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Ombla
EntityQ931551· pop 14· linked from 114 articles

The Ombla is a short river in Croatia, northeast of Dubrovnik. Its course is approximately long, and it empties into the Rijeka Dubrovačka, a ria of the Adriatic Sea near Komolac in Dubrovnik-Neretva County. Rijeka Dubrovačka is actually a ria, a flooded river valley formed through changes in sea surface elevation on a geologic time scale. The river rises as a karst spring fed by groundwater replenished by Trebišnjica, which is an influent stream flowing in Popovo Polje, in the immediate hinterland of the Ombla. The elevation difference between the river's source and its mouth is just over . T

Key facts

River.name
Ombla
River.image
Izvor Omble.JPG
River.image_caption
The Ombla at Komolac, Croatia
River.map
Ombla catchment.svg
River.map_caption
Ombla catchment area: ; Inset map: location of the area within Croatia and Bosnia-Herzegovina
River.subdivision_type1
Country
River.subdivision_name1
Croatia
River.subdivision_type3
Region
River.subdivision_name3
Dalmatia
River.subdivision_type4
District
River.subdivision_name4
Dubrovnik-Neretva County
River.length_km
0.03
River.discharge1_location
source
River.source1
Golubov Kamen
River.source1_location
Komolac, Croatia
River.mouth
Adriatic Sea
River.mouth_location
Komolac, Croatia
River.basin_size_km2
600

via Wikipedia infobox

Wikidata facts

Image
Dubrovnik-bridge.jpg
Length
3
Show 4 more facts
watershed area
600
Commons category
Ombla
discharge
239
name
Ombla
Sources (1)

via Wikidata · CC0

~11 min read

Article

7 sections
Contents
  • Source and course
  • Drainage basin
  • Economy
  • Proposed power plant
  • Etymology
  • See also
  • References

The Ombla is a short river in Croatia, northeast of Dubrovnik. Its course is approximately long, and it empties into the Rijeka Dubrovačka, a ria of the Adriatic Sea near Komolac in Dubrovnik-Neretva County. Rijeka Dubrovačka is actually a ria, a flooded river valley formed through changes in sea surface elevation on a geologic time scale. The river rises as a karst spring fed by groundwater replenished by Trebišnjica, which is an influent stream flowing in Popovo Polje, in the immediate hinterland of the Ombla. The elevation difference between the river's source and its mouth is just over . The average discharge of the river is per second. The drainage basin of the Ombla encompasses and, besides the short surface course, includes only groundwater flow.

The Ombla is used as a source of drinking water for Dubrovnik's water supply network, and construction of a hydroelectric power plant has been planned for the past two decades. , the plans entail construction of a subsurface reservoir and a 68 megawatt power plant. The plan sparked controversy amid doubts raised with respect to environmental protection and biodiversity management, technical and financial feasibility, and procedural problems related to the project. A particular concern expressed was that the underground reservoir might trigger earthquakes.

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4 mapped locations

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