The Effects of Tectonic Activity in Morphology of Rueen Basin in the North East Part of Iran
Roein basin is one of the sub-basins of CalShour River, which is located in the northeastern part of Iran, on the southern slopes of the Aladagh Mountains. Tectonic activities of this basin has been started from the last Laramide orogeny and is continuing. These activities, in addition to the occurr...
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| Format: | Article |
| Language: | fas |
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University of Sistan and Baluchestan
2016-05-01
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| Series: | جغرافیا و توسعه |
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| Online Access: | https://gdij.usb.ac.ir/article_2479_2ccff1f15ba92cb4f0c2c3fc6a94b9fa.pdf |
| _version_ | 1797804978593595392 |
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| author | Gholamreza Maghami moghim |
| author_facet | Gholamreza Maghami moghim |
| author_sort | Gholamreza Maghami moghim |
| collection | DOAJ |
| description | Roein basin is one of the sub-basins of CalShour River, which is located in the northeastern part of Iran, on the southern slopes of the Aladagh Mountains. Tectonic activities of this basin has been started from the last Laramide orogeny and is continuing. These activities, in addition to the occurrence of natural disasters have many effects on different characteristics of this basin. Information about the tectonic activities due to the vicinity with this basin and its influence on Bojnoord city, (center of Northern Khorasan province) and river planning is a necessity.To investigate these activities ,Morph tectonic indicators which were related to geomorphologic were used, It means the comparison of the longitudinal and logarithmic profile; width of the valley floor index to its height ratio (vf), Sinuosity Mountain Front index (smf), sinusoidal index of river (s) and index of tectonic activities(lat). The obtained results of these indicators and the influence of folds indicated that this area is subject to intense tectonic activities and these activities in this basin have caused irregular longitudinal profile of rivers, deep and narrow valleys, extended basins and the low maze path of rivers and mountain front. Also , this study indicate that tectonic activities at the tributary of this river, in fact in the Domannim region has reached to its peak and its result is a narrow strait , steep rocky and the river slope phenomenon which is given special feature to the topography of this basin. |
| first_indexed | 2024-03-13T05:45:14Z |
| format | Article |
| id | doaj.art-d5e3f3b9cfd644daa03c250278ce85ad |
| institution | Directory Open Access Journal |
| issn | 1735-0735 2676-7791 |
| language | fas |
| last_indexed | 2024-03-13T05:45:14Z |
| publishDate | 2016-05-01 |
| publisher | University of Sistan and Baluchestan |
| record_format | Article |
| series | جغرافیا و توسعه |
| spelling | doaj.art-d5e3f3b9cfd644daa03c250278ce85ad2023-06-13T20:19:15ZfasUniversity of Sistan and Baluchestanجغرافیا و توسعه1735-07352676-77912016-05-011443719010.22111/gdij.2016.24792479The Effects of Tectonic Activity in Morphology of Rueen Basin in the North East Part of IranGholamreza Maghami moghimRoein basin is one of the sub-basins of CalShour River, which is located in the northeastern part of Iran, on the southern slopes of the Aladagh Mountains. Tectonic activities of this basin has been started from the last Laramide orogeny and is continuing. These activities, in addition to the occurrence of natural disasters have many effects on different characteristics of this basin. Information about the tectonic activities due to the vicinity with this basin and its influence on Bojnoord city, (center of Northern Khorasan province) and river planning is a necessity.To investigate these activities ,Morph tectonic indicators which were related to geomorphologic were used, It means the comparison of the longitudinal and logarithmic profile; width of the valley floor index to its height ratio (vf), Sinuosity Mountain Front index (smf), sinusoidal index of river (s) and index of tectonic activities(lat). The obtained results of these indicators and the influence of folds indicated that this area is subject to intense tectonic activities and these activities in this basin have caused irregular longitudinal profile of rivers, deep and narrow valleys, extended basins and the low maze path of rivers and mountain front. Also , this study indicate that tectonic activities at the tributary of this river, in fact in the Domannim region has reached to its peak and its result is a narrow strait , steep rocky and the river slope phenomenon which is given special feature to the topography of this basin.https://gdij.usb.ac.ir/article_2479_2ccff1f15ba92cb4f0c2c3fc6a94b9fa.pdfrueen basinmorpho tectonic indexmorphology of basin |
| spellingShingle | Gholamreza Maghami moghim The Effects of Tectonic Activity in Morphology of Rueen Basin in the North East Part of Iran جغرافیا و توسعه rueen basin morpho tectonic index morphology of basin |
| title | The Effects of Tectonic Activity in Morphology of Rueen Basin
in the North East Part of Iran |
| title_full | The Effects of Tectonic Activity in Morphology of Rueen Basin
in the North East Part of Iran |
| title_fullStr | The Effects of Tectonic Activity in Morphology of Rueen Basin
in the North East Part of Iran |
| title_full_unstemmed | The Effects of Tectonic Activity in Morphology of Rueen Basin
in the North East Part of Iran |
| title_short | The Effects of Tectonic Activity in Morphology of Rueen Basin
in the North East Part of Iran |
| title_sort | effects of tectonic activity in morphology of rueen basin in the north east part of iran |
| topic | rueen basin morpho tectonic index morphology of basin |
| url | https://gdij.usb.ac.ir/article_2479_2ccff1f15ba92cb4f0c2c3fc6a94b9fa.pdf |
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