Zarafshan Range | |
---|---|
Highest point | |
Peak | Chimtarga Peak |
Elevation | 5,489 m (18,009 ft) |
Coordinates | 39°20′N69°40′E / 39.333°N 69.667°E |
Dimensions | |
Length | 230 mi (370 km)East–West |
Naming | |
Native name | |
Geography | |
Countries | Tajikistan 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.
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]
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]
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.
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]
The Fann Mountains, and, to a lesser extent, the Matcha Mountains are popular among mountaineers and hikers. [10]
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.
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.
Fergana Valley is a valley in Central Asia, lying mostly in eastern Uzbekistan, extending into southern Kyrgyzstan and northern Tajikistan.
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.
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.
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.
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.
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).
The Emirate of Bukhara was a Muslim-Uzbek polity in Central Asia that existed from 1785 to 1920 in what is now Uzbekistan, Tajikistan, Turkmenistan and Kazakhstan. It occupied the land between the Amu Darya and Syr Darya rivers, known formerly as Transoxiana. Its core territory was the fertile land along the lower Zarafshon river, and its urban centres were the ancient cities of Samarqand and the emirate's capital, Bukhara. It was contemporaneous with the Khanate of Khiva to the west, in Khwarazm, and the Khanate of Kokand to the east, in Fergana. In 1920, it ceased to exist with the establishment of the Bukharan People's Soviet Republic.
Sughd Province, also referred to as the Sogdia Region, is one of the four administrative divisions and one of the three provinces that make up Tajikistan. Centered in the historical Sogdiana, it is located in the northwest of the country, with an area of some 25,400 square kilometers and a population of 2,707,300, up from 2,233,550 according to the 2010 census and 1,871,979 in 2000. The capital is Khujand. The Province's ethnic composition in 2010 was 84% Tajik, 14.8% Uzbek, 0.6% Kyrgyz, 0.4% Russian and 0.1% Tatar.
The Yaghnob is a river in Ayni District of Sughd Region, Tajikistan. Together with the Iskander Darya, it forms the Fan Darya, a major left tributary of the Zeravshan.
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.
One of the northern extensions of the Pamir-Alay system, the Turkestan Range stretches for a total length of 340 km from the Alay Mountains on the border of Kyrgyzstan with Tajikistan to the Samarkand oasis in Uzbekistan. It runs in the east–west direction, north of the Zeravshan Range, forming the southern boundary of the Ferghana Valley in Tajikistan and Golodnaya Steppe in Uzbekistan. The highest elevations are in the east, near the border with Kyrgyzstan. The maximum elevation is the Pik Skalisty at 5,621 metres (18,442 ft). Glaciation occurs especially in the east. The southern slopes are bare cliffs and mountain steppe; the northern slopes are covered with forests. A highway through the Shakhristan Pass at 3,378 meters (11,083 ft) connects the capital Dushanbe with Khujand in Northern Tajikistan.
Iskanderkul is a mountain lake of glacial origin in Tajikistan's Sughd Province. It lies at an altitude of 2,195 metres (7,201 ft) on the northern slopes of the Gissar Range in the Fann Mountains. Triangular in shape, it has a surface area of 3.4 square kilometres (1.3 sq mi) and is up to 72 metres (236 ft) deep. Formed by a landslide that blocks the Saratogh river, the outflow of the lake is called the Iskander Darya, which joins the Yaghnob River to form the Fan Darya, a major left tributary of the Zeravshan River.
The Pamir-Alay is a mountain system in Tajikistan, Kyrgyzstan and Uzbekistan, encompassing four main mountain ranges extending west from the Tian Shan Mountains, and located north of the main range of Pamir. They are variously considered part of the Tian Shan, of the Pamir, or a separate mountain system. The term "Pamiro-Alay" is also used to refer to the mountain region encompassing the Pamir, the Pamir-Alay proper and the Tajik Depression.
The Fan Darya is a river located in Ayni District of Sughd Region, Tajikistan. The Fan Darya is 24 kilometres (15 mi) long, and the area of its drainage basin is 3,230 square kilometres (1,250 sq mi). It is a major left tributary of the Zeravshan.
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.
The Tajikistan–Uzbekistan border is an international border between Tajikistan and Uzbekistan. It is 1,312 kilometres (815 mi) in length and runs from the tripoint with Kyrgyzstan to the tripoint with Afghanistan.
Mikhail Stepanovich Andreyev was a Russian-Uzbek and Soviet orientalist, cultural researcher of Central Asia, ethnographer, linguist, and archaeologist. He was initially supervised by Vladimir Nalivkin, and was the teacher of Olga Alexandrovna Sukhareva. He was a corresponding member of the Russian Academy of Sciences.
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.