Armancon river
Also known as: L'Armancon
The Armancon (also known as L'Armancon) is a European river flowing through France. As of 2026-10-15, the Armancon was flowing at about 0.107 m³/s at the La Brenne à Montbard gauge.
- Canonical name
- Armancon
- Local names / aliases
- L'Armancon
- Countries
- France
- Maximum upstream drainage area
- 2,182 km²
- Mapped river length
- 103.3 km
- Gauging stations
- 4
- Latest measured discharge
- 0.107 m³/s (La Brenne à Montbard, 2026-10-15)
Gauging stations on the Armancon
The following 4 gauging stations report discharge for the Armancon, 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 |
|---|---|---|---|---|---|---|---|---|---|
| La Brenne à Montbard | France | 0.107 | Much below normal96% below the historic median | daily mean | Donnée brute | Hub'Eau Hydrométrie | 47.623, 4.324 | source | |
| L'Armançon à Aisy-sur-Armançon - aval | France | 0.38 | Much below normal92% below the historic median | daily mean | Donnée brute | Hub'Eau Hydrométrie | 47.668, 4.233 | source | |
| [La fosse Dionne] à Tonnerre | France | 0.014 | Much below normal91% below the historic median | daily mean | Donnée brute | Hub'Eau Hydrométrie | 47.857, 3.971 | source | |
| L'Armançon à Tronchoy | France | 1.438 | Much below normal77% below the historic median | daily mean | Donnée brute | Hub'Eau Hydrométrie | 47.914, 3.939 | 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.