Bâsca Roziliei River

Râul Bâsca Roziliei
River
The Bâsca River near confluence with Buzău River
Countries	Romania
Region	Transylvania, Wallachia
Counties	Covasna, Buzău
Commune	Comandău, Gura Teghii
Source
- location	Lacăuţi Mountains, Cuverture Charpatinas
- elevation	1,500 m (4,921 ft)
- coordinates	45°51′32″N 26°22′14″E / 45.85889°N 26.37056°E / 45.85889; 26.37056
Mouth	Buzău River
- location	Upstream of Lunca Priporului, Buzău
- elevation	385 m (1,263 ft)
- coordinates	45°26′21″N 26°18′44″E / 45.43917°N 26.31222°E / 45.43917; 26.31222Coordinates: 45°26′21″N 26°18′44″E / 45.43917°N 26.31222°E / 45.43917; 26.31222
Length	81 km (50 mi)
Basin	785.1 km2 (303 sq mi)
Discharge	for Bâsca Roziliei hydrometryc station,[1][2]
- average	11.7 m3/s (413 cu ft/s)
- max	960 m3/s (33,902 cu ft/s)
- min	1.72 m3/s (61 cu ft/s)
Official River Code	XII_1.82.15…[3]

The Bâsca Roziliei River, also called Bâsca Rusilei, Bâsca Rosiliei or simply Bâsca (Romanian: Bɨs'ca),^[4][5] is a main tributary (discharge and watershed) of the Buzău River, from Romania.

Geographic position

Positioned in the external region of the curvature of Carpathians (subunit of Eastern Carpathians),^[6] the Bâsca River Catchment has a surface of 785.1 km² (data obtained using the Topographic Maps of Romania at scale 1:25,000).^[7] It lies at an average altitude of 1,081 m between the Lăcăuți Peak (1,777 m altitude) and the confluence with the Buzău River (385 m altitude).

Geology

From the geological point of view, the Bâsca River Catchment overlaps the orogenic unit of the Eastern Carpathians, where the external Paleogene flysch is predominant, including: sandstones (Tarcău sandstones Facies), marl, conglomerates. This area is characterised by tectonic uplift and by severe seismicity related to the Vrancea Epicentral Area, being affected by deep-seated landslides (Ielenicz, 1984). Lithology is dominated by the presence of the hardest and hard rocks, covering 96.7% of the catchment surface.

Climate

The climate of the Bâsca Catchment is temperate-continental. Föhn phenomena moderate the characteristics parameters of climatic elements, e.g. average multiannual atmospheric temperature between 1.2 °C at the Lăcăuți meteorological station between 1961 and 2000, see Table, and 2.4 °C at the Penteleu station (1988–2007), combined with precipitations of 664.3 mm at Penteleu and 830.1 mm at Lăcăuți.^[8]

Hydrography

• Major river tributaries

The following rivers are tributaries to the Bâsca River:

– left: Delușor, Ghiurca Mare, Slobod, Pătac, Bâsculița, Cernat, Milei, Bâsca Mică (with Giurgiu, Fagul Alb, Ciulianoș, Bălescuțu, Şapte Izvoare, Secuiul, Brebu and Boul), Varlaam, Tigva, Fulgeriş, Tainiţă, Gotiş, Hânsaru, Valea Largă, Aniniş;

– right: Toplița, Ruginosul, Saroș, Dârnăul Mare, Cireș, Corongoș, Surduc, Coceanul, Piciorul Milei, Brațul, Tega, Păltiniş, Vineţişu.

• Reservoirs

On the Bâsca River the project "Hydropower Siriu – Surduc Development”, has been developed (being now in construction stage). This project includes a permanent water reservoir "Cireșu" on the upper part of the Bâsca River and an underground derivation "Surduc – Nehoiașu", from Cireșu Accumulation and Bâsca River towards the "CHE Nehoiaşu II” hydroelectric power station.^[10]

• Morphometrical features of the Bâsca River Catchment and its main sub-catchments^[11]

Hydrology

The most common risk hydric phenomena affecting the catchment area are floods and flooding. Associated to these are processes of river channel dynamics, landslides and falls. The frequency analysis of the maximum monthly discharge indicates that the month with the highest flood potential is July, followed by June. In July were recorded the highest floods. Among them, remarkable for their socio-economic consequences where those from 1969, 1975, 2002. The annual maximum flow of the Bâsca River varied between 39.4 m³/s (year 1986) and 960 m³/s (year 1975, 2 Jul). Exceptionally floods were recorded in the years: 1975 (960 m³/s), 1969 (697 m³/s), 1991 (530 m³/s) and 1985 (515 m³/s).^[12][13] Multiannual average flow at this station is about 12 m³/s. Damaging effects caused by floods and flooding have determined property damage, such as flooded homes (e.g. on 20 July 2002, Păltiniş River inundated homes in the area of the confluence with the Bâsca River), landslides and slope destabilization of versants; destruction of undermining and hydrotechnical works, affecting sections of the roads and humans casualties.

Demographic and socio-economic features

• from a demographic point of view, the Bâsca River Catchment is situated in a human area with low density (8.35 inhabitants/km²). In this catchment they are two communes: Comandău (1,042 inhabitants) and Gura Teghii (3,884 inhabitants) and two villages appartining to the town of Nehoiu: Bâsca Roziliei (1,428 inhabitants) and Vineţişu (206 inhabitants);^[14]
• localities situated in the upper part: Comandău commune and lower part of the Bâsca River Catchment: Vadu Oii (on Bâsca Mică River), Varlaam (at confluence Bâsca River or Bâsca Mare River with Bâsca Mică River), Gura Teghii, Nemertea, Furtunești, Păltiniș and Bâsca Roziliei;
• the economical areas of activities of local profile it is focused on tree cutting from the forest and primary processed seasonal activity of pastoral and harvest of therapeutically herbs.

References

Maps

• Harta Siriu – Trasee Montane
• Harta Munții Buzăului
• geo-spatial.org, accessed 2010