Mzymta River
Geography
The source of the Mzymta is in Lake Verkhny Kardyvach in Western Caucasus, at the height of 2,980 metres (9,780 ft). The upper course of the river is located within the Caucasus Zapovednik. The Mzymta flows in a narrow valley through Lake Kardyvach and forms several waterfalls, the biggest of which is Izumrudny (Emerald), 15 metres (49 ft). Downstream of Lake Kardyvach, the river flows west and enters Sochi National Park. The banks are covered with beech forests and chestnuts, and also ancient Ubykh gardens with wild pear, walnut and chestnut. In Esto-Sadok and Krasnaya Polyana the Mzymta flows through the first urban area, where some of the events of the 2014 Winter Olympics took place. Downstream it turns south. The Mzymta comes through Akhshtyr and Dzykhra gorges, popular tourist attractions. The Mzymta enters the Black Sea in Adler, where the rest of the Winter Olympics took place. At the mouth, there is a big talus train, dividing into branches across the floodplains. Mzymta carries out to sea large amounts of silt. Mineral springs are also found in the catchment basin. The river is fed by spring tides and rain freshets.
The Mzymta is a floatable river, and the popular attraction is rafting. Krasnopolyanskaya hydroelectric power station has a reservoir with a daily streamflow regulation.
Average intensity of flow
- Krasnaya Polyana: 33.2 cubic metres per second (1,170 cu ft/s)
- Kepsh: 45.6 cubic metres per second (1,610 cu ft/s) (max 764 cubic metres per second (27,000 cu ft/s))
Major inflows
Inhabited localities
- Estosadok
- Krasnaya Polyana
- Chvizhepse
- Kepsha
- Monastyr
- Galitsyno
- Kazachy Brod
- Vysokoye
- Moldovka
- Adler
References
- ^ Река Мзымта (in Russian). State Water Register of Russia. Retrieved 1 February 2014.