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Tviberi Glacier
Tviberi ( ka, ტვიბერი) is a glacier located in the Svaneti Region of Georgia on the southern slopes of the Greater Caucasus Mountain Range. The length of the Tviberi Glacier is and its surface area is . The tongue of the glacier descends to above sea level. Tviberi represents a polisynthetic type of a valley glacier. It has many tributaries among which are Laskhedari, Iriti, Asmashi, Toti, Seri and others. The surface of Tviberi is mainly covered with morainal sediments and debris. The glacier feeds off of the runoff and ice flows from the adjacent peaks.''Georgian State (Soviet) Encyclopedia.'' 1985. Book 9. p. 710. The nearest larger community is Mestia, 13.5 km southwest of Tviberi Glacier. The area around Tviberi Glacier consists mainly of grassland A grassland is an area where the vegetation is dominated by grasses ( Poaceae). However, sedge ( Cyperaceae) and rush ( Juncaceae) can also be found along with variable proportions of legumes, like clover ... [...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] |
Mestia
Mestia ( ka, მესტია ) is a highland townlet ('' daba'') in northwest Georgia, at an elevation of in the Caucasus Mountains. General information Mestia is located in the Svaneti region of Samegrelo-Zemo Svaneti province (''mkhare''), some northeast of the regional capital of Zugdidi. Mestia and the adjoining 132 villages form Mestia District (''raioni''). Its area is ; and its population is 9,316 (1,973 in the town itself), according to the 2014 Georgia census. It was granted the status of a townlet (Georgian: ''daba'') in 1968. Historically and ethnographically, Mestia has always been regarded a chief community of Zemo, or Upper Svaneti province. It was formerly known as Seti (სეტი). The population is mostly Svans, a cultural and linguistic subgroup of the Georgians. Despite its small size, the townlet was an important centre of Georgian culture for centuries and contains a number of medieval monuments, such as churches and forts, included in a list of UNESCO ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Grassland
A grassland is an area where the vegetation is dominated by grasses (Poaceae). However, sedge (Cyperaceae) and rush (Juncaceae) can also be found along with variable proportions of legumes, like clover, and other herbs. Grasslands occur naturally on all continents except Antarctica and are found in most ecoregions of the Earth. Furthermore, grasslands are one of the largest biomes on earth and dominate the landscape worldwide. There are different types of grasslands: natural grasslands, semi-natural grasslands, and agricultural grasslands. They cover 31–69% of the Earth's land area. Definitions Included among the variety of definitions for grasslands are: * "...any plant community, including harvested forages, in which grasses and/or legumes make up the dominant vegetation." * "...terrestrial ecosystems dominated by herbaceous and shrub vegetation, and maintained by fire, grazing, drought and/or freezing temperatures." (Pilot Assessment of Global Ecosystems, 2000) * "A ... [...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] |
