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Kalinovik

Kalinovik
Калиновик
View on Kalinovik
View on Kalinovik
Location of Kalinovik within Bosnia and Herzegovina
Location of Kalinovik within Bosnia and Herzegovina
Coordinates: 43°30′N 18°27′E / 43.500°N 18.450°E / 43.500; 18.450
Country  Bosnia and Herzegovina
Entity  Republika Srpska
Government
 • Mayor Mileva Komlenović (Bosnia and Herzegovina)
Area
 • Total 681,15 km2 (26,299 sq mi)
Population (2013 census)
 • Total 2,240
 • Density 3,3/km2 (90/sq mi)
Time zone CET (UTC+1)
 • Summer (DST) CEST (UTC+2)
Area code(s) 57
Website http://www.kalinovik.net

Kalinovik (Serbian Cyrillic: Калиновик) is a town and municipality in the Republika Srpska entity of Bosnia and Herzegovina. Kalinovik is located about 40 kilometres south of Sarajevo, in the middle of one of the karstic landscapes characteristic of the region. Water erosion has left the calcareous plateaus strewn with dolines and poljes (sinkholes and flat-floored depressions).

The municipality has a population of only 2,500, down from 4,657 in 1991. The municipality adjoins the municipality of Konjic, with which the boundary also forms part of the Inter-Entity Boundary Line (IEBL) between the two constituent entities of Bosnia and Herzegovina.

Kalinovik is located about 70 kilometres south of Sarajevo, in the middle of one of the Karstic landscapes characteristic of the region. The calcareous plateaus, eaten into by water, are strewn with valleys or fields, types of sinkhole-like lunar craters.

The municipality adjoins the municipality of Konjic. The towns of Konjic and Kalinovik are connected by an asphalt road. Communications were disrupted when the bridge over the Ljuta river at Dindo was destroyed in autumn 1995, in the last months of the war, but were restored after a replacement bridge was constructed in 2002.

The boundary between the municipalities of Konjic and Kalinovik also forms part of the Inter-Entity Boundary Line (IEBL) between the two constituent entities of Bosnia and Herzegovina.

Climate in this area has mild differences between highs and lows, and there is adequate rainfall year round. The Köppen Climate Classification subtype for this climate is "Cfb" (Marine West Coast Climate/Oceanic climate).


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