| Keli Highland | |
|---|---|
.jpg) Keli Lake and Keli Highland | |
| Highest point | |
| Elevation | 3,736 m (12,257 ft)[1] |
| Coordinates | 42°27′N44°15′E / 42.45°N 44.25°E /42.45; 44.25[1] |
| Geography | |
  Keli Highland  Keli Highland | |
| Parent range | Greater Caucasus |
TheKeli (Qeli) Highland (Georgian:ყელის ზეგანი,qelis zegani) is avolcanic field inGeorgia on the western side of theJvari Pass south to theGreater Caucasus range. More than thirty volcanic edifices on an area of 20x30km2 make up this volcanic field, which consists mostly of monogenetic volcanic structures.[2] The lavas arerhyolites,trachyandesites andandesites.[3]
The riversTetri Aragvi,Patara Liakhvi,Ksani andDidi Liakhvi originate from the Keli volcanic area, and some peaks drain into theTerek river. Several mountain ranges separate the area into distinct high plains. QuaternaryDacite lava flows overlie thichMesozoic sedimentary sequences.[2][4]
Western Khorisar (elevation 3736 m) and Didi-Nepiskalo (3694 m) are the highest summits close to the crest of theGreater Caucasus.[4] In the northeastern part of the system are the Nepiskalo volcanoes and several smaller structures. The Patara-Nepiskalo volcano is strongly degraded by glacial action and may have had a caldera. Other volcanoes are Sharkhokh, Northern Shadilkhokh, and Southern Shadilkhokh in the western Kaidon range and the lava flows created by the latter two volcanoes between theArkhi Range,Keli Lake and theAragvistavi river, the Ermani–Akhubata lava plateau, Eastern Sharkhokh volcano and several lava domes (Ermani, Fidarkokh and others).[2][4]
Nikoloz Skhirtladze first studied the volcanoes and divided the volcanism into glacial and postglacial stages.[2] Later research indicated three phases of volcanism: A first phase 245–170ka involvedlava dome formation including Kordieritovyi dome, Patara-Nepiskalo volcano and Kabardzhin–Sakokhe centre and its associated a laval flow in the Aragvi valley. A second phase 137–70ka with large scale effusive activity included the "Pyramidal Peak" Volcano which dammed local rivers with lava flows. From 90ka on activity formed Didi-Nepiskalo and the Ekisom and Khorisar domes. The third phase less than 30ka with evidence that it continued into the Holocene formed Eastern Khorisa and Ploskaya Vershina. Activity of East Khorisar Volcano spans both stages and created lava flows in theTerek river valley, at the end involving the collapse of the northern flank of its crater.[4][3]