SLIDE INVENTORY IN DUBRACINA RIVER BASIN
he slide inventory in Dubračina river basin consists of 39 slides. They have been detected by field geomorphological mapping and visual analysis of 1 meter digital elevation model. The slides detected using elevation model are validated by the field checking as well. The outline of all slides is gen...
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| Format: | Article |
| Language: | English |
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Faculty of Mining, Geology and Petroleum Engineering
2013-12-01
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| Series: | Rudarsko-geološko-naftni Zbornik |
| Subjects: | |
| Online Access: | http://hrcak.srce.hr/index.php?show=clanak&id_clanak_jezik=165693&lang=en |
| _version_ | 1797712007922712576 |
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| author | Aleksandar Toševski |
| author_facet | Aleksandar Toševski |
| author_sort | Aleksandar Toševski |
| collection | DOAJ |
| description | he slide inventory in Dubračina river basin consists of 39 slides. They have been detected by field geomorphological mapping and visual analysis of 1 meter digital elevation model. The slides detected using elevation model are validated by the field checking as well. The outline of all slides is generated using digital elevation model. The total area affected by sliding is 81873 m2 which is 0,44% of researched area. The area, volume, total lenght, width of displaced mass, dip angle of slope on the slide location and dip direction of sliding have been defined for each slide. Slides areas are ranging from 150 to 12956 m2. Minimal total slide lenght from the crown to the tip is 20 m and maximal is 226 m. Angles of slope dip on slide locations are ranging from 10,1° to 28,6° focusing that 76,7% total area affected by sliding has slope dip angle on slide location up to 20°. According to weighting factor calculations lithological unit flysch (E2,3) is marked as the most significant lithological factor of the sliding. All slides are located in the flysch weathering zone where zone crop out. It has been shown that terrain tendency for excessive erosion is very limitative factor in using digital elevation model for the remote slide mapping (the paper is published in Croatian). |
| first_indexed | 2024-03-12T07:15:26Z |
| format | Article |
| id | doaj.art-8b09faeefe8c44109d7f6572b514220b |
| institution | Directory Open Access Journal |
| issn | 0353-4529 1849-0409 |
| language | English |
| last_indexed | 2024-03-12T07:15:26Z |
| publishDate | 2013-12-01 |
| publisher | Faculty of Mining, Geology and Petroleum Engineering |
| record_format | Article |
| series | Rudarsko-geološko-naftni Zbornik |
| spelling | doaj.art-8b09faeefe8c44109d7f6572b514220b2023-09-02T22:50:02ZengFaculty of Mining, Geology and Petroleum EngineeringRudarsko-geološko-naftni Zbornik0353-45291849-04092013-12-01271116SLIDE INVENTORY IN DUBRACINA RIVER BASINAleksandar Toševski0Geološko kartiranje, d.o.o., Zvonimirova 117A, 21210 Solin, Hrvatskahe slide inventory in Dubračina river basin consists of 39 slides. They have been detected by field geomorphological mapping and visual analysis of 1 meter digital elevation model. The slides detected using elevation model are validated by the field checking as well. The outline of all slides is generated using digital elevation model. The total area affected by sliding is 81873 m2 which is 0,44% of researched area. The area, volume, total lenght, width of displaced mass, dip angle of slope on the slide location and dip direction of sliding have been defined for each slide. Slides areas are ranging from 150 to 12956 m2. Minimal total slide lenght from the crown to the tip is 20 m and maximal is 226 m. Angles of slope dip on slide locations are ranging from 10,1° to 28,6° focusing that 76,7% total area affected by sliding has slope dip angle on slide location up to 20°. According to weighting factor calculations lithological unit flysch (E2,3) is marked as the most significant lithological factor of the sliding. All slides are located in the flysch weathering zone where zone crop out. It has been shown that terrain tendency for excessive erosion is very limitative factor in using digital elevation model for the remote slide mapping (the paper is published in Croatian).http://hrcak.srce.hr/index.php?show=clanak&id_clanak_jezik=165693&lang=enslide inventoryDubracina river basinflyschfield geomorphological mappingdigital elevation modeldip angleexcessive erosion |
| spellingShingle | Aleksandar Toševski SLIDE INVENTORY IN DUBRACINA RIVER BASIN Rudarsko-geološko-naftni Zbornik slide inventory Dubracina river basin flysch field geomorphological mapping digital elevation model dip angle excessive erosion |
| title | SLIDE INVENTORY IN DUBRACINA RIVER BASIN |
| title_full | SLIDE INVENTORY IN DUBRACINA RIVER BASIN |
| title_fullStr | SLIDE INVENTORY IN DUBRACINA RIVER BASIN |
| title_full_unstemmed | SLIDE INVENTORY IN DUBRACINA RIVER BASIN |
| title_short | SLIDE INVENTORY IN DUBRACINA RIVER BASIN |
| title_sort | slide inventory in dubracina river basin |
| topic | slide inventory Dubracina river basin flysch field geomorphological mapping digital elevation model dip angle excessive erosion |
| url | http://hrcak.srce.hr/index.php?show=clanak&id_clanak_jezik=165693&lang=en |
| work_keys_str_mv | AT aleksandartosevski slideinventoryindubracinariverbasin |