This article provides information on water sources in the Southern Fergana landscape and their role in recreation. Nazarov H. Yo | Xusanov Sh | Shokiraliyeva Sh "Water Sources of the Southern Fergana Landscape and their Role in Recreation" Published in International Journal of Trend in Scientific Research and Development (ijtsrd), ISSN: 2456-6470, Special Issue | Innovative Development of Modern Research , April 2021, URL: https://www.ijtsrd.com/papers/ijtsrd41158.pdf Paper URL : https://www.ijtsrd.com/humanities-and-the-arts/geography/41158/water-sources-of-the-southern-fergana-landscape-and-their-role-in-recreation/nazarov-h-yo
International Journal of Trend in Scientific Research and Development (IJTSRD)
Special Issue on Innovative Development of Modern Research
Available Online: www.ijtsrd.com e-ISSN: 2456 – 6470
ID: IJTSRD41158 | Special Issue on Innovative Development of Modern Research
Page 155
Water Sources of the Southern Fergana
Landscape and their Role in Recreation
Nazarov H. Yo1, Xusanov Sh2, Shokiraliyeva Sh2
1Lecturer at the Department of Geography and Economics of KSPI, Uzbekistan
2Student Majoring in Geography and Economics of KSPI, Uzbekistan
ABSTRACT
This article provides information on water sources in the
Southern Fergana landscape and their role in recreation.
Rivers, lakes and groundwater make up the water resources
of the region. The foothills and plains of the region belong to
the area that hydrologically consumes and evaporates water,
and the mountains to the south of it from the surface and
groundwater runoff.
The Syrdarya is a transit river that begins and flows out of
the region. Its left bank to the middle stream flows at a
certain distance to the Kayrakkum Reservoir, creating
recreational landscapes in the region.
The main rivers flowing into the region are the Sokh,
Isfayram and Isfara rivers, which are actively involved in the
formation of recreational landscape complexes. Some of
them start in the Alay Mountains (Isfayram, Shohimardon),
while Isfara is a fast-flowing mountain river that starts from
the Turkestan ridge. As they emerge from the mountains, the
water of these rivers divides and spreads into irrigation
canals and ditches, none of which reaches the Syrdarya.
One of the rivers abounding with water in southern Fergana
is the Sokh. It starts from the Matchokh mountain node,
which is separated from the Alay, Turkestan and Zarafshan
mountains, by a glacier at an altitude of 5549 m. It flows
through a deep and narrow ravine in the upper reaches of
the Sokh River. Here the average depth of the river valley is
1190 m, and the average slope of the slopes is 27