Dushanbe vs Valley

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Dushanbe (Tajik: Душанбе, IPA: [duʃæmˈbe]; significance Monday in Persian) is the capital and largest city of Tajikistan. As of January 2020, Dushanbe had a population of 863,400 and as of 2010 that population was largely Tajik. Until 1929, the town was known in Russian as Dyushambe (Russian: Дюшамбе, Dyushambe), and from 1929 to 1961 as Stalinabad (Tajik: Сталинобод, Stalinobod), after Joseph Stalin. Dushanbe is located in the Gissar valley, bounded by the Gissar Range in the north and east and the Babatag, Aktau, Rangontau and Karatau mountains in the south, and has an altitude of 750--900 m. The town is divided into four districts, all named after historical figures: Ismail Samani, Avicenna, Ferdowsi, and Shah Mansur. In ancient times, what is currently or is near modern Dushanbe was settled by different empires and individuals, including Mousterian tool-users, various neolithic cultures, the Achaemenid Empire, Greco-Bactria, the Kushan Empire, and the Hephalites. In the Middle Ages, more settlements started near modern-day Dushanbe such as Hulbuk and its famous palace. In the 17th century to the early 20th, Dushanbe started to grow into a market village controlled at times by the Beg of Hisor, Balkh, and eventually Bukhara. Soon after the Russian invasion in 1922, the city was made the capital of the Tajik Autonomous Soviet Socialist Republic in 1924, which initiated Dushanbe's development and rapid population growth that lasted until the Tajik Civil War. Following the war, the city became capital of an independent Tajikistan and continued its growth and development into a modern city which now is home to many international conventions. Dushanbe's modern culture had its beginnings in the 1920s, where Soviet music, cinema, theatre, sculpture, film, and sports all started.

Music, primarily shashmaqam before the Soviet invasion, took off in the city as a result of Russian influence and local opera houses and symphonies. Tajik figures like Sadriddin Ayni contributed greatly to the development of Dushanbe's literature, which went through many changes during and after the Soviet period. Theater and movie both saw their infancy in the 1930s and were heavily influenced by Soviet tendencies. The design of Dushanbe, once neoclassical, transitioned to a minimalist and eventually modern style. The town is a centre for newspapers, radio stations, and television of the nation, with almost 200 newspapers and over a dozen television studios working in 1999. A lot of Dushanbe's education system dates from Soviet times and has a legacy of state control; even now, the greatest university in Dushanbe, the Tajik National University, is funded by the government. Dushanbe International Airport is the principal airport serving the city. Other forms of transport include the trolleybus system dating from 1955, the small rail system, and the streets that traverse the city. Dushanbe's electricity is primarily hydroelectric, produced from the Nurek Dam, and the aging water system dates from 1932. Tajikistan's health care system is concentrated in Dushanbe, meaning that the major hospitals of the country are in the city. The city constitutes 20 percent of Tajikistan's GDP and has large industrial, financial, retail, and tourism businesses. Parks and main areas of the city include Victory Park, Rudaki Park, the Tajikistan National Museum, the Dushanbe Flagpole, and the Tajikistan National Museum of Antiquities.

Source: Wikipedia

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A valley is an elongated low area often running between hills or mountains which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period of time. Some valleys are formed through erosion by glacial ice. These glaciers may remain present in valleys in high mountain or polar areas. At lower latitudes and latitudes, these glacially-formed valleys may have been created or enlarged during ice ages but now be ice-free and occupied by streams or rivers.

In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In areas of limestone bedrock, dry valleys may also result from drainage taking place underground rather than at the surface. Rift valleys arise principally from earth movements, rather than erosion. Many different types of valley are described by geographers, using terms that may be global in use or else applied only locally.

Source: Wikipedia