{"title":"GEOMORPHOLOGICAL SCHEMATIZATION OF THE DRAINAGE OF THE SHARYN RIVER BASIN","authors":"Z. Mustafaev, A.R. Zhansykpaev","doi":"10.54668/2789-6323-2021-102-3-6-16","DOIUrl":null,"url":null,"abstract":"On the basis of the geosystem approach, using the laws of geographic vertical zoning, the energy resources of river basins and groundwaters, the natural and climatic potential of natural systems that characterize the heat and moisture supply of natural landscapes were determined, which made it possible to carry out a geomorphological schematization of the catchment area of the class of landscapes (eluvial facies), foothill subclass of landscapes (transeluvial facies), foothill lowland subclass of landscapes (transaccumulative facies) and plain class of landscapes (superaquial and subaquial facies) and the natural function of the river basin, that is, nature improvement.","PeriodicalId":256870,"journal":{"name":"Hydrometeorology and ecology","volume":"49 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Hydrometeorology and ecology","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.54668/2789-6323-2021-102-3-6-16","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
On the basis of the geosystem approach, using the laws of geographic vertical zoning, the energy resources of river basins and groundwaters, the natural and climatic potential of natural systems that characterize the heat and moisture supply of natural landscapes were determined, which made it possible to carry out a geomorphological schematization of the catchment area of the class of landscapes (eluvial facies), foothill subclass of landscapes (transeluvial facies), foothill lowland subclass of landscapes (transaccumulative facies) and plain class of landscapes (superaquial and subaquial facies) and the natural function of the river basin, that is, nature improvement.
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