What makes this place unique
Terrain, waters and landscape
Terrain
At the bottom of this valley within the borders of Polateli, there is a rich river and flora ecosystem. You can utilize the Harita section to see the deepest points of the valley and the surrounding trails. The alluvial soils at the valley bottom are also suitable for traditional viticulture activities in southeastern Türkiye.
Practical notes before you go
Visit
- Type
- Canyons
- Tip
- Check weather and trail conditions before visiting high terrain.
Related places around here
Nearby
Mountain
3)
Mountain
Polateli Hills
These hills, forming the rugged morphology of Polateli district, lay the groundwork for microclimatic conditions.
Mountain
Ravanda Mountain Foothills
The slopes of the mountainous mass extending into the boundaries of Polateli draw attention with their steep and limestone structure.
Mountain
Ravanda Castle Hill
Rising within the borders of Polateli , this historical and natural hill is known for the castle upon it. It is one of the most iconic elevations in the geography of Kilis .
Plain
2
Plain
Polateli Agricultural Plain
The plains spreading across the center and villages of Polateli form the most fertile agricultural production areas of the region.
Plain
Polateli Plain
This fertile plain located within Polateli is the heart of agricultural activities. Making up a large part of the agricultural land in the region, the plain holds an important place throughout Kilis .
Lakes
1Plateau
1Forest
1Stream
3
Stream
Afrin Stream (Polateli Basin)
The branches of the Afrin Stream passing through Polateli lands shape the hydrographic structure and fertile lands of the district.
Stream
Sogutlu Stream
Flowing through the valleys of Polateli and having a seasonal flow, Sogutlu Stream is an important part of the local ecology.
Stream
Afrin Stream (Polateli Section)
Passing through the lands of Polateli , the Afrin Stream is the most important water resource of the region. The river, which is the lifeblood of district agriculture, has a critical role in the hydrography of Kilis .
