Zarafshan Range

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Zarafshan Range
Anzob mountains.jpg
Part of the Zarafshan Range seen from Anzob Pass
Highest point
PeakChimtarga Peak
Elevation 5,489 m (18,009 ft)
Coordinates 39°20′N69°40′E / 39.333°N 69.667°E / 39.333; 69.667
Dimensions
Length230 mi (370 km)East–West
Naming
Native name
  • Қаторкӯҳҳои Зарафшон (Tajik)
  • Зеравшанский хребет (Russian)
  • Zarafshon (Uzbek)
Geography
Tajikistan relief map.svg
Red triangle with thick white border.svg
Location in Tajikistan
CountriesTajikistan and Uzbekistan
Parent range Pamir-Alay

The Zarafshan Range, [lower-alpha 1] formerly the Zeravshan Range, [lower-alpha 2] is a mountain range in Tajikistan and Uzbekistan, part of the Pamir-Alay mountains. [1] Almost all of the range belongs to the drainage basins of the Zarafshan River.

Contents

The Persian name is believed to possibly be a reference to gold found in bed of the Zarafshan River and its tributaries, which has ushered prosperity to the region from ancient times. [2]

Geography and geology

The Zarafshan River Ayni zarafshon river.jpg
The Zarafshan River
View from the Takhta-Karacha Pass on the M39 between Samarkand and Shahrisabz. View from Takhta-Karacha Pass 1.jpg
View from the Takhta-Karacha Pass on the M39 between Samarkand and Shahrisabz.

The range extends over 370 kilometres (230 mi) in an east−west direction along the south of Sughd Region in Tajikistan, reaching the highest point of 5,489 metres (18,009 ft) (Chimtarga Peak) in its central part. South-west of Panjakent the range crosses from Tajikistan into Uzbekistan, where it continues at decreasing elevations (1,500–2,000 metres (4,900–6,600 ft)) along the internal border between Samarkand and Kashkadarya Regions provinces, until it blends into the desert south-west of Samarkand. [3]

There are two other mountain ranges running in an east−west direction parallel to the Zarafshan Range. To the north, the Zeravshan Valley runs east for approximately 250 kilometres (160 mi) from Samarkand and separates the Zarafshan Range from the Turkestan Range. [4] To the south, the Hisar range runs parallel to the Zarafshan Range. [1] To the west of Lake Iskanderkul, the Zarafshan Range and the Gissar Range are connected by the Fann Mountains, which is the highest part of both ranges.

The Zarafshan Range is crossed in the meridional direction by three rivers: the Fan Darya, the Kashtutu Darya, and the Maghian Darrya, all of which flow north and are left tributaries of the Zarafshan. The part of the Zarafshan Range east of the Fan Darya is known as the Matcha Range. It has heights around 5 kilometres (16,000 ft) and in the east, it is connected to the Alay Range and the Turkestan Range. This point (the Matcha Mountains) is the location of the Zarafshan Glacier, which is 24.75 kilometres (15.38 mi) long and is one of the longest glaciers of the Central Asia. The northern slopes of the Matcha Range are relatively smooth and descend to the Zarafshan, whereas the southern slopes sharply drop to the valley of the Yaghnob River. [5] [6] [7]

The highest part of the range is located between the Fan Darya and the Kashtutu Darya and includes the Fann Mountains. The western part of the range is up to 3 kilometres (9,800 ft) and is forested. [5] The southern slopes of the western part of the ridge belong to the drainage basin of the Kashka Darya, which rises in the range's southern watershed. [1] The river terminates between Panjakent and Lake Karakul. Water is precious in the region and is utilized for irrigation − an irrigation system that has developed involves 85 main canal totalling a length of 2,530 kilometres (1,570 mi). [8]

There are several passes crossing the range, including Akhba-Tavastfin, Akhba-Bevut, Akhba-Guzun, Akhba-Surkltat, Darkh Pass, Minora, and Marda-Kishtigeh. [6] Various elevations include 3,550 metres (11,650 ft) at Kshtut Pass, 5,600 metres (18,400 ft) at Mount Chandara, and 4,600 metres (15,100 ft) at Mount Hazret Sultan. [6] Fan Darya makes a gorge going across the ridge. The road connecting Dushanbe and Khujand is built in the ridge.

The geological formations in the mountains of the upper Zarafshan Valley contain minerals such as coal, iron, gold alum and sulphur. Gold is reported from the entire course of the Fan Darya, Kashtutu Darya, and Maghian Darya. [6]

History

The slopes of the range have been populated since antiquity. Prehistoric Siypantosh Rock Paintings are preserved in the Uzbek portion of the range. In about 400 BC, they belonged to the Iranian civilization of Sogdiana. In 330 BC, during the Asian Campaign, troops of Alexander the Great reached the Zarafshan Valley. The name of Lake Iskanderkul clearly originates from the name of Alexander - Iskander; however, attempts to place a connection between the lake and the campaign only exist at the level of legend. [9] Together with the rest of Western Tajikistan, the Zarafshan Range has changed hands several times, being part of the Hephthalite Empire, the Umayyad Caliphate, and the Samanid Empire. In the 13th century, it was taken over by the Mongols, and in the 16th century, became part of the Khanate of Bukhara. The Zarafshan, Yaghnob, and Fan Darya valleys were essentially controlled by local authorities (beks). The fortress of Sarvoda was built to protect the gorge of the Fan Darya. [10]

In 1862, the Russian Empire started to penetrate to Central Asia. By 1870, Russian troops occupied both the Zarafshan and the Yaghnob valleys, with the last operation being the Iskanderkul Expedition in the spring of 1870, under the command of the Major General Alexander Abramov. During the expedition, Russian troops took the Yaghnob Valley under control. After 1870, military topographers started to map the mountains, including the Zarafshan Range. [10] In 1870, Alexey Fedchenko lead an expedition to the Zarafshan Valley, and in 1880, Ivan Mushketov discovered the Zarafshan Glacier and investigated the upper part of the valley. In 1892, Vladimir Komarov investigated the Yaghnob valley. [11]

In 1868, Zarafshan Okrug was split from the Emirate of Bukhara. The Okrug was controlled by Russian authorities, but the authority at the local level remained with the beks. The whole Zarafshan Range was inside the okrug. On January 1, 1887 Samarkand Oblast was established, with the administrative center in Samarkand. In 1924, Samarkand Oblast was abolished and split between newly established Uzbek Soviet Socialist Republic and Tajik Autonomous Soviet Socialist Republic, corresponding to the contemporary division between Uzbekistan and Tajikistan.

Population

All valleys of the range are populated. There are no towns in the range; the closest towns are Panjakent and Samarkand. A major road between Dushanbe and Khujand crosses the range; another road to Samarkand follows the Zarafshan River. The roads into secondary valleys, including the Yaghnob valley, are mostly unpaved and poorly maintained.

Most of the population of the range are Tajiks. The population of the Yaghnob Valley are the Yaghnobi. [10]

Tourism

The Fann Mountains, and, to a lesser extent, the Matcha Mountains are popular among mountaineers and hikers. [10]

See also

Notes

Related Research Articles

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Tajikistan harkens to the Samanid Empire (819–999). The Tajik people came under Russian rule in the 1860s. The Basmachi revolt broke out in the wake of the Russian Revolution of 1917 and was quelled in the early 1920s during the Russian Civil War. In 1924, Tajikistan became an Autonomous Soviet Socialist Republic of the Soviet Union, the Tajik ASSR, within Uzbekistan. In 1929, Tajikistan was made one of the component republics of the Soviet Union – Tajik Soviet Socialist Republic – and it kept that status until gaining independence 1991 after the dissolution of the Soviet Union.

<span class="mw-page-title-main">Geography of Tajikistan</span>

Tajikistan is nestled between Kyrgyzstan and Uzbekistan to the north and west, China to the east, and Afghanistan to the south. Mountains cover 93 percent of Tajikistan's surface area. The two principal ranges, the Pamir Mountains and the Alay Mountains, give rise to many glacier-fed streams and rivers, which have been used to irrigate farmlands since ancient times. Central Asia's other major mountain range, the Tian Shan, skirts northern Tajikistan. Mountainous terrain separates Tajikistan's two population centers, which are in the lowlands of the southern and northern sections of the country. Especially in areas of intensive agricultural and industrial activity, the Soviet Union's natural resource utilization policies left independent Tajikistan with a legacy of environmental problems.

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<span class="mw-page-title-main">Uzbek Soviet Socialist Republic</span> Constituent Republic of the Soviet Union

The Uzbek Soviet Socialist Republic, also known as Soviet Uzbekistan, the Uzbek SSR, UzSSR, or simply Uzbekistan and rarely Uzbekia or Red Uzbekistan, was a union republic of the Soviet Union. It was governed by the Uzbek branch of the Soviet Communist Party, the legal political party, from 1925 until 1990. From 1990 to 1991, it was a sovereign part of the Soviet Union with its own legislation.

<span class="mw-page-title-main">Fann Mountains</span> Mountains in Tajikistan

The Fann Mountains are part of the western Pamir-Alay mountain system in Tajikistan's Sughd Province, between the Zarafshan Range to the north and the Gissar Range to the south. In an east-west direction, they extend from the Fan Darya to the Archimaydan River.

<span class="mw-page-title-main">Khujand</span> City in northwestern Tajikistan

Khujand, sometimes spelled Khodjent and formerly known as Leninabad from 1936 to 1991, is the second-largest city of Tajikistan and the capital of Tajikistan's northernmost Sughd province.

<span class="mw-page-title-main">Russian Turkestan</span> 1867–1917 governorate-general of the Russian Empire

Russian Turkestan was the western part of Turkestan within the Russian Empire’s Central Asian territories, and was administered as a Krai or Governor-Generalship. It comprised the oasis region to the south of the Kazakh Steppe, but not the protectorates of the Emirate of Bukhara and the Khanate of Khiva. It was populated by speakers of Russian, Uzbek, Kazakh, Kyrgyz, and Tajik.

<span class="mw-page-title-main">Zarafshon (river)</span> River in Tajikistan, Uzbekistan

The Zarafshon is a river in Tajikistan and Uzbekistan in Central Asia. Its name, "spreader of gold" in Persian, refers to the presence of gold-bearing sands in the upper reaches of the river. To the ancient Greeks it was known as the Polytimetus. It was also formerly known as Sughd River. The river is 877 kilometres (545 mi) long and has a basin area of 17,700 square kilometres (6,800 sq mi).

<span class="mw-page-title-main">Emirate of Bukhara</span> 1785–1920 state in Central Asia

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<span class="mw-page-title-main">Sughd Region</span> Region of Tajikistan

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<span class="mw-page-title-main">Yaghnob (river)</span> River in northwestern Tajikistan

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Jangal is a village in north-west Tajikistan, part of the city of Panjakent in Sughd Region. It is a western suburb of Panjakent, located on the river Zeravshan on the border with Uzbekistan. It lies on the road from Panjakent to Samarkand.

<span class="mw-page-title-main">Turkestan Range</span> Mountain range mostly in western Tajikistan

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<span class="mw-page-title-main">Iskanderkul</span> Glacial lake in Gissar Range, Fann Mountains

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<span class="mw-page-title-main">Pamir-Alay</span> Mountain system mostly in Tajikistan and Kyrgyzstan

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<span class="mw-page-title-main">Iskander Darya</span> River in Tajikistan

The Iskander Darya is a river in Ayni District of Sughd Region, Tajikistan. The Iskander Darya is 20 kilometres (12 mi) long, and the area of its drainage basin is 950 square kilometres (370 sq mi) long. It is the left source river of the Fan Darya.

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<span class="mw-page-title-main">Zarafshan Bridge</span> Bridge in Uzbekistan

Zarafshan Bridge is an architectural monument located 7–8 km northeast of Samarkand on the left bank of the Zarafshan River. The bridge was built in the year 1502 by the order of Muhammad Shaybani. It served as a water divider on the Zarafshan River, giving rise to two branches—Akdarya and Karadarya.

References

  1. 1 2 3 4 Soucek, Svat (17 February 2000). A History of Inner Asia . Cambridge University Press. pp.  4–. ISBN   978-0-521-65704-4.
  2. Henry Lansdell (1885). Russian Central Asia: Including Kuldja, Bokhara, Khiva and Merv. Sampson Low, Marston, Searle and Rivington. pp.  534–.
  3. Atlas of the Soviet Republics of Central Asia (in Russian), Moscow (1988).
  4. Murcott, Susan (1 November 2012). Arsenic Contamination in the World: An International Sourcebook 2012. IWA Publishing. pp. 164–. ISBN   978-1-78040-038-9.
  5. 1 2 Гиссаро-Алай (in Russian). A.S.T. Company. Retrieved 27 May 2013.
  6. 1 2 3 4 Royal Geographical Society (Great Britain) (1886). Supplementary Papers (Public domain ed.). J. Murray. pp. 213–.
  7. Eugene Schuyler; Vasilīĭ Vasilʹevich Grigorʹev (1877). Turkistan: Notes of a Journey in Russian Turkistan, Khokand, Bukhara, and Kuldja. Scribner, Armstrong & Company. pp.  275–.
  8. Eugene Schuyler (1966). Turkistan. Taylor & Francis. pp. 145–. ISBN   9780710050533.
  9. Искандеркуль (in Russian). Tajikistan Development Gateway Team. Retrieved 28 May 2013.
  10. 1 2 3 4 Пагануцци, Н. В. (1968). Фанские горы и Ягноб (in Russian). Moscow: Fizkultura i sport.
  11. Гвоздецкий, Н. А. (1953). Владимир Леонтьевич Комаров (in Russian). Moscow: Geografgiz.