Official Name: | Kandovan |
Native Name: | كندوان |
Settlement Type: | Village |
Pushpin Map: | Iran |
Mapsize: | 150px |
Subdivision Type: | Country |
Subdivision Type1: | Province |
Subdivision Name1: | East Azerbaijan |
Subdivision Type2: | County |
Subdivision Name2: | Osku |
Subdivision Type3: | Bakhsh |
Subdivision Name3: | Central |
Subdivision Type4: | Rural District |
Subdivision Name4: | Sahand |
Population As Of: | 2006 |
Population Total: | 601 |
Population Density Km2: | auto |
Timezone: | IRST |
Utc Offset: | +3:30 |
Timezone Dst: | IRDT |
Utc Offset Dst: | +4:30 |
Coordinates: | 37.795°N 46.2486°W |
Kandovan (Persian: كندوان, also romanized as Kandovān and Kandavān; also known as Kanvān) is an ancient village in Sahand Rural District in the Central District of Osku County, East Azerbaijan Province, northwestern Iran. It is situated in the foothills of Mount Sahand, near the city of Osku. At the 2006 census, the village population was 601, in 168 families.
The village exemplifies manmade cliff dwellings which are still inhabited. The troglodyte homes, excavated inside volcanic rocks similar to dwellings in the Turkish region of Cappadocia, are locally called Karaan.[1] Karaans were cut into non-welded ignimbrites, also called "ash-flow tuffs," of Mount Sahand. The cone form of the houses is the result of the erosion of ignimbrite layers consisting of porous, round and angular pumice together with other volcanic particles that were positioned in a grey, acidic matrix. During the eruption of Sahand, pyroclastic flows formed the rocks of Kandovan. Around the village the thickness of this formation exceeds and with time, due to water erosion, the cone-shaped cliffs were formed.[2]
Mount Sahand is one of the most important mountains, the Silent volcano in Iran for one hundred and forty thousand years ago, After the retreat of Kandovan Lake basin, The stone of Kandovan has appeared.There are several narrations about the causes of the emergence of the village: