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Sarez Lake
Sarez Lake (russian: Сарезское озеро; tg, Сарез кӯл, Sarez Kūl) is a lake in Rushon District of Gorno-Badakhshan province, Tajikistan. Length about , depth few hundred meters, water surface elevation about above sea level and volume of water is more than . The mountains around rise more than above the lake level. The lake formed in 1911, after a great earthquake, when the Murghab River (Tajikistan), Murghab River was blocked by a big landslide. Scientists believe that the landslide dam formed by the earthquake, known as the Usoi Dam, is unstable given local seismicity, and that the terrain below the lake is in danger of catastrophic flood if the dam were to fail during a future earthquake. The Usoi Dam wall survived a localised 7.2 magnitude earthquake, the 2015 Tajikistan earthquake, on the 7th December 2015 with no visible signs of deterioration. Shadau Lake is a small water body southwest of the Usoi Dam and west of Sarez Lake. Formation The format ...
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Usoi Dam
The Usoi Dam is a natural landslide dam along the Murghab River (Tajikistan), Murghab River in Tajikistan. At high, it is the tallest dam in the world, either natural or man-made. The dam was created on February 18, 1911, when the 7.4-Surface wave magnitude, Ms 1911 Sarez earthquake, Sarez earthquake caused a massive landslide that blocked the flow of the river. The dam is formed of approximately of rock dislodged from the steeply sloped river valley of the Murghab River, Murghab, which cuts from east to west through the high and rough Pamir Mountains. It is named after the village of Usoi, which was completely buried by the 1911 landslide. The dam rises to a height of from the original valley floor. The basin formed by Usoi Dam now holds Sarez Lake, a -long lake holding of water. Water does not flow over the top of the dam, which would quickly cause it to erode away; instead, water seeps out of the base of the dam at a rate which approximately matches the rate of inflow, mai ...
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1911 Sarez Earthquake
A notable ongoing event was the race for the South Pole. Events January * January 1 – A decade after federation, the Northern Territory and the Australian Capital Territory are added to the Commonwealth of Australia. * January 3 ** 1911 Kebin earthquake: An earthquake of 7.7 moment magnitude strikes near Almaty in Russian Turkestan, killing 450 or more people. ** Siege of Sidney Street in London: Two Latvian anarchists die, after a seven-hour siege against a combined police and military force. Home Secretary Winston Churchill arrives to oversee events. * January 5 – Egypt's Zamalek SC is founded as a general sports and Association football club by Belgian lawyer George Merzbach as Qasr El Nile Club. * January 14 – Roald Amundsen's South Pole expedition makes landfall, on the eastern edge of the Ross Ice Shelf. * January 18 – Eugene B. Ely lands on the deck of the USS ''Pennsylvania'' stationed in San Francisco harbo ...
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Gorno-Badakhshan Autonomous Region
Gorno-Badakhshan, officially the Badakhshan Mountainous Autonomous Region,, abbr. / is an autonomous region in eastern Tajikistan, in the Pamir Mountains. It makes up nearly forty-five percent of the country's land area, but only two percent of its population.''Population of the Republic of Tajikistan as of 1 January 2008'', State Statistical Committee, Dushanbe, 2008 Name The official English name of the autonomous region is the Badakhshan Mountainous Autonomous Region. The name "Badakhshan" (russian: Бадахшан, Badakhshan; tg, Бадахшон, Badaxşon) is derived from the Sasanian title or . "Gorno-Badakhshan" literally means "mountainous Badakhshan" and is derived from the Russian name of the autonomous region, . The Russian abbreviation "GBAO" is also commonly used in English-language publications by national and international bodies such as the government of Tajikistan and the United Nations. History Prior to 1895, several semi-self governing statelet ...
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Lakes Of Tajikistan
A lake is an area filled with water, localized in a basin, surrounded by land, and distinct from any river or other outlet that serves to feed or drain the lake. Lakes lie on land and are not part of the ocean, although, like the much larger oceans, they do form part of the Earth's water cycle. Lakes are distinct from lagoons, which are generally coastal parts of the ocean. Lakes are typically larger and deeper than ponds, which also lie on land, though there are no official or scientific definitions. Lakes can be contrasted with rivers or streams, which usually flow in a channel on land. Most lakes are fed and drained by rivers and streams. Natural lakes are generally found in mountainous areas, rift zones, and areas with ongoing glaciation. Other lakes are found in endorheic basins or along the courses of mature rivers, where a river channel has widened into a basin. Some parts of the world have many lakes formed by the chaotic drainage patterns left over from the last ice ...
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Khorog
Khorugh ( tg, Хоруғ, ; russian: Хорог, translit=Khorog; ) is the capital of the Gorno-Badakhshan Autonomous Region (GBAO) in Tajikistan. It is also the capital of the Shughnon District of Gorno-Badakhshan. It has a population of 30,500 (2020 ). Khorugh is above sea level in the Pamir Mountains (ancient Mount Imeon) at the confluence of the rivers Ghunt and Panj. The city is bounded to the south (Nivodak) and to the north (Tem) by the deltas of the Shakhdara and Ghunt, respectively. The two rivers merge in the eastern part of the city flow through the city, dividing it almost evenly until its delta in the Panj, on the border with Afghanistan. Khorugh is known for its poplar trees that dominate the flora of the city. History Until the late 19th century, Khorugh was in an area disputed between the Emir of Bukhara, Shah of Afghanistan, Russia and Britain. The Russians emerged the winners of the region after The Great Game, which fixed the current northern border of A ...
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Murghab, Tajikistan
Murghob ( tg, Мурғоб) or Murghab (russian: Мургаб, from the Persian word ''margh-ab'', meaning 'prairie river') is the capital of Murghob District in the Pamir Mountains of Gorno-Badakhshan, Tajikistan. With a population of just under 7,500, Murghob is the only significant town in the eastern half of Gorno-Badakhshan. It is the highest town in Tajikistan (and of the former Soviet Union) at 3,650 meters above sea level. It is where the Pamir Highway crosses the Bartang river.Jamoat-level basic indicators
United Nations Development Programme in Tajikistan, accessed 5 October 2020
The goes north to
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Old Style
Old Style (O.S.) and New Style (N.S.) indicate dating systems before and after a calendar change, respectively. Usually, this is the change from the Julian calendar to the Gregorian calendar as enacted in various European countries between 1582 and 1923. In England, Wales, Ireland and Britain's American colonies, there were two calendar changes, both in 1752. The first adjusted the start of a new year from Lady Day (25 March) to 1 January (which Scotland had done from 1600), while the second discarded the Julian calendar in favour of the Gregorian calendar, removing 11 days from the September 1752 calendar to do so.Spathaky, MikOld Style and New Style Dates and the change to the Gregorian Calendar "Before 1752, parish registers, in addition to a new year heading after 24th March showing, for example '1733', had another heading at the end of the following December indicating '1733/4'. This showed where the Historical Year 1734 started even though the Civil Year 1733 continued u ...
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2015 Tajikistan Earthquake
On December 7, 2015, an earthquake measuring 7.2 on the moment magnitude scale struck Tajikistan west of Murghab at 07:50 UTC at a depth of . The earthquake was also felt in neighboring Xinjiang in China, India, Afghanistan, Pakistan and Kyrgyzstan. The earthquake was felt with intensities of MMI IV in Islamabad, Pakistan, MMI IV in New Delhi, India, MMI IV in Kashgar, China, MMI II in Dushanbe, Tajikistan, MMI II in Kabul, Afghanistan, MMI III in Tashkent, Uzbekistan, MMI III in Bishkek, Kyrgyzstan, and MMI II in Almaty, Kazakhstan. A truck driver and a policeman were killed while dozens more were injured and 500 homes destroyed. The epicentre of this quake was approximately distant from the epicentre of the M7.3 1911 Sarez earthquake which formed the Usoi Dam across the Murghab river. Tectonic setting The eastern part of Tajikistan (the Pamir Mountains) lies within the complex zone of collision between the Indian Plate and the Eurasian Plate. The dominant structures in thi ...
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Murghab River (Tajikistan)
The Bartang (Russian and Tajik: Бартанг) is a river of Central Asia, tributary to the Panj and consequently to the Amu Darya. In its upper reaches, it is also known as the Murghab and Aksu; it flows through the Wakhan in Afghanistan, then through the Rushon District of the Gorno-Badakhshan autonomous region, Tajikistan. The river is long (133 km excluding Aksu and Murghab) and has a basin area of .Бартанг


Course

The river rises in Chaqmaqtin Lake in the



Seismicity
Seismicity is a measure encompassing earthquake occurrences, mechanisms, and magnitude at a given geographical location. As such, it summarizes a region's seismic activity. The term was coined by Beno Gutenberg and Charles Francis Richter in 1941. Seismicity is studied by geophysicists. Calculation of seismicity Seismicity is quantitatively computed. Generally, the region under study is divided in equally sized areas defined by latitude and longitude, and the Earth's interior is divided into various depth intervals on account of Earth's layering: Up to depth, , and > . The usual formula to calculate seismicity is: S = \frac where : _i: is the energy of a single seismic event (i.e., earthquake); : _0: interval of latitude; : _0: interval of longitude : _0: interval of the hypocenter; : _0: interval of the time of the seismic event. : The result is seismicity as energy per cubic unit. See also * Moment magnitude scale * Plate tectonics * Seismology * Wadati–Benioff zo ...
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Landslide Dam
A landslide dam or barrier lake is the natural damming of a river by some kind of landslide, such as a debris flow, rock avalanche or volcanic eruption. If the damming landslide is caused by an earthquake, it may also be called a quake lake. Some landslide dams are as high as the largest existing artificial dam.Robert B. Jansen (1988) "Advanced Dam Engineering for Design, Construction, and Rehabilitation", Causes The major causes for landslide dams investigated by 1986 are landslides from excessive precipitation and earthquakes, which account for 84%. Volcanic eruptions account for a further 7% of dams. Other causes of landslides account for the remaining 9%. Consequences The water impounded by a landslide dam may create a dam reservoir (lake) that may last for a short time, to several thousand years. Because of their rather loose nature and absence of controlled spillway, landslide dams frequently fail catastrophically and lead to downstream flooding, often with high casualti ...
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