| Ulluchay Ullu-Chay | |
|---|---|
Ulluchay River | |
| Etymology | Kumyk for "big river" |
| Native name | Уллучай (Russian) |
| Location | |
| Country | Russia |
| Federal subject | Dagestan |
| Region | Caucasus |
| Districts | Dakhadayevsky, Kaytagsky, and Derbentsky |
| Nearby village | Segeler |
| Physical characteristics | |
| Source | Springs near the northwestern end of the Kokmadag Range |
| • location | Dagestan, Russia |
| • coordinates | 41°59′53″N 47°20′05″E / 41.99806°N 47.33472°E |
| Mouth | Caspian Sea |
• location | Near Segeler, Dagestan, Russia |
• coordinates | 42°56′13″N 48°07′57″E / 42.93694°N 48.13250°E |
| Length | 111 km (69 mi) |
Basin size | 1,440 km2 (560 sq mi) |
| Discharge | |
| • average | 4.83 m3/s (171 cu ft/s) |
| • maximum | 366 m3/s (12,900 cu ft/s) |
| Basin features | |
| Tributaries | |
| • right | Kunki, Anklyuglyuchay, Jivus, Nakhalu, Shurkhla |
Ulluchay (Dargwa: ХулахӀеркӀ, Уллучай хӀеркӀ; Kumyk: Уллу Чай) is a river that flows through the Dakhadayevsky, Kaytagsky, and Derbentsky districts of Dagestan.
Ulluchay translates from the Kumyk language as “big river”: “ullu” means “big,” while “chay” means “river.”
The river is 111 km long, and its drainage basin covers an area of 1,440 km2.
The river originates from springs near the northwestern end of the Kokmadag Range and flows into the Caspian Sea near the village of Segeler.
The river is characterized by a flood regime during the warm season and low-water conditions in winter. The highest annual water discharge rates usually occur during periods of rainfall. Summer rain-induced floods sometimes reach catastrophic proportions. Mudflows have also been recorded along the river channel. The average annual discharge is 4.83 m3/s, while the maximum discharge is 366 m3/s.
The main tributaries are the Kunki, Anklyuglyuchay, Jivus, Nakhalu, Shurkhla, and others.
The river has been studied at stream gauging stations in Madzhalis and Berikey. Its waters are extensively used for irrigation, as a result of which the lower reaches of the river frequently experience a complete absence of flow.