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Kodori (river)


FieldValue
nameKodori
mapKodori River Watershed.jpg
map_size270
map_captionKodori River watershed ([Interactive map](https://mghydro.com/watersheds/shared/123B73.html))
source1Kelasuri First / Kelasuri Second
source1_locationMain Caucasian Range
Caucasus Major
source1_elevation1380 m
mouthGeorgia/Abkhazia
mouth_locationBlack Sea
mouth_coordinates
mouth_elevation0 ft
subdivision_type1Country
subdivision_name1Georgia/Abkhazia
length105 km
discharge1_avg144 m3/s
basin_size2051 km2

Caucasus Major

The Kodori (კოდორი; ) is one of the two longest rivers of Abkhazia, along with the Bzyb. It is formed by the joining of the rivers Sakeni and Gvandra. The Kodori is first among Abkhazia's rivers with respect to average annual discharge at 144 m3/s and drainage basin area at 2051 km2. It is second after the Bzyb with respect to length at 105 km when combined with the Sakeni.

Course

The Kodori River originates at the confluence of the glacial-fed Sakeni and Gvandra rivers in the Caucasus Mountains, at an elevation of approximately 1,380 meters. It flows swiftly through steep, rocky terrain in its upper course, moving through subalpine meadows and forested areas. As it descends, the river enters a narrow gorge, eventually widening into a floodplain near its mouth. The river empties into the Black Sea along the Abkhazian coastline.

Hydrology

The river has an average annual discharge of about 144 cubic meters per second, making it the largest in Abkhazia by flow. Its catchment area spans roughly 2,051 square kilometers. The river is fed by a combination of snowmelt, rainfall, and glacial runoff, leading to seasonal surges in volume during the spring and summer months.

Studies on the river’s estuarine zone have shown that the Kodori plays a major role in transporting sediment to the Black Sea, particularly during periods of high discharge. These sediment inputs affect the morphology of the coastline and the ecological conditions of the nearshore marine environment.

Ecology

The Kodori River supports a range of aquatic habitats that vary according to elevation and water chemistry. Its upper sections are oligotrophic, with cold, clear waters supporting limited but specialized biota. In contrast, the estuarine zone near the mouth hosts a broader diversity of species. A 2015 study reported the presence of 84 species of phytoplankton, 19 species of zooplankton, and 105 species of benthic invertebrates in the river’s estuary.{{cite journal|last1=Mingazova

Strategic importance

The Kodori Valley has been a significant location in the context of regional geopolitics. The upper part of the valley, known as "Upper Abkhazia," remained under Georgian government control until the 2008 conflict between Georgia and Russian-backed Abkhaz forces. The valley was the site of the 2006 Kodori crisis and other strategic military operations in the ongoing dispute over Abkhazia.

References

References

  1. {{Abkhazia-note
  2. Dbar, Roman. (1999). "The Abkhazians - a handbook". Curzon.
  3. (2015). "Conditions of estuarine rivers of the Abkhazia Republic and their impact on the Black Sea coast". Marine Biological Journal.
  4. Stepanenko, Y.. (2018). "Sediment Dynamics of the Kodori Estuary". Ecology and Noospherology.
  5. (2015). "Ecological features of Kodori estuarine river: hydrology, plankton and sediment transport". Marine Biological Journal.
  6. (2015). "Impact of estuarine rivers on sediment transport along the Black Sea coast of Abkhazia". Marine Biological Journal.
  7. (2020). "Current state and long-term changes in the mesozooplankton community of the Ukrainian and Georgian parts of the Black Sea as indicators of its ecological status". Biosystems Diversity.
  8. Antidze, Margarita. (28 July 2006). "Kodori Gorge Under Georgian Control". The Moscow Times.
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