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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Main Authors: ALIN MIHU-PINTILIE, GHEORGHE ROMANESCU, CRISTIAN STOLERIU
Format: Article
Language:English
Published: Cluj University Press 2012-03-01
Series:Aerul şi Apa: Componente ale Mediului
Subjects:
Online Access:http://aerapa.conference.ubbcluj.ro/2012/pdf/60%20a%20Mihu-Pintilie_Romanescu_Stoleriu.pdf
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spelling 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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