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Jetisu
Jetisu (Kazakh: Жетісу, IPA: [(d)ʑetʰɪ̥sʊ́w]), also known as Semirechye (Russian: Семиречье, IPA: [sʲɪmʲɪˈrʲetɕje]) and Heptopotamia, is a historical region in Central Asia corresponding to the southeastern part of modern Kazakhstan.
Jetisu is also transcribed Jeti-Suu (Kyrgyz: Жети-Суу, romanized: Jeti-Suu, pronounced [dʑetɪˈsuː]), Zhetisu, Jetisuw, Jetysu, Jeti-su or Jity-su,
The name comes from "seven rivers" in Kazakh but meant "abounding in water", in contrast to the dry steppes of the eastern Balkhash area. It owes its name to the rivers that flow from the southeast into Lake Balkhash. Jetisu primarily falls into today's Jetisu Region and Almaty Region and other South-Eastern parts of Kazakhstan and some parts of Northern Kyrgyzstan.
The lands of the 19th-century Semirechye Oblast included the steppes south of Lake Balkhash and parts of the Tian Shan Mountains around Lake Issyk Kul. The province had an area of 147,300 km², and was bounded by the province of Semipalatinsk on the north, by China (Xinjiang) on the east and south, and by the former Russian provinces of Fergana, Syr-darya, and Akmolinsk on the west.
The Dzungarian Alatau Mountains, which separated it from the Chinese region of Kulja, extend south-west towards the river Ili, with an average height of 2,700 m (9,000 ft) above the sea, several isolated snow-clad peaks reaching 3,400 to 4,300 m (11,000 to 14,000 ft). In the south, the region embraces the intricate systems of the Ala-Tau and the Tian Shan. Two ranges of the former, the Trans-Ili Ala-tau and the Terskey Ala-tau, stretch along the north shore of Lake Issyk Kul, both ranging from 3,000 to 4,600 m (10,000 to 15,000 ft) and both partially snow-clad. South of the lake, two ranges of the Tian Shan, separated by the valley of the Naryn, stretch in the same direction, lifting up their icy peaks to 1,800 and 2,400 m (6,000 and 8,000 ft); while westwards from the lake the precipitous slopes of the Alexander chain, 2,700 to 3,000 m (9,000 to 10,000 ft) high, with peaks rising 900 to 1,200 m (3,000 to 4,000 ft) higher, extend into the former province of Syr-darya (containing the southern Kazakh cities of Chimkent, Auliye-ata and Turkestan). Another mountain complex of much lower elevation runs north-westwards from the Trans-Ili Ala-tau towards the southern extremity of Lake Balkhash. In the north, where the province bordered Semipalatinsk, it included the western parts of the Tarbagatai range, the summits of which (3,000 m or 10,000 ft) do not reach the limit of perpetual snow. The remainder of the province consisted of a fertile steppe in the north-east (Sergiopol), and vast uninhabitable sand-steppes on the south of Lake Balkhash. Southwards from these at the foot of the mountains and at the entrance to the valleys, there are rich areas of fertile land.
The climate in Jetisu is thoroughly continental. In the Balkhash steppes the winter is very cold. The lake freezes every year, with temperatures falling to −11 °C (13 °F). In the Ala-kul steppes the winds blow away the snow. The passage from winter to spring is very abrupt, and the steppes are rapidly clothed with vegetation, which, however, is soon scorched by the sun. Average temperatures at Almaty (733 m, 2,405 ft high) are: for the year 8 °C (46 °F), for January −8 °C (17 °F), for July 23 °C (74 °F). At Przhevalsk (1,660 m, 5,450 ft): for the year 2.5 °C (36.5 °F), for January −5 °C (23 °F), for July 17 °C (63 °F); still higher in the mountains, at Naryn (2,100 m, 6,900 ft), the average temperature for the year is only 6.5 °C (43.7 °F), for January −17 °C (1.4 °F), for July 18 °C (64.4 °F).
The most important river is the Ili, which enters Jetisu from the Tian Shan mountains of China's Ili Kazakh Autonomous Prefecture in northern Xinjiang, and drains it for 250 km before it enters Lake Balkhash. The Chu River also rises in the Tian Shan mountains and flows north-westwards through the former Akmolinsk province of the Governor-Generalship of the Steppes. The Naryn River flows south-westwards along a longitudinal valley of the Tian Shan, and enters the Fergana Valley to join the Syr Darya. The major lakes of the area include Lake Balkhas (or Denghiz) and Lake Ala Kul, which was connected with Balkash in the post-Pliocene period but now stands some hundred feet higher, connected by a chain of smaller lakes with Sissyk Kul, Lake Issyk-Kul, and the alpine lakes of Son-Kul and Chatyr-Kul.
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Jetisu
Jetisu (Kazakh: Жетісу, IPA: [(d)ʑetʰɪ̥sʊ́w]), also known as Semirechye (Russian: Семиречье, IPA: [sʲɪmʲɪˈrʲetɕje]) and Heptopotamia, is a historical region in Central Asia corresponding to the southeastern part of modern Kazakhstan.
Jetisu is also transcribed Jeti-Suu (Kyrgyz: Жети-Суу, romanized: Jeti-Suu, pronounced [dʑetɪˈsuː]), Zhetisu, Jetisuw, Jetysu, Jeti-su or Jity-su,
The name comes from "seven rivers" in Kazakh but meant "abounding in water", in contrast to the dry steppes of the eastern Balkhash area. It owes its name to the rivers that flow from the southeast into Lake Balkhash. Jetisu primarily falls into today's Jetisu Region and Almaty Region and other South-Eastern parts of Kazakhstan and some parts of Northern Kyrgyzstan.
The lands of the 19th-century Semirechye Oblast included the steppes south of Lake Balkhash and parts of the Tian Shan Mountains around Lake Issyk Kul. The province had an area of 147,300 km², and was bounded by the province of Semipalatinsk on the north, by China (Xinjiang) on the east and south, and by the former Russian provinces of Fergana, Syr-darya, and Akmolinsk on the west.
The Dzungarian Alatau Mountains, which separated it from the Chinese region of Kulja, extend south-west towards the river Ili, with an average height of 2,700 m (9,000 ft) above the sea, several isolated snow-clad peaks reaching 3,400 to 4,300 m (11,000 to 14,000 ft). In the south, the region embraces the intricate systems of the Ala-Tau and the Tian Shan. Two ranges of the former, the Trans-Ili Ala-tau and the Terskey Ala-tau, stretch along the north shore of Lake Issyk Kul, both ranging from 3,000 to 4,600 m (10,000 to 15,000 ft) and both partially snow-clad. South of the lake, two ranges of the Tian Shan, separated by the valley of the Naryn, stretch in the same direction, lifting up their icy peaks to 1,800 and 2,400 m (6,000 and 8,000 ft); while westwards from the lake the precipitous slopes of the Alexander chain, 2,700 to 3,000 m (9,000 to 10,000 ft) high, with peaks rising 900 to 1,200 m (3,000 to 4,000 ft) higher, extend into the former province of Syr-darya (containing the southern Kazakh cities of Chimkent, Auliye-ata and Turkestan). Another mountain complex of much lower elevation runs north-westwards from the Trans-Ili Ala-tau towards the southern extremity of Lake Balkhash. In the north, where the province bordered Semipalatinsk, it included the western parts of the Tarbagatai range, the summits of which (3,000 m or 10,000 ft) do not reach the limit of perpetual snow. The remainder of the province consisted of a fertile steppe in the north-east (Sergiopol), and vast uninhabitable sand-steppes on the south of Lake Balkhash. Southwards from these at the foot of the mountains and at the entrance to the valleys, there are rich areas of fertile land.
The climate in Jetisu is thoroughly continental. In the Balkhash steppes the winter is very cold. The lake freezes every year, with temperatures falling to −11 °C (13 °F). In the Ala-kul steppes the winds blow away the snow. The passage from winter to spring is very abrupt, and the steppes are rapidly clothed with vegetation, which, however, is soon scorched by the sun. Average temperatures at Almaty (733 m, 2,405 ft high) are: for the year 8 °C (46 °F), for January −8 °C (17 °F), for July 23 °C (74 °F). At Przhevalsk (1,660 m, 5,450 ft): for the year 2.5 °C (36.5 °F), for January −5 °C (23 °F), for July 17 °C (63 °F); still higher in the mountains, at Naryn (2,100 m, 6,900 ft), the average temperature for the year is only 6.5 °C (43.7 °F), for January −17 °C (1.4 °F), for July 18 °C (64.4 °F).
The most important river is the Ili, which enters Jetisu from the Tian Shan mountains of China's Ili Kazakh Autonomous Prefecture in northern Xinjiang, and drains it for 250 km before it enters Lake Balkhash. The Chu River also rises in the Tian Shan mountains and flows north-westwards through the former Akmolinsk province of the Governor-Generalship of the Steppes. The Naryn River flows south-westwards along a longitudinal valley of the Tian Shan, and enters the Fergana Valley to join the Syr Darya. The major lakes of the area include Lake Balkhas (or Denghiz) and Lake Ala Kul, which was connected with Balkash in the post-Pliocene period but now stands some hundred feet higher, connected by a chain of smaller lakes with Sissyk Kul, Lake Issyk-Kul, and the alpine lakes of Son-Kul and Chatyr-Kul.
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