Moulin de Tallené river
Also known as: le Moulin de Tallené
The Moulin de Tallené (also known as le Moulin de Tallené) is a European river flowing through France. As of 2026-10-15, the Moulin de Tallené was flowing at about 0.734 m³/s at the Le Blavet à Plélauff - Bon-Repos gauge.
- Canonical name
- Moulin de Tallené
- Local names / aliases
- le Moulin de Tallené
- Countries
- France
- Maximum upstream drainage area
- 2,054 km²
- Mapped river length
- 89.7 km
- Gauging stations
- 4
- Latest measured discharge
- 0.734 m³/s (Le Blavet à Plélauff - Bon-Repos, 2026-10-15)
Gauging stations on the Moulin de Tallené
The following 4 gauging stations report discharge for the Moulin de Tallené, 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 |
|---|---|---|---|---|---|---|---|---|---|
| Le Blavet à Plélauff - Bon-Repos | France | 0.734 | Much below normal64% below the historic median | daily mean | Donnée brute | Hub'Eau Hydrométrie | 48.213, -3.131 | source | |
| Le Blavet à Neulliac - Le Stumo | France | 2.953 | — | daily mean | Donnée brute | Hub'Eau Hydrométrie | 48.143, -3.005 | source | |
| Le Moulin de Tallené [Le Sebrevet] à Quistinic - Pont er Garrec | France | 0.082 | Much below normal71% below the historic median | daily mean | Donnée brute | Hub'Eau Hydrométrie | 47.906, -3.201 | source | |
| Le Blavet à Languidic - Craninen [Etiage] | France | 3.553 | — | daily mean | Donnée brute | Hub'Eau Hydrométrie | 47.856, -3.212 | source |
Related rivers
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.