located at the northernmost end of the Sarnıç Plateau, approximately 1,260 million years ago.
It is one of Turkey's most important 15 geothermal fields. Located in the lower extremities of Kurşunlu stream, the area is on the Izmir Ankara road and is an important thermal tourism area.
The tradition of pottery making for centuries is maintained by more than 100 households in Gökeyüp. In Gökeyüp, where old techniques are still used, pottery-eyed gneiss is obtained by grinding the bedrock.