Vitunjčica
| Vitunjčica | |
|---|---|
| Location | |
| Countries | |
| Physical characteristics | |
| Source | |
| • location | Vitunj |
| • coordinates | 45°17′29″N 15°08′25″E / 45.2914°N 15.1404°E[2] |
| • elevation | 347.8 m (1,141 ft)[2] |
| Mouth | |
• location | Turkovići Ogulinski |
• coordinates | 45°16′52″N 15°10′31″E / 45.2810°N 15.1752°E[1] |
| Length | 4.13 km (2.57 mi)[2][3] |
| Basin size | 18 square kilometres (6.9 mi2)[2][3][1] |
| Basin features | |
| Progression | Dobra→ Kupa→ Sava→ Danube→ Black Sea |
Vitunjčica is a right tributary of the Gornja Dobra that runs through the karst polje of Vitunj, flowing into the Ogulin-Plaški valley.
Name
Derived from the oikonym Vitunj.[4]: 47, 48
Hydrology
Since at least 1981, the water level of the Vitunjčica has been recorded at the Brestovica station. Its mean maximum discharge exceeds 400 l/s.[5]
At high flow, the water level at the springs is up to 1 metre (3.3 ft) higher in elevation.[6]: 54
Geology
Its source is in the contact zone between Limestone and Dolomite of the Lower Cretaceous, in a basin of mostly Lower Cretaceous and Malmic Dolomite, but the constant flow indicates a significant subterranean length.[6]: 53
The source itself is a double fracture spring, each individual crack sloped downward. There spring immediately flows as a river, without pooling.[6]: 54
Biology
The diatom Navicula trivialis Lange-Bertalot was found in the Vitunjčica.[7]: 40
Tributaries
It has permanent left tributaries Lubardinka (188 metres (617 ft)), Klanac[8] and Rakovac (3.18 kilometres (1.98 mi)).[6] There are also the permanent right tributaries Jarak (1.94 kilometres (1.21 mi)), which flows into the spring of the Vitunjčica, Kobeljak (3.46 kilometres (2.15 mi)), Crni Potok (4.6 kilometres (2.9 mi)), and seasonal right tributaries Bare (612 metres (2,008 ft)) and Bocinka (780 metres (2,560 ft)), between which lie the Zdenac springs. Many smaller springs flow the Vitunjčica from its source to the mouth of the Lubardinka, 3 seasonal or fossil springs from there to the mouth of the Rakovac, and 3 springs with streams on the field after the fishery, 2 springs with streams on the field south of Grabovača, and several smaller springs from the cliffs of Grabovača, all on the left bank.[1]
Crni Potok was first studied in depth in 2017, although it had been mentioned by both Poljak 1926[8] and Bahun 1968.[6] It is very steep, cascading along most of its course.[9]
References
- ^ a b c Državna geodetska uprava (1983). Hrvatska osnovna kartau mjerilu 1:5000 (Map). § Ogulin: 5 G 18 - 37.
- ^ a b c d Državna geodetska uprava (1983). Hrvatska osnovna kartau mjerilu 1:5000 (Map). § Ogulin: 5 G 18 - 26.
- ^ a b Državna geodetska uprava (1983). Hrvatska osnovna kartau mjerilu 1:5000 (Map). § Ogulin: 5 G 18 - 36.
- ^ Vidović, Domagoj (2011). "Toponimija sela Zvirovići". Župa Studenci u Hercegovini. Mostar: Crkva na kamenu. pp. 47–57. ISBN 978-9958-1918-1-7.
- ^ Pavlić, Krešimir; Jakobović, Daniel (2018-06-11). "High flows from Gornja Dobra basin". Rudarsko-geološko-naftni zbornik. 33 (3): 45–52. doi:10.17794/rgn.2018.3.5. eISSN 1849-0409.
- ^ a b c d e Bahun, Stjepan (1968). "Geološka osnova hidrogeološkh odnosa krškog područja između Slunja i Vrbovskog" (PDF). Geološki vjesnik. 21: 19–82. ISSN 0016-7924.
- ^ Tadić, Nela (2022-06-15) [defended 2022-06-13]. Rasprostranjenost i ekološke značajke algi kremenjašica roda Navicula u tekućicama u Hrvatskoj [Distribution and ecology of the diatom genus Navicula in running water in Croatia] (Thesis) (in Croatian). Zagreb: Prirodoslovno-matematički fakultet Sveučilišta u Zagrebu.
- ^ a b Poljak, Josip (1926). "Geomorfologija i hidrografija okoliša Ogulina i ogulinskog Zagorja". Spomenica u počast prof. dr. Gorjanović-Krambergeru [Geomorphology and Hydrography of the Ogulin and Ogulinsko Zagorje Regions] (in Croatian). Zagreb: Hrvatsko prirodoslovno društvo. pp. 111–137.
- ^ Džankić, Marija (2018-03-13) [defended 2017-09-22]. Geomorfološka obilježja doline Crnog potoka kod Ogulina [Geomorphological features of Crni potok valley near Ogulin] (Thesis) (in Croatian). Zagreb: Prirodoslovno-matematički fakultet Sveučilišta u Zagrebu.
Further reading
- Bahun, Stjepan (1968). "Geološka osnova hidrogeoloških odnosa krškog područja između Slunja i Vrbovskog" [Geological basis of the hydrogeological relations in the karst area between Slunj and Vrbovsko] (PDF). Geološki Vjesnik (in Serbo-Croatian). 21: 19–82. ISSN 0016-7924.
- Senta Marić, Ankica; Čepelak, Radovan; Andabaka, Damir (2014). "Rijeka Dobra s pritocima". 13.stručni sastanak laboratorija ovlaštenih za ispitivanje voda [The River Dobra with Tributaries] (in Croatian). Rijeka: Zigo. pp. 61–66.
- Pavlić, Krešimir; Parlov, Jelena (2019-02-13). "Cross-Correlation and Cross-Spectral Analysis of the Hydrographs in the Northern Part of the Dinaric Karst of Croatia". Geosciences. 9 (2) 86. doi:10.3390/geosciences9020086. eISSN 2076-3263.