التحليل المورفومتري لحوض وادي الغانمي
Abstract
THE BASIN VALLEY GHANIMI OF DRY VALLEYS IN THE PLATEAU OF SOUTHERN IRAQ AND IS LOCATED WITHIN THE ADMINISTRATIVE BOUNDARIES OF THE PROVINCE OF MUTHANNA, HAS BEEN USED VISUALIZATION SPACE AND VISUAL RADAR AND TOPOGRAPHIC MAPS AND GEOLOGICAL AS WELL AS A FIELD STUDY IN ORDER TO VERIFY FACTORS TABIEIYH AFFECTING THE PELVIS, PARTICULARLY THE NATURE AND ROCKY CLIMATE AND TOPOGRAPHICAL CHARACTERISTICS, THE TOTAL AREA OF THE BASIN (1308.031 KM 2), ACTING IN ITS WATERS IN THE RAINY SEASON TO THE LOW ALSALIBAT, THE BASIN HAS BEEN DIVIDED INTO 4 POOLS IN THE SECONDARY VARIED IN SIZE DEPENDING ON THE VARIATION OF THE FACTORS AND GEOMORPHOLOGICAL PROCESSES. THROUGH ANALYSIS ALMORVOMITRI TO NETWORK PROPERTIES WATERY DISCHARGE SHOW THAT THE BASIN IS CLOSE TO RECTANGULAR AND CLOSER TO FORM A TRIANGLE, AS SHOWN THROUGH THE ANALYSIS OF LONGITUDINAL SECTIONS OF THE BASINS OF THE STUDY AREA, THE VALLEYS PASS IN THE BEGINNING STAGES OF DEVELOPMENT GEOMORPHOLOGICAL OTHER WORDS, THE PROCESS OF EROSION EXCEEDS THE DEPOSITION PROCESS, THE NUMBER OF STREAMS RIVER BASINS ALL ARRANGED TO (THE COURSE OF 4482), THIS HAS BEEN VARIED IN THE SEWER BASINS PREPARED ACCORDING TO ALTHRIA DUE TO VARIATION IN THE COMPOSITION AND OPERATIONS OF ITS INCEPTION, AS WELL AS THE VARIATION OF THE ENVIRONMENT COMPONENT TO IT.
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