Kígyós-patak river
The Kígyós-patak is a European river flowing through Hungary. As of 2026-10-16, the Kígyós-patak was flowing at about 0.34 m³/s at the Veszprémgalsa gauge.
- Canonical name
- Kígyós-patak
- Countries
- Hungary
- Maximum upstream drainage area
- 1,943 km²
- Mapped river length
- 53 km
- Gauging stations
- 3
- Latest measured discharge
- 0.34 m³/s (Veszprémgalsa, 2026-10-16)
Gauging stations on the Kígyós-patak
The following 3 gauging stations report discharge for the Kígyós-patak, ordered downstream (largest catchment first). Discharge is in cubic metres per second (m³/s).
| Station | Country | Discharge (m³/s) | Historical Comparison | Observed | Measurement | Data quality | Provider | Lat, Lon | Source |
|---|---|---|---|---|---|---|---|---|---|
| Veszprémgalsa | Hungary | 0.34 | Normal26% above the historic median | instantaneous | operational open-data observation | Hungarian General Directorate of Water Management | 47.095, 17.267 | source | |
| Karakó | Hungary | 0.105 | Much below normal88% below the historic median | instantaneous | operational open-data observation | Hungarian General Directorate of Water Management | 47.12, 17.208 | source | |
| Mersevát | Hungary | 0.128 | Much below normal92% below the historic median | instantaneous | operational open-data observation | Hungarian General Directorate of Water Management | 47.289, 17.212 | source |
Related rivers
- Tisza
- Mureș
- Jászsági-főcsatorna
- Maros
- Nagykunsági-főcsatorna
- Hármas-Körös
- Szamos
- Sio
- Sajó
- Sebes-Körös
- Rába
- Kettős-Körös
Data, sources & timestamps
Geometry is the HydroRIVERS network (HydroSHEDS): European reaches with at least 500 km² of upstream catchment, merged into chains between confluences. Flow direction comes from the network itself; river names are the canonical English label joined from provider metadata and Natural Earth, with local-language aliases retained.
Discharge is normalised observed streamflow from official national hydrology providers, measured where a gauge sits on the river and interpolated between gauges. Pale/estimated values are derived from drainage area × the local specific discharge of nearby gauges and are never presented as measurements.