Reasons and mechanism for soil sliding processes in the Rebrnice area, Vipava valley, SW Slovenia
A motorway Razdrto–Podnanos is being built across Rebrnice area in Vipava valley. There is limestone scree material deposed on flysch rocks.Limestones creeis unstable and gradually slides downslopes because of slope inclination, underground water and clayey zones. Clayey zones have been created on t...
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| Format: | Article |
| Language: | English |
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Geological Survey of Slovenia
2007-06-01
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| Series: | Geologija |
| Subjects: | |
| Online Access: | http://www.geologija-revija.si/dokument.aspx?id=345 |
| _version_ | 1797945350308233216 |
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| author | Jernej Jež |
| author_facet | Jernej Jež |
| author_sort | Jernej Jež |
| collection | DOAJ |
| description | A motorway Razdrto–Podnanos is being built across Rebrnice area in Vipava valley. There is limestone scree material deposed on flysch rocks.Limestones creeis unstable and gradually slides downslopes because of slope inclination, underground water and clayey zones. Clayey zones have been created on the contact between scree and flysch rocks. Material movements can be observed on the surface but they were also measured in wells. Limestone scree composition and reasons for landslides were described in this article. |
| first_indexed | 2024-04-10T20:53:43Z |
| format | Article |
| id | doaj.art-ba534a68ae9049c9ab0a1448350e20d3 |
| institution | Directory Open Access Journal |
| issn | 0016-7789 1854-620X |
| language | English |
| last_indexed | 2024-04-10T20:53:43Z |
| publishDate | 2007-06-01 |
| publisher | Geological Survey of Slovenia |
| record_format | Article |
| series | Geologija |
| spelling | doaj.art-ba534a68ae9049c9ab0a1448350e20d32023-01-23T08:10:15ZengGeological Survey of SloveniaGeologija0016-77891854-620X2007-06-015015563Reasons and mechanism for soil sliding processes in the Rebrnice area, Vipava valley, SW SloveniaJernej JežA motorway Razdrto–Podnanos is being built across Rebrnice area in Vipava valley. There is limestone scree material deposed on flysch rocks.Limestones creeis unstable and gradually slides downslopes because of slope inclination, underground water and clayey zones. Clayey zones have been created on the contact between scree and flysch rocks. Material movements can be observed on the surface but they were also measured in wells. Limestone scree composition and reasons for landslides were described in this article.http://www.geologija-revija.si/dokument.aspx?id=345RebrnicelandslideflyschlimestonescreeVipavavalleySlovenia |
| spellingShingle | Jernej Jež Reasons and mechanism for soil sliding processes in the Rebrnice area, Vipava valley, SW Slovenia Geologija Rebrnice landslide flysch limestonescree Vipavavalley Slovenia |
| title | Reasons and mechanism for soil sliding processes in the Rebrnice area, Vipava valley, SW Slovenia |
| title_full | Reasons and mechanism for soil sliding processes in the Rebrnice area, Vipava valley, SW Slovenia |
| title_fullStr | Reasons and mechanism for soil sliding processes in the Rebrnice area, Vipava valley, SW Slovenia |
| title_full_unstemmed | Reasons and mechanism for soil sliding processes in the Rebrnice area, Vipava valley, SW Slovenia |
| title_short | Reasons and mechanism for soil sliding processes in the Rebrnice area, Vipava valley, SW Slovenia |
| title_sort | reasons and mechanism for soil sliding processes in the rebrnice area vipava valley sw slovenia |
| topic | Rebrnice landslide flysch limestonescree Vipavavalley Slovenia |
| url | http://www.geologija-revija.si/dokument.aspx?id=345 |
| work_keys_str_mv | AT jernejjez reasonsandmechanismforsoilslidingprocessesintherebrniceareavipavavalleyswslovenia |