Samsari Range
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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 ...
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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 ...
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Mount Samsari
Mount Samsari ( ka, სამსარი) is a peak of the Abul-Samsari Range in Southern Georgia. The elevation of the mountain is above sea level. Mount Samsari represents a volcanic cone, inside of which lies a caldera with a diameter of 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, dacite Dacite () is a volcanic rock formed by rapid solidification of lava that is high in silica and low in alkali metal oxides. It has a fine-grained (aphanitic) to porphyritic texture and is intermediate in composition between andesite and rhyolite ...s and rhyolites. The slopes of Samsari are mainly devoid of vegetation. The caldera formed rough ...
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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''), ...
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Javakheti Range
Javakheti Range or Javakhk Range (also Kechut Range or Wet Mountains; ka, ჯავახეთის ქედი; hy, Ջավախքի լեռնաշղթա) – is a volcanic range in southern Georgia and northern Armenia. The range is about 50 km (31 mi) long and runs north to south from Trialeti to Bazum Range. The highest peak is Achkasar at an elevation 3196 m (10485 ft) above sea level. Other notable peaks include Leyli (3154), Yemlikli (3054), Garanlig (3039), Aghrigar (2973) and Shambiani (2923). Javakheti Range is known with a lot of rainfall too. The name of Wet Mountains originated herein. Range are mainly covered with alpine meadows and grasslands. There are a number of small-sized lakes in and around the Javakheti Range. See also * Mount Yemlikli * Mount Leyli * Javakheti Plateau * Abul-Samsari Range * Lesser Caucasus The Lesser Caucasus, also called Caucasus Minor, is the second of the two main mountain ranges of Caucasus mountains, of length abou ...
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Paravani Lake
__NOTOC__ Paravani lake ( ka, ფარავნის ტბა; hy, Փարվանա (Parvana)) is a volcanic lake in Georgia, located in Javakheti Plateau between Abul-Samsari and Javakheti Ranges. Geography and hydrography Paravani Lake is located above sea level and has a surface area of and a drainage basin of . Its maximum and average depths are and respectively. The volume of the lake is . The water level is low during October and November and is high during May and June. The lake is frozen during wintertime and the thickness of the ice ranges from . In addition to the small rivers of Shaori, Sabadostskali, and Rodionovskis Tskali, the lake gets its water from snow, rain, and underground springs. The river Paravani begins from the southern part of the lake, and connects to the Mtkvari The Kura is an east-flowing river south of the Greater Caucasus Mountains which drains the southern slopes of the Greater Caucasus east into the Caspian Sea. It also drains the n ...
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Grasslands
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 r ...
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Alpine Meadow
Alpine tundra is a type of natural region or biome that does not contain trees because it is at high elevation, with an associated harsh climate. As the latitude of a location approaches the poles, the threshold elevation for alpine tundra gets lower until it reaches sea level, and alpine tundra merges with polar tundra. The high elevation causes an adverse climate, which is too cold and windy to support tree growth. Alpine tundra transitions to sub-alpine forests below the tree line; stunted forests occurring at the forest-tundra ecotone are known as ''Krummholz''. With increasing elevation it ends at the snow line where snow and ice persist through summer. Alpine tundra occurs in mountains worldwide. The flora of the alpine tundra is characterized by dwarf shrubs close to the ground. The cold climate of the alpine tundra is caused by adiabatic cooling of air, and is similar to polar climate. Geography Alpine tundra occurs at high enough altitude at any latitude. Portions ...
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Caldera
A caldera ( ) is a large cauldron-like hollow that forms shortly after the emptying of a magma chamber in a volcano eruption. When large volumes of magma are erupted over a short time, structural support for the rock above the magma chamber is gone. The ground surface then collapses into the emptied or partially emptied magma chamber, leaving a large depression at the surface (from one to dozens of kilometers in diameter). Although sometimes described as a Volcanic crater, crater, the feature is actually a type of sinkhole, as it is formed through subsidence and collapse rather than an explosion or impact. Compared to the thousands of volcanic eruptions that occur each century, the formation of a caldera is a rare event, occurring only a few times per century. Only seven caldera-forming collapses are known to have occurred between 1911 and 2016. More recently, a caldera collapse occurred at Kīlauea, Hawaii in 2018. Etymology The term ''caldera'' comes from Spanish language, S ...
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Tavkvetili
Mount Tavkvetili ( ka, თავკვეთილი) 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 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 Andesite () is a volcanic rock of intermediate composition. In a general sense, it is the intermediate type between silica-poor basalt and silica-rich rhyolite. It is fine-grained (aphanitic) to porphyritic in texture, and is composed predomin ... and andesitic-dacitic lavas. The lower slopes of Mount Tavkvetili are covered by subalpine meadows while the upper slopes are covered by alpine meadows. Natural disasters Mount Tavkvetili has destructive earthquakes around once every 50 years that rank over a 7 on the Richter magnitude scale. References * ''Georgian Sta ...
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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 ...
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Didi Abuli
Didi Abuli ( ka, დიდი აბული; hy, Աբուլ (Abul)) is one of the highest peak of the Lesser Caucasus Mountains in the nation of Georgia. The mountain is located in the 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 ... at an elevation of above sea level. Didi Abuli is an extinct stratovolcano External links * Mountains of Georgia (country) Mountains of Samtskhe-Javakheti region {{Georgia-geo-stub ...
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Paravani
The Paravani ( ka, ფარავანი) is a river of southern Georgia. It is long, and has a drainage basin of .Statistical Yearbook of Georgia: 2020
National Statistics Office of Georgia, Tbilisi, 2020, p. 12. The Paravani is the outflow of . It is a right tributary of the (Mtkvari), which it joins in the village
Khertvisi Khertvisi is a village in Aspindza Municipality of Samtskhe-Javakheti region, the Republic of Georg ...
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