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Shavnabada (Samsari)
Shavnabada ( ka, შავნაბადა) 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. References L. Maruashvili, Georgian Soviet Encyclopedia The ''Georgian Soviet Encyclopedia'' ( ka, ქართული საბჭოთა ენციკლოპედია, ქსე) is the first universal encyclopedia in the Georgian language, printed in Tbilisi from 1965, the editor in chi ..., V. 10, p. 675, Tbilisi, 1986. category:Volcanoes of Georgia (country) Mountains of Samtskhe-Javakheti region Extinct volcanoes Stratovolcanoes {{Georgia-geo-stub ... [...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] |
Abul-Samsari Range
Samsari RangeOrthographic dictionary of geographic names of Georgian, p. 148, Tbilisi, 2009 ( ka, სამსრის ქედი) is a volcanic range in southern Georgia, to the southwest of Tbilisi. It is a part of the Highland of Southern Georgia and rises above the Javakheti and Tsalka Plateaus. The range itself is long and runs north to south from the Ktsia to the Paravani River Gorges. There is archaeological evidence of ancient forts on some of the peaks. Mountains The highest mountain is Didi Abuli at an elevation of above sea level. Other notable peaks include: * Godorebi () * Karakuzei () * Shavnabada () * Samsari () * Mt. Tavkvetili () * Western Shaori () Mount Samsari has a fairly large caldera, the floor of which is covered by the rocks from the mountain's last eruption. Vegetation The slopes of the Abul-Samsari Range are mainly covered with alpine meadows and grasslands. Forests are less common and are usually found at the lowest elevations of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Extinct Volcano
A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates are diverging or converging, and most are found underwater. For example, a mid-ocean ridge, such as the Mid-Atlantic Ridge, has volcanoes caused by divergent tectonic plates whereas the Pacific Ring of Fire has volcanoes caused by convergent tectonic plates. Volcanoes can also form where there is stretching and thinning of the crust's plates, such as in the East African Rift and the Wells Gray-Clearwater volcanic field and Rio Grande rift in North America. Volcanism away from plate boundaries has been postulated to arise from upwelling diapirs from the core–mantle boundary, deep in the Earth. This results in hotspot volcanism, of which the Hawaiian hotspot is an example. Volcanoes are usually not created where two tectonic plates slide ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lesser Caucasus
The Lesser Caucasus, also called Caucasus Minor, is the second of the two main mountain ranges of Caucasus mountains, of length about . The western portion of the Lesser Caucasus overlaps and converges with east Turkey and northwest Iran. It runs parallel to the Greater Caucasus, at a distance averaging about south from the Likhi Range (Georgia) and limits east Turkey from the north and north-east. It is connected to the Greater Caucasus by the Likhi Range (Georgia) and separated from it by the Kolkhida Lowland (Georgia) in the west and Kura-Aras Lowland (Azerbaijan) (by the Kura River) in the east. The highest peak is Aragats, . The borders between Georgia, Turkey, Armenia, Azerbaijan and Iran run through the range, although its crest does not usually define the border. The range was historically called ''Anticaucasus'' or ''Anti-Caucasus'' (Greek: Αντι-Καύκασος, Russian Russian(s) refers to anything related to Russia, including: *Russians (, ''russkiye''), ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Georgian Soviet Encyclopedia
The ''Georgian Soviet Encyclopedia'' ( ka, ქართული საბჭოთა ენციკლოპედია, ქსე) is the first universal encyclopedia in the Georgian language, printed in Tbilisi from 1965, the editor in chief of which was Irakli Abashidze. The encyclopedia consists of 11 alphabetic volumes and a 12th exclusively dedicated to the Georgian SSR, printed in both Georgian and Russian. Sources * R. Metreveli, ''Georgian Soviet Encyclopedia'', X, p. 483, Tbilisi, 1986 See also * ''Great Soviet Encyclopedia The ''Great Soviet Encyclopedia'' (GSE; ) is one of the largest Russian-language encyclopedias, published in the Soviet Union from 1926 to 1990. After 2002, the encyclopedia's data was partially included into the later ''Bolshaya rossiyskaya e ...'' National Soviet encyclopedias Georgian Soviet Socialist Republic Georgian-language encyclopedias 20th-century encyclopedias {{Encyclopedia-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanoes Of Georgia (country)
A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates are diverging or converging, and most are found underwater. For example, a mid-ocean ridge, such as the Mid-Atlantic Ridge, has volcanoes caused by divergent tectonic plates whereas the Pacific Ring of Fire has volcanoes caused by convergent tectonic plates. Volcanoes can also form where there is stretching and thinning of the crust's plates, such as in the East African Rift and the Wells Gray-Clearwater volcanic field and Rio Grande rift in North America. Volcanism away from plate boundaries has been postulated to arise from upwelling diapirs from the core–mantle boundary, deep in the Earth. This results in hotspot volcanism, of which the Hawaiian hotspot is an example. Volcanoes are usually not created where two tectonic plates slide pa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Samtskhe-Javakheti Region
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] |
Extinct Volcanoes
A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates are diverging or converging, and most are found underwater. For example, a mid-ocean ridge, such as the Mid-Atlantic Ridge, has volcanoes caused by divergent tectonic plates whereas the Pacific Ring of Fire has volcanoes caused by convergent tectonic plates. Volcanoes can also form where there is stretching and thinning of the crust's plates, such as in the East African Rift and the Wells Gray-Clearwater volcanic field and Rio Grande rift in North America. Volcanism away from plate boundaries has been postulated to arise from upwelling diapirs from the core–mantle boundary, deep in the Earth. This results in hotspot volcanism, of which the Hawaiian hotspot is an example. Volcanoes are usually not created where two tectonic plates slide ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
