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Bezengi Wall
Bezengi Wall, Pitsrula ( ka, ბეზენგის კედელი; russian: link=no, Безенгийская стена, also known as the Khalde Wall) is a long mountain range of the Greater Caucasus, in the Svaneti region of Georgia and Kabardino-Balkaria region of Russia. Highest section of the Central Caucasus. The highest point of the Bezengi Wall is high mount Shkhara, the highest peak of Georgia. Notable peaks include Janga (), Katyn-Tau (), Shota Rustaveli Peak (), Gistola (), Lalveri () and Esenin Peak (). Bezengi Wall surrounded by ice cliffs on either side. The geologic makeup of the mountains consists of grey granitoids. Bezengi Glacier lies on the northern slopes of the range and the Khalde Glacier and Shkhara Glacier located on the southern slopes. Avalanches An avalanche is a rapid flow of snow down a slope, such as a hill or mountain. Avalanches can be set off spontaneously, by such factors as increased precipitation or snowpack weakening, or ... [...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] |
Gistola
Gistola ( ka, გისტოლა) is a peak in the central part of the Greater Caucasus Mountain Range on Georgia–Russia border. The elevation of the mountain is above sea level. The mountain is made up of 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 ' ... granites. The slopes of Gistola are covered with ice. See also * Adishi Glacier References Sources * ''Georgian State (Soviet) Encyclopedia.'' 1978. Book 3. p. 172. Mountains of Georgia (country) Svaneti Four-thousanders of the Caucasus {{georgia-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Avalanches
An avalanche is a rapid flow of snow down a slope, such as a hill or mountain. Avalanches can be set off spontaneously, by such factors as increased precipitation or snowpack weakening, or by external means such as humans, animals, and earthquakes. Primarily composed of flowing snow and air, large avalanches have the capability to capture and move ice, rocks, and trees. Avalanches occur in two general forms, or combinations thereof: slab avalanches made of tightly packed snow, triggered by a collapse of an underlying weak snow layer, and loose snow avalanches made of looser snow. After being set off, avalanches usually accelerate rapidly and grow in mass and volume as they capture more snow. If an avalanche moves fast enough, some of the snow may mix with the air, forming a powder snow avalanche. Though they appear to share similarities, avalanches are distinct from slush flows, mudslides, rock slides, and serac collapses. They are also different from large scale movements ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shkhara Glacier
Shkhara ( ka, შხარა) is the highest point in the nation of Georgia It is located near the Russian-Georgian border, in Russia's Kabardino-Balkaria region on the northern side, and the Svaneti region of Georgia in the south. Shkhara lies north of the city of Kutaisi, Georgia's second-largest city, and closer to the townlet of Mestia in Svaneti. The summit lies in the central part of the Greater Caucasus Mountain Range, to the south-east of Mount Elbrus, Europe's highest mountain. Shkhara is the third-highest peak in the Caucasus, just behind Dykh-Tau. Morphology Shkhara is the high point and the eastern anchor of a massif known as the Bezingi (or Bezengi) Wall, a ridge. It is a large, steep peak in a heavily glaciated region, and presents serious challenges to mountaineers. Its north face (on the Russian side) is high and contains several classic difficult routes. The significant sub-summit Shkhara West, at , is a climbing objective in its own right, and a traverse ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Khalde Glacier
Khaldah ( ar, خلدة) is a coastal town located south of Beirut, Lebanon. It is famous as a tourist destination in the summer, especially for its various beach resorts. The southern portion of Beirut–Rafic Hariri International Airport is located in Khaldah, in addition to a Lebanese Air Force base. Also, the motorway connecting Beirut and Southern Lebanon passes through Khaldah. The town itself lacks any form of urban planning, and in the past few years, most of the green areas have been replaced by commercial and apartment buildings. Some vegetables and citrus trees can still be seen growing in smaller and dispersed areas. As for industries, there are aluminum and glass factories in this area. Schools and universities Besides commerce and industries, Khaldah also houses educational institutions such as one University and two Schools. History Archeological excavations, now covered over, evidence that the site has been occupied since at least the beginning of the first millenn ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bezengi Glacier
The Bezengi Glacier ( krc, Uluchiran) is a vast valley-type glacier in the Republic of Kabardino-Balkaria, Russia, near the northern slope of the Main Caucasian Range of the Caucasus. Klok, E. J., and J. Oerlemans. ''Climate Reconstructions Derived from Global Glacier Length Records.'' Arctic, Antarctic, and Alpine Research, vol. 36, no. 4, 2004, pp. 575–583. JSTOR, www.jstor.org/stable/1552311. Accessed 28 Sept. 2020. Morphology The Bezengi Glacier runs from the peaks of Shkhara and Janga until it drops to height 2000 m. Glacier area 36 km, length 17.6 km, tongue about 9 km. Much of the tongue of the mare is covered with moraines and fragments. The Bezengi Glacier is a source of the river Cherek. See also * List of glaciers in Russia This is a list of glaciers in Russia. It includes glaciers, ice caps and ice domes located in the Russian Federation. List of glaciers and ice caps Ice caps * Academy of Sciences Glacier () – Severnaya Zemlya. Largest si ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Granitoids
A granitoid is a generic term for a diverse category of coarse-grained igneous rocks that consist predominantly of quartz, plagioclase, and alkali feldspar. Granitoids range from plagioclase-rich tonalites to alkali-rich syenites and from quartz-poor monzonites to quartz-rich quartzolites. As only two of the three defining mineral groups (quartz, plagioclase, and alkali feldspar) need to be present for the rock to be called a granitoid, foid-bearing rocks, which predominantly contain feldspars but no quartz, are also granitoids. The terms ''granite'' and ''granitic rock'' are often used interchangeably for granitoids; however, granite is just one particular type of granitoid. Granitoids are diverse; no classification system for granitoids can give a complete and unique characterization of the origin, compositional evolution, and geodynamic environment for the genesis of a granitoid. Accordingly, multiple granitoid classification systems have been developed such as those based on ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Levan Maruashvili
Levan Iosifovich Maruashvili ( ka, ლევან იოსების ძე მარუაშვილი; born 25 October 1912, Novocherkassk, Russian Empire, – 5 December 1992, Tbilisi, Georgia) was a prominent Georgian geographer. Doctor of Geographical Sciences (1954), professor (1965).Encyclopedia TBILISI Was edited by I. Abashidze Chief Editorial Board of Georgian Encyclopedia in 2002. Honored Scientist of the Georgian SSR (1966) and Abkhaz ASSR. Honorary member of the (1985). He introduced a new concept of Karstosphere ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Esenin Peak
Sergei Alexandrovich Yesenin ( rus, Сергей Александрович Есенин, p=sʲɪrˈɡʲej ɐlʲɪkˈsandrəvʲɪtɕ jɪˈsʲenʲɪn; ( 1895 – 28 December 1925), sometimes spelled as Esenin, was a Russian lyric poet. He is one of the most popular and well-known Russian poets of the 20th century, known for "his lyrical evocations of and nostalgia for the village life of his childhoodno idyll, presented in all its rawness, with an implied curse on urbanisation and industrialisation." Biography Early life Sergei Yesenin was born in Konstantinovo in Ryazan Governorate of the Russian Empire to a peasant family. His father was Alexander Nikitich Yesenin (1873–1931), his mother's name was Tatyana Fyodorovna (nee Titova, 1875–1955). [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
