WJavalkheti Plateau is a volcanic plateau within the Caucasus Mountains that covers the Samtskhe-Javakheti region of Georgia, along the border with Turkey and Armenia. Its elevation is over 2,000 m.
WKabargin Oth Group is a group of volcanoes located in Georgia. It consists of a dozen cinder cones and lava domes and is located near the border with Russia, southwest of Mount Kazbek volcano.
WMount Kazbegi is a dormant stratovolcano and one of the major mountains of the Caucasus located on the border of Georgia's Kazbegi District
WThe Keli (Qeli) Highland is a volcanic field in Georgia on the western side of the Jvari Pass south to the Greater Caucasus range. More than thirty volcanic edifices on an area of 20x30km2 make up this volcanic field, which consists mostly of monogenetic volcanic structures. The lavas are rhyolites, trachyandesites and andesites.
WMount Khabarjina is a mountain and dormant volcano in the Caucasus of Georgia. It has an elevation of 3,142 metres. It is located near Mount Kazbek and is a part of its volcanic group. It is better known under the name Mount Kabardzhin.
WMount Leyli, also Leili is a 3,157 m (10,358 ft) tall mountain between the Georgian provinces of Samtskhe-Javakheti and Kvemo Kartli. Leyli is second highest peak of the Javakheti Range in the Lesser Caucasus Mountains.
WMount Samsari is a peak of the Abul-Samsari Range in Southern Georgia. The elevation of the mountain is 3,285 metres (10,778 ft) above sea level. Mount Samsari represents a volcanic cone, inside of which lies a caldera with a diameter of 3 kilometres (1.9 mi) with a semicircular ridge surrounding it. The formation of the caldera is linked to local fault systems. The floor of the caldera is lined with rocks and glacial debris as well as small lakes and contains volcanokarst formations. The caldera rim contains traces of previous glaciation, including cirques. The mountain was built up during the late Quaternary period and is made up of andesites, dacites and rhyolites. The slopes of Samsari are mainly devoid of vegetation. The caldera formed roughly 200ka ago.
WShavnabada is a mountain and extinct volcano of 770 m height in southeastern Georgia, some 96 km from the nation’s capital Tbilisi.
WShavnabada is a mountain and extinct volcano of 2929 m/9507 ft height in southeastern Georgia. It is one of the highest mountains of the Abul-Samsari Range, a part of the Lesser Caucasus.
WMount Tavkvetili is a volcanic mountain in the northern part of the Abul-Samsari Range in the Samtskhe-Javakheti region of Southern Georgia. It is also known as Gora Tavk'vetili and Mta Tavk'vetili. The elevation of the mountain is 2,583 metres (8,474 ft) above sea level and is the 323rd highest mountain in Georgia. The mountain has the shape of a decapitated cone and is composed of young andesitic and andesitic-dacitic lavas. The lower slopes of Mount Tavkvetili are covered by subalpine meadows while the upper slopes are covered by alpine meadows.
WTsiteli Khati is a summit of the Kharuli Range in Northern Georgia. The elevation of the peak is 3,026 metres (9,928 ft) above sea level. The mountain is located within the Kheli Volcanic Region of Georgia, an area which is the largest source of volcanism on the southern slopes of the Greater Caucasus Mountain Range within Georgia's boundaries. Tsiteli Khati is built up of holocene age andesites and dacitic lavas. The peak itself is a young volcanic cone with slopes that show no signs of any significant erosion. The vegetation of the mountain consists of subalpine and alpine meadows.
WMount Yemlikli, also Emlikli, Emlik'li is a 3,054 m (10,020 ft) tall mountain near Saghamo and between the Georgian provinces of Samtskhe-Javakheti and Kvemo Kartli. Yemlikli is one of the high peaks of the Lesser Caucasus Mountains and is in the Javakheti Range.