Trebišnjica wellsprings group
Trebišnjica wellspring-group is a system of two geographically and hydrologically distinct principal groupings of strong karstic springs, Trebišnjica and Čeplica, which together constitute source of the Trebišnjica river. Wellsprings are located just below town of Bileća in Bosnia and Herzegovina. The entire area where springs are situated is submerged under Bilećko Lake since 1968, with construction of Trebinje-1 Hydroelectric Power Station and its dam at Grnčarevo village.[3]
Trebišnjica wellsprings group | |
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Karst spring | |
Dejanova Pećina, main wellspring of the Trebišnjica river - photochrome cca 1890 | |
Location | Bileća, Bosnia and Herzegovina |
Coordinates | 42.8644525°N 18.4212613°E |
Spring source | Trebišnjica river |
Elevation | 325 m 1,066 ft a.s.l.[1] |
Type | Karst spring |
Discharge | 125 m3/s 4,400 cu ft/s to 220 m3/s 7,800 cu ft/s[2] |
Location in Bosnia and Herzegovina Wellspring location in Bosnia and Herzegovina |
Springs
The Trebišnjica river emerges under the karstic plateau on which town of Bileća sits. There are two main spring-groups, first in immediate proximity of town itself, and second some 3 kilometers downstream at Ćeplica village.
Trebišnjica spring-group
The Trebišnjica spring-group below Bileća, at 325 m (1,066 ft) a.s.l.,[1] is composed of three major wellspring outlets, "Dejanova Pećina", "Vrelo Oko", and "Nikšičko Vrelo".
Čepelica spring-group
Another submerged springs are Čepelica river spring-group ("Čeplica spring-group"), located at Ćeplica village, 3.25 kilometres (2.02 mi) further down the stream from first group, at 324 m (1,063 ft) a.s.l.[1] The Čepelica river itself was less than 2 kilometres (1.2 mi) long seasonal river, and flowed through valley of "Luke" (literally transl. Bay, Haven, Harbour; figuratively transl. glade(s), meadow(s)) before it meet Trebišnjica at "Mistialj" confluence. The Čepelica spring-group consists of two main karst hydrological features, Wellspring Čepo (Vrelo "Čepo") with three main outlets, and group of smaller estavelles (sinkholes) and springs on the left-bank side of the Čeplica river streambed.
See also
References
- "KARST HYDROLOGY & HYDROGEOLOGY - The Trebišnjica River Spring-group below Bileća (Vrela Rijeke Trebišnjice) - 2.3.2. Overview of the Fatničko Polje Karst Outlet Springs". www.devonkarst.org.uk. The Devon Karst Research Society. Retrieved 21 January 2019.
- "KARST HYDROLOGY & HYDROGEOLOGY - The Trebišnjica River Spring-group below Bileća (Vrela Rijeke Trebišnjice) - Monitored Effects during and after the Submersion of the Trebišnjica". www.devonkarst.org.uk. The Devon Karst Research Society. Retrieved 21 January 2019.
- "KARST HYDROLOGY & HYDROGEOLOGY - The Trebišnjica River Spring-group below Bileća (Vrela Rijeke Trebišnjice)". www.devonkarst.org.uk. The Devon Karst Research Society. Retrieved 29 October 2018.