geo.wikisort.org - River

The Bâsca (Romanian: Bɨs'ca), also called Bâsca Mare in its upper course,[3] and Bâsca Roziliei in its lower course,[4] is a left tributary of the river Buzău, in Romania.[3][5] It discharges into the Buzău near Nehoiu.

Bâsca Bâsca Roziliei
The Bâsca near confluence with Buzău
Location
Country	Romania
Counties	Covasna, Buzău
Physical characteristics
Source	Lăcăuți Peak
• location	Vrancea Mountains
• coordinates	45°51′32″N 26°22′14″E
• elevation	1,500 m (4,900 ft)
Mouth	Buzău
• location	Upstream of Lunca Priporului
• coordinates	45°26′21″N 26°18′44″E
• elevation	385 m (1,263 ft)
Length	81 km (50 mi)
Basin size	785.1 km2 (303.1 sq mi)
Discharge
• location	Bâsca Roziliei hydrometric station,[1][2]
• average	11.7 m3/s (410 cu ft/s)
• minimum	1.72 m3/s (61 cu ft/s)
• maximum	960 m3/s (34,000 cu ft/s)
Basin features
Progression	Buzău→ Siret→ Danube→ Black Sea
Tributaries
• left	Bâsculița, Bâsca Mică

Geographic position

Positioned in the external region of the curvature of Carpathians (subunit of Eastern Carpathians),[6] the Bâsca drainage basin has an area of 783 km² (302 sq mi).[3] Its length is 76 km (47 mi).[3] 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).[7]

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 river Bâsca (from source to mouth):[3]

– left: Țiganu, Delușor (Holom), Ghiurca Mare, Slobod, Pătac, Bâsculița, Izvorul Ascuns, Izvorul Stâncos, Cernat, Milei, Bâsca Mică, Varlaam, Tigva, Fulgeriș, Tainița, Gotiș, Hânsaru;

– right: Râșdaș, Reghin, Poplița, Saroș, Dârnăul Mic, Dârnăul Mare, Cireș, Ioviz, Surducul Mare, Cocean, Copăcelu, Piciorul Milei, Bratu, Tega, Păltiniș.

River	Catchment area (km2)[7]	River length (km)[7]
Bâsca Mică	238	46.5
Bâsculița	40	11.5
Poplița	34.2 (incl. Ruginosul)	9.3
Cireș	32.4 (incl. Corongoș)	11.1
Păltiniș	25.1	9.7
Ghiurca Mare	23.3	9.6
Dârnăul Mare	21.5	10.6
Delușor	20.9	6.9
Pătac	18.5	10
Giurgiu	16.2	6.5
Șapte Izvoare	15.6	6.6
Milei	15.8	6.4
Saroș	14.9	7.8
Corongoș	12.8	5.3
Brebu	11.1	6.6
Ruginosul	11.8	5.1
Cernat	11.1	6.7
Slobod	9.2	6.2

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 Nehoiașu II” hydroelectric power station.[10]

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).[11][12] 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, the Păltiniș inundated homes in the area of the confluence with the Bâsca), 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 appertaining to the town of Nehoiu: Bâsca Roziliei (1,428 inhabitants) and Vinețișu (206 inhabitants);[13]
• localities situated in the upper part: Comandău commune and lower part of the Bâsca River Catchment: Vadu Oii (on the Bâsca Mică), Varlaam (at confluence of the Bâsca or Bâsca Mare with the Bâsca Mică), Gura Teghii, Nemertea, Furtunești, Păltiniș and Bâsca Roziliei;
• the economical areas of activities of local it is focused on tree cutting from the forest and primary processed seasonal activity of pastoral and harvest of therapeutical herbs.

References

Maps

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

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