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Adishi
Mount Adishi ( ka, ადიში) also known as Hadishi, is a peak in the central part of the Greater Caucasus Mountain Range. The elevation of the mountain is above sea level. The mountain is made up of paleozoic granites. The slopes of Adishi are covered by glaciers. See also *Adishi Glacier Adishi Glacier ( ka, ადიშის მყინვარი) is a valley glacier located in the central part of the Greater Caucasus Mountain Range in the Svaneti Region of Georgia. The glacier lies on the southern slopes of the Caucasus. Th ... References * ''Georgian State (Soviet) Encyclopedia.'' 1975. Book 1. p. 96. Mountains of Georgia (country) Svaneti Four-thousanders of the Caucasus {{georgia-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Adishi Glacier
Adishi Glacier ( ka, ადიშის მყინვარი) is a valley glacier located in the central part of the Greater Caucasus Mountain Range in the Svaneti Region of Georgia. The glacier lies on the southern slopes of the Caucasus. The length of the Adishi Glacier is and its surface area is . The tongue of the glacier descends down to above sea level. The glacier feeds off of the runoff and ice flows from the adjacent glaciers that are located on the southern slopes of Tetnuldi, Gistola and Lakutsia. The Adishi Glacier is the source of the river Adishischala. The glacier takes its name from the nearby village Adishi. See also * Mount Adishi *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) Encycloped ... [...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] |
Caucasus Mountains
The Caucasus Mountains, : pronounced * hy, Կովկասյան լեռներ, : pronounced * az, Qafqaz dağları, pronounced * rus, Кавка́зские го́ры, Kavkázskiye góry, kɐfˈkasːkʲɪje ˈɡorɨ * tr, Kafkas Dağları, * fa, كوه هاى قفقاز are a mountain range at the intersection of Asia and Europe. Stretching between the Black Sea and the Caspian Sea, they are surrounded by the Caucasus region and are home to Mount Elbrus, the list of elevation extremes by region, highest peak in Europe at above sea level. The Caucasus Mountains include the Greater Caucasus in the north and Lesser Caucasus in the south. The Greater Caucasus runs west-northwest to east-southeast, from the Western Caucasus, Caucasian Natural Reserve in the vicinity of Sochi, Russia on the northeastern shore of the Black Sea to Baku, Azerbaijan on the Caspian Sea. The Lesser Caucasus runs parallel to the Greater about south. The Greater and Lesser Caucasus ranges are co ... [...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] |
Paleozoic
The Paleozoic (or Palaeozoic) Era is the earliest of three geologic eras of the Phanerozoic Eon. The name ''Paleozoic'' ( ;) was coined by the British geologist Adam Sedgwick in 1838 by combining the Greek words ''palaiós'' (, "old") and ''zōḗ'' (), "life", meaning "ancient life" ). It is the longest of the Phanerozoic eras, lasting from , and is subdivided into six geologic periods (from oldest to youngest): # Cambrian # Ordovician # Silurian # Devonian # Carboniferous # Permian The Paleozoic comes after the Neoproterozoic Era of the Proterozoic Eon and is followed by the Mesozoic Era. The Paleozoic was a time of dramatic geological, climatic, and evolutionary change. The Cambrian witnessed the most rapid and widespread diversification of life in Earth's history, known as the Cambrian explosion, in which most modern phyla first appeared. Arthropods, molluscs, fish, amphibians, reptiles, and synapsids all evolved during the Paleozoic. Life began in the ocean ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Georgia (country)
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
