Balkhan Ranges
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Balkhan Ranges
Balkhan Ranges or Balkan Ranges, also Balkhans, Balkans (, Balkan Mountains) are mountains by the eastern shores of the Caspian Sea in the Balkan Region of Turkmenistan. They consist of the Greater Balkan, or Uly Balkan and the Lesser Balkan . They are separated by Uzboy, a dried-out distributary of the Amu Darya The Amu Darya ( ),() also shortened to Amu and historically known as the Oxus ( ), is a major river in Central Asia, which flows through Tajikistan, Turkmenistan, Uzbekistan, and Afghanistan. Rising in the Pamir Mountains, north of the Hindu Ku .... References {{reflist Mountain ranges of Asia Mountains of Turkmenistan ...
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Turkmenistan
Turkmenistan is a landlocked country in Central Asia bordered by Kazakhstan to the northwest, Uzbekistan to the north, east and northeast, Afghanistan to the southeast, Iran to the south and southwest and the Caspian Sea to the west. Ashgabat is the capital and largest city. It is one of the six independent Turkic states. With a population over 7 million, Turkmenistan is the 35th most-populous country in Asia and has the lowest population of the Central Asian republics while being one of the most sparsely populated nations on the Asian continent. Turkmenistan has long served as a thoroughfare for several empires and cultures. Merv is one of the oldest oasis-cities in Central Asia, and was once among the biggest cities in the world. It was also one of the great cities of the Islamic world and an important stop on the Silk Road. Annexed by the Russian Empire in 1881, Turkmenistan figured prominently in the anti-Bolshevik movement in Central Asia. In 1925, Turkmenistan be ...
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Mount Arlan
Mount Arlan () is an peak in the western plains of Turkmenistan in Balkan Province. Mount Arlan stands about 2,000 metres above the shore of the below-sea level Caspian Sea. It is the highest summit of the Uly Balkan range. The town of Balkanabat, the capital of Balkan Province Balkan Region () is the westernmost of the five regions of Turkmenistan. Clockwise from north it borders Kazakhstan, Uzbekistan (north); two provinces of Turkmenistan (east), Iran (south), and the Caspian Sea (west). The capital city is Balkana ..., lies 25 km to the southwest. See also * List of Ultras of Central Asia Notes External links * Balkan Daglary {{Turkmenistan-geo-stub ...
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Caspian Sea
The Caspian Sea is the world's largest inland body of water, described as the List of lakes by area, world's largest lake and usually referred to as a full-fledged sea. An endorheic basin, it lies between Europe and Asia: east of the Caucasus, west of the broad steppe of Central Asia, south of the fertile plains of Southern Russia in Eastern Europe, and north of the mountainous Iranian Plateau. It covers a surface area of (excluding the highly saline lagoon of Garabogazköl to its east), an area approximately equal to that of Japan, with a volume of . It has a salinity of approximately 1.2% (12 g/L), about a third of the salinity of average seawater. It is bounded by Kazakhstan to the northeast, Russia to the northwest, Azerbaijan to the southwest, Iran to the south, and Turkmenistan to the southeast. The name of the Caspian Sea is derived from the ancient Iranian peoples, Iranic Caspians, Caspi people. The sea stretches from north to south, with an average width of . Its gr ...
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Balkan Region
Balkan Region () is the westernmost of the five regions of Turkmenistan. Clockwise from north it borders Kazakhstan, Uzbekistan (north); two provinces of Turkmenistan (east), Iran (south), and the Caspian Sea (west). The capital city is Balkanabat, formerly known as Nebit Dag. The region's boundaries are identical to those of the former ''Krasnovodsk Oblast''', a Soviet-era province of the Turkmen Soviet Socialist Republic with its capital in the city of Krasnovodsk. This oblast was liquidated and restored repeatedly in the 20th century, concluding with its abolition in 1988. However, the administrative boundaries of the region were restored in 1991 when Balkan Region was established with its capital being moved to Nebit Dag which was later renamed Balkanabat. The province covers 139,270 square kilometers and counts 529,895 residents (2022 estimate). A large minority of these are nomadic herding families.''Statistical Yearbook of Turkmenistan 2000-2004'', National Institute o ...
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Uly Balkan
The Uly Balkan (, Greater Balkan Mountains), also the Great Balkhan or Greater Balkhan is a mountain range in Turkmenistan, part of the Balkhan Ranges. The highest summit is Mount Arlan at . References

{{reflist Mountain ranges of Asia Mountain ranges of Turkmenistan ...
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Uzboy
The Uzboy (sometimes spelled Uzboj) was a distributary of the Amu Darya river which flowed through the northwestern part of the Karakum Desert of Turkmenistan until the 17th century, when it abruptly dried up, eliminating the agricultural population that had thrived along its banks. (It was a part of the ancient region of Dahistan). Now a dry river channel and a center for archaeological excavations, the Uzboy flowed some , from a branch in the Amu Darya River via Sarykamysh Lake to the Caspian Sea. A riverine civilization existed along the banks of the river from at least the 5th century BC until the 17th century AD, when the water which had fed the Uzboy abruptly stopped flowing out of the main course of the Amu Darya. The Uzboy dried up, and the tribes which had inhabited the river's banks were abruptly dispersed, the survivors becoming nomadic desert dwellers. In the early 1950s, construction work started to build a major irrigation canal roughly along the river bed of the f ...
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Distributary
A distributary, or a distributary channel is a stream channel that branches off and flows a main stream channel. It is the opposite of a ''tributary'', a stream that flows another stream or river. Distributaries are a result of river bifurcation and are often found where a river approaches a lake or an ocean and divides into distributary networks; as such they are a common feature of river deltas. They can also occur inland, on alluvial fans, or where a tributary stream bifurcates as it nears its confluence with a larger stream. In some cases, a minor distributary can divert so much water from the main channel that it can later become the main route. Related terms Common terms to name individual river distributaries in English-speaking countries are ''arm'' and ''channel''. These terms may refer to a distributary that does not rejoin the channel from which it has branched (e.g., the North, Middle, and South Arms of the Fraser River, or the West Channel of the Mackenzie River ...
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Amu Darya
The Amu Darya ( ),() also shortened to Amu and historically known as the Oxus ( ), is a major river in Central Asia, which flows through Tajikistan, Turkmenistan, Uzbekistan, and Afghanistan. Rising in the Pamir Mountains, north of the Hindu Kush, the Amu Darya is formed by the confluence of the Vakhsh River, Vakhsh and Panj River, Panj rivers, in the Tigrovaya Balka Nature Reserve on the border between Afghanistan and Tajikistan, and flows from there north-westwards into the South Aral Sea, southern remnants of the Aral Sea. In its upper course, the river forms part of Afghanistan's northern border with Tajikistan, Uzbekistan, and Turkmenistan. In ancient history, the river was regarded as the boundary of Greater Iran with Turan, which roughly corresponded to present-day Central Asia.B. SpulerĀmū Daryā in Encyclopædia Iranica, online ed., 2009 The Amu Darya has a flow of about 70 cubic kilometres per year on average. Names In classical antiquity, the river was known as the ...
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Mountain Ranges Of Asia
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and climate, mountains ...
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