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Fergana valley distribution landscapes establishment and exploration

Boymirzaev Karimjon MirzaxmedovichNamangan State UniversityKhalilova Khurshida TeshaevnaTashkent regional center for retraining and advanced training of public educators
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AbstractThis article deals with the formation of distribution landscapes in the Fergana Valley and the research of specialists. The conical spreads of Uzbekistan, including the Fergana Basin, are still experiencing a significant rise and expansion. The rise of conical distribution and dry deltas, as well as the dynamic changes in their morphological structure, have found their bright expression in their upper and middle parts. Delta or conical distributions can be in water and on land, which differ in the natural properties of the environment in which they are formed. The main reason for this is that the rivers and streams that flow from the mountain ranges that surround the basins on all sides flow into the foothill plains, splitting into branches and laying out the muddy rocks that have flowed. The greater the number of streams, streams, and rivers flowing from the mountains, the greater the number of conical distributions and dry deltas, or conversely, the lower the number of rivers and streams, the lower the number of conical distributions and dry deltas.

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