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Lekhziri Glacier
Lekhziri Glacier ( ka, ლეხზირი) is a valley glacier located on the southern slopes of the Greater Caucasus Mountain Range in the Svaneti Region of Georgia. The length of the glacier is and its surface area is . The tongue of the glacier descends down to above sea level. Lekhziri consists of three separate glaciers; North, East and West Lekhziri. From the point where the three different glaciers intersect, the surface of Lekhziri becomes largely covered with morainal sediments and debris. The glacier feeds off the ice-flows and avalanches from the adjacent mountains. See also *Glaciers of Georgia The glaciers of Georgia are mainly located along the Greater Caucasus Mountain Range. Geography The spatial distribution of contemporary glaciers in the territory of Georgia is stipulated by the peculiarities of atmospheric processes, morpho ... References * ''Georgian State (Soviet) Encyclopedia.'' 1983. Book 6. p. 209. Glaciers of Georgia (country) ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Valley Glacier
A valley is an elongated low area often running between hills or mountains, which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In areas of limestone bedrock, dry valleys may also result from drainage now taking place underground rather than at the surface. Rift valleys arise principally from earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms that may be global in use or else applied only locally. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Svaneti
Svaneti or Svanetia (Suania in ancient sources; ka, სვანეთი ) is a historic province in the northwestern part of Georgia (country), Georgia. It is inhabited by the Svans, an ethnic subgroup of Georgians. Geography Situated on the southern slopes of the central Caucasus Mountains and surrounded by 3,000–5,000 meter peaks, Svaneti is the highest inhabited area in the Caucasus. Four of the 10 highest peaks of the Caucasus Mountains, Caucasus are located in the region. The highest mountain in Georgia, Mount Shkhara at 5,201 meters (17,059 feet), is located in the province. Prominent peaks include Tetnuldi (4,974 m / 16,319 ft), Shota Rustaveli (4,960 m / 16,273 ft), Mount Ushba (4,710 m / 15,453 ft), Ailama (4,525 m / 14,842 ft), as well as Lalveri, Latsga and others. Svaneti has two parts corresponding to two inhabited valleys: * Upper Svaneti (''Zemo Svaneti'') on the upper Inguri River; administratively part of Samegrelo-Zemo Svaneti; mai ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Georgia (country)
Georgia (, ; ) is a transcontinental country at the intersection of Eastern Europe and Western Asia. It is part of the Caucasus region, bounded by the Black Sea to the west, by Russia to the north and northeast, by Turkey to the southwest, by Armenia to the south, and by Azerbaijan to the southeast. The country covers an area of , and has a population of 3.7 million people. Tbilisi is its capital as well as its largest city, home to roughly a third of the Georgian population. During the classical era, several independent kingdoms became established in what is now Georgia, such as Colchis and Iberia. In the early 4th century, ethnic Georgians officially adopted Christianity, which contributed to the spiritual and political unification of the early Georgian states. In the Middle Ages, the unified Kingdom of Georgia emerged and reached its Golden Age during the reign of King David IV and Queen Tamar in the 12th and early 13th centuries. Thereafter, the kingdom decl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Valley Glacier
A valley is an elongated low area often running between hills or mountains, which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In areas of limestone bedrock, dry valleys may also result from drainage now taking place underground rather than at the surface. Rift valleys arise principally from earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms that may be global in use or else applied only locally. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glaciers Of Georgia
The glaciers of Georgia are mainly located along the Greater Caucasus Mountain Range. Geography The spatial distribution of contemporary glaciers in the territory of Georgia is stipulated by the peculiarities of atmospheric processes, morphological-morphometric conditions of the relief and their interaction. Main centers of glaciation are related to the elevated Greater Caucasus watershed range and Kazbegi massif. Individual centers can be found in the Greater Caucasus branch ranges: Bzipi, Kodori, Samegrelo, Svaneti, Lechkhumi Range, Pirikita, etc. According to the data of 2015 there are 637 glaciers in Georgia with a total area of 355.80 km2. Contemporary glaciers are mainly concentrated in the Enguri, Rioni, Kodori and Tergi River basins, where there are the peaks of 4500 m and higher. 89.32% of the amount and 97.15% of the area of glaciers of Georgia are located in these basins. Contemporary glaciers are unevenly distributed between the different river basins. Here t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glaciers Of Georgia (country)
The glaciers of Georgia are mainly located along the Greater Caucasus Mountain Range. Geography The spatial distribution of contemporary glaciers in the territory of Georgia is stipulated by the peculiarities of atmospheric processes, morphological-morphometric conditions of the relief and their interaction. Main centers of glaciation are related to the elevated Greater Caucasus watershed range and Kazbegi massif. Individual centers can be found in the Greater Caucasus branch ranges: Bzipi, Kodori, Samegrelo, Svaneti, Lechkhumi Range, Pirikita, etc. According to the data of 2015 there are 637 glaciers in Georgia with a total area of 355.80 km2. Contemporary glaciers are mainly concentrated in the Enguri, Rioni, Kodori and Tergi River basins, where there are the peaks of 4500 m and higher. 89.32% of the amount and 97.15% of the area of glaciers of Georgia are located in these basins. Contemporary glaciers are unevenly distributed between the different river basins. Here t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
