MORPHO-BATHYMETRIC PARAMETERS OF RECESS CRUCII LAKE (STÂNIŞOAREI MOUNTAINS)
Morpho-bathymetric parameters of recess Crucii Lake (Stânişoarei Mountains). Crucii Lake from Stânişoarei Mountains was formed in 1978 as a result of riverbed dam Cuejdel after a landslide triggered on the western slope of Muncelul Peak. The event led initially to a small accumulation of 250-300 acv...
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Cluj University Press
2012-03-01
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doaj-375474efb7b04bfaaff3a71901e179202020-11-24T20:54:00ZengCluj University PressAerul şi Apa: Componente ale Mediului2067-743X2012-03-012012445452MORPHO-BATHYMETRIC PARAMETERS OF RECESS CRUCII LAKE (STÂNIŞOAREI MOUNTAINS)ALIN MIHU-PINTILIEGHEORGHE ROMANESCUCRISTIAN STOLERIUMorpho-bathymetric parameters of recess Crucii Lake (Stânişoarei Mountains). Crucii Lake from Stânişoarei Mountains was formed in 1978 as a result of riverbed dam Cuejdel after a landslide triggered on the western slope of Muncelul Peak. The event led initially to a small accumulation of 250-300 acvatoriu m, 25-30 m wide and 4-5 m maximum depth. In the summer of 1991 following the construction of a forest road in the flysch, and amid a high humid conditions, the slide was reactivated, leading to the formation of the largest natural dam lake in Romania. It has a length of 1 km, area of 12.2 ha, maximum depth of 16 m and a water volume of ca. 907.000 m3. Morphometric and morpho-bathymetric measurements performed in the summer of 2011, with the help of the integrated 1.200 GPS of Station Leica System 1.200 surveying measurements and bathymetric measurements Valeyport Ecosounder Midas showed new values for the morpho-bathymetric parameters. Among them stands out: 13,95 ha area, perimeter 2801,1 m, maximum length of 1004,82 m, 282,6 m maximum width, maximum depth 16,45 m. To achieve the numerical model of the lake basin were more than 45.000 points bali reading, with equidistance of 0,25 m. The scale of detail work aimed to draw up a proper database to eliminate suspicions about the old analytical methods inaccuracies. At the same time was studied the evolution of the lake’s basin in the context of relatively recent geomorphological changes.http://aerapa.conference.ubbcluj.ro/2012/pdf/60%20a%20Mihu-Pintilie_Romanescu_Stoleriu.pdfbathymetryCrucii lakemorpho-graphical evolutionnatural dam laketopographic surveys |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
ALIN MIHU-PINTILIE GHEORGHE ROMANESCU CRISTIAN STOLERIU |
spellingShingle |
ALIN MIHU-PINTILIE GHEORGHE ROMANESCU CRISTIAN STOLERIU MORPHO-BATHYMETRIC PARAMETERS OF RECESS CRUCII LAKE (STÂNIŞOAREI MOUNTAINS) Aerul şi Apa: Componente ale Mediului bathymetry Crucii lake morpho-graphical evolution natural dam lake topographic surveys |
author_facet |
ALIN MIHU-PINTILIE GHEORGHE ROMANESCU CRISTIAN STOLERIU |
author_sort |
ALIN MIHU-PINTILIE |
title |
MORPHO-BATHYMETRIC PARAMETERS OF RECESS CRUCII LAKE (STÂNIŞOAREI MOUNTAINS) |
title_short |
MORPHO-BATHYMETRIC PARAMETERS OF RECESS CRUCII LAKE (STÂNIŞOAREI MOUNTAINS) |
title_full |
MORPHO-BATHYMETRIC PARAMETERS OF RECESS CRUCII LAKE (STÂNIŞOAREI MOUNTAINS) |
title_fullStr |
MORPHO-BATHYMETRIC PARAMETERS OF RECESS CRUCII LAKE (STÂNIŞOAREI MOUNTAINS) |
title_full_unstemmed |
MORPHO-BATHYMETRIC PARAMETERS OF RECESS CRUCII LAKE (STÂNIŞOAREI MOUNTAINS) |
title_sort |
morpho-bathymetric parameters of recess crucii lake (stânişoarei mountains) |
publisher |
Cluj University Press |
series |
Aerul şi Apa: Componente ale Mediului |
issn |
2067-743X |
publishDate |
2012-03-01 |
description |
Morpho-bathymetric parameters of recess Crucii Lake (Stânişoarei Mountains). Crucii Lake from Stânişoarei Mountains was formed in 1978 as a result of riverbed dam Cuejdel after a landslide triggered on the western slope of Muncelul Peak. The event led initially to a small accumulation of 250-300 acvatoriu m, 25-30 m wide and 4-5 m maximum depth. In the summer of 1991 following the construction of a forest road in the flysch, and amid a high humid conditions, the slide was reactivated, leading to the formation of the largest natural dam lake in Romania. It has a length of 1 km, area of 12.2 ha, maximum depth of 16 m and a water volume of ca. 907.000 m3. Morphometric and morpho-bathymetric measurements performed in the summer of 2011, with the help of the integrated 1.200 GPS of Station Leica System 1.200 surveying measurements and bathymetric measurements Valeyport Ecosounder Midas showed new values for the morpho-bathymetric parameters. Among them stands out: 13,95 ha area, perimeter 2801,1 m, maximum length of 1004,82 m, 282,6 m maximum width, maximum depth 16,45 m. To achieve the numerical model of the lake basin were more than 45.000 points bali reading, with equidistance of 0,25 m. The scale of detail work aimed to draw up a proper database to eliminate suspicions about the old analytical methods inaccuracies. At the same time was studied the evolution of the lake’s basin in the context of relatively recent geomorphological changes. |
topic |
bathymetry Crucii lake morpho-graphical evolution natural dam lake topographic surveys |
url |
http://aerapa.conference.ubbcluj.ro/2012/pdf/60%20a%20Mihu-Pintilie_Romanescu_Stoleriu.pdf |
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1716795450008272896 |