HYDROLOGICAL RISKS CHARACTERISTIC FOR PRAPASTIILOR DRAINAGE BASIN, PIATRA CRAIULUI MOUNTAINS
Hydrological Risks Characteristic for Prăpăstiilor Drainage Basin, Piatra Craiului Mountains. The subject of this paper aims to present the characteristics of extreme hydrological phenomena form Prăpăstiilor Drainage Basin. Prăpăstiilor Drainage Basin is situated in the north-eastern part of Piatra...
| Main Authors: | , |
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| Format: | Article |
| Language: | English |
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Cluj University Press
2012-03-01
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| Series: | Aerul şi Apa: Componente ale Mediului |
| Subjects: | |
| Online Access: | http://aerapa.conference.ubbcluj.ro/2012/pdf/59%20Munteanu%20Anca.pdf |
| _version_ | 1827613309151477760 |
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| author | ANCA MUNTEANU VALENTINA ILINCA STOICA |
| author_facet | ANCA MUNTEANU VALENTINA ILINCA STOICA |
| author_sort | ANCA MUNTEANU |
| collection | DOAJ |
| description | Hydrological Risks Characteristic for Prăpăstiilor Drainage Basin, Piatra Craiului Mountains. The subject of this paper aims to present the characteristics of extreme hydrological phenomena form Prăpăstiilor Drainage Basin. Prăpăstiilor Drainage Basin is situated in the north-eastern part of Piatra CraiuluiMountains, eastern Carpathians. The structural conformation, given by the presence of Piatra Craiului syncline and by the limestone-conglomerate lithologic pattern, determines certain characteristics of the hydrographic network, which is mostly temporary, because of the water infiltration into the substrate. The springs, which provide permanent flow to the network, occur only on the syncline axis and at the base of slope deposits. When entering the gorge areas, they disappear in the same substrate, and reappear as springs, downstream of the gorges. Thus, because of these aspects, over which climate elements overlap, during periods of heavy rain, extreme events like floods frequently occur in different sectors. Effects on the environment components are complex. The floods accelerate the erosion, can affect the forest roads, construction or isolated houses along water bodies. Sometimes, the floods reach Zărnești town, causing damages or casualties. This paper comes to complete studies conducted till present on the enigmatic Piatra Craiului Mountains and its surroundings, which were included in Piatra Craiului National Park. |
| first_indexed | 2024-03-09T08:36:55Z |
| format | Article |
| id | doaj.art-6b6e6977971446138d50ecf14bb83004 |
| institution | Directory Open Access Journal |
| issn | 2067-743X |
| language | English |
| last_indexed | 2024-03-09T08:36:55Z |
| publishDate | 2012-03-01 |
| publisher | Cluj University Press |
| record_format | Article |
| series | Aerul şi Apa: Componente ale Mediului |
| spelling | doaj.art-6b6e6977971446138d50ecf14bb830042023-12-02T17:58:56ZengCluj University PressAerul şi Apa: Componente ale Mediului2067-743X2012-03-012012437444HYDROLOGICAL RISKS CHARACTERISTIC FOR PRAPASTIILOR DRAINAGE BASIN, PIATRA CRAIULUI MOUNTAINSANCA MUNTEANUVALENTINA ILINCA STOICAHydrological Risks Characteristic for Prăpăstiilor Drainage Basin, Piatra Craiului Mountains. The subject of this paper aims to present the characteristics of extreme hydrological phenomena form Prăpăstiilor Drainage Basin. Prăpăstiilor Drainage Basin is situated in the north-eastern part of Piatra CraiuluiMountains, eastern Carpathians. The structural conformation, given by the presence of Piatra Craiului syncline and by the limestone-conglomerate lithologic pattern, determines certain characteristics of the hydrographic network, which is mostly temporary, because of the water infiltration into the substrate. The springs, which provide permanent flow to the network, occur only on the syncline axis and at the base of slope deposits. When entering the gorge areas, they disappear in the same substrate, and reappear as springs, downstream of the gorges. Thus, because of these aspects, over which climate elements overlap, during periods of heavy rain, extreme events like floods frequently occur in different sectors. Effects on the environment components are complex. The floods accelerate the erosion, can affect the forest roads, construction or isolated houses along water bodies. Sometimes, the floods reach Zărnești town, causing damages or casualties. This paper comes to complete studies conducted till present on the enigmatic Piatra Craiului Mountains and its surroundings, which were included in Piatra Craiului National Park.http://aerapa.conference.ubbcluj.ro/2012/pdf/59%20Munteanu%20Anca.pdfhydrological riskshydrographic factorsfloodsPrăpăstiile Zărneștiului Drainage BasinPiatra Craiului Mountains |
| spellingShingle | ANCA MUNTEANU VALENTINA ILINCA STOICA HYDROLOGICAL RISKS CHARACTERISTIC FOR PRAPASTIILOR DRAINAGE BASIN, PIATRA CRAIULUI MOUNTAINS Aerul şi Apa: Componente ale Mediului hydrological risks hydrographic factors floods Prăpăstiile Zărneștiului Drainage Basin Piatra Craiului Mountains |
| title | HYDROLOGICAL RISKS CHARACTERISTIC FOR PRAPASTIILOR DRAINAGE BASIN, PIATRA CRAIULUI MOUNTAINS |
| title_full | HYDROLOGICAL RISKS CHARACTERISTIC FOR PRAPASTIILOR DRAINAGE BASIN, PIATRA CRAIULUI MOUNTAINS |
| title_fullStr | HYDROLOGICAL RISKS CHARACTERISTIC FOR PRAPASTIILOR DRAINAGE BASIN, PIATRA CRAIULUI MOUNTAINS |
| title_full_unstemmed | HYDROLOGICAL RISKS CHARACTERISTIC FOR PRAPASTIILOR DRAINAGE BASIN, PIATRA CRAIULUI MOUNTAINS |
| title_short | HYDROLOGICAL RISKS CHARACTERISTIC FOR PRAPASTIILOR DRAINAGE BASIN, PIATRA CRAIULUI MOUNTAINS |
| title_sort | hydrological risks characteristic for prapastiilor drainage basin piatra craiului mountains |
| topic | hydrological risks hydrographic factors floods Prăpăstiile Zărneștiului Drainage Basin Piatra Craiului Mountains |
| url | http://aerapa.conference.ubbcluj.ro/2012/pdf/59%20Munteanu%20Anca.pdf |
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