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| == Course == | == Course == | ||
| {{unreferenced section|date= December 2024}} | |||
| The stream originates from ] in the upper Valtournenche. Along its course, it receives several tributaries that originate from the numerous glaciers in the valley. It flows through the length of the Valtournenche, passing through the Gouffre des Busserailles, and finally empties into the Dora Baltea near ]. | The stream originates from ] in the upper Valtournenche. Along its course, it receives several tributaries that originate from the numerous glaciers in the valley. It flows through the length of the Valtournenche, passing through the Gouffre des Busserailles, and finally empties into the Dora Baltea near ]. | ||
Latest revision as of 09:21, 26 December 2024
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| Marmore | |
|---|---|
 | |
| Location | |
| Country | Italy |
| Region | Aosta Valley |
| Physical characteristics | |
| Source | |
| • location | Lake Goillet |
| Length | 30.7 km (19.1 mi) |
| Basin size | 207.32 km (80.05 sq mi) |
| Basin features | |
| Progression | Dora Baltea→ Po→ Adriatic Sea |
The Marmore is a stream which flows through the Valtournenche in the Aosta Valley, Italy. It is a tributary of the Dora Baltea.
Course
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The stream originates from Lake Goillet in the upper Valtournenche. Along its course, it receives several tributaries that originate from the numerous glaciers in the valley. It flows through the length of the Valtournenche, passing through the Gouffre des Busserailles, and finally empties into the Dora Baltea near Châtillon.
The stream is used for hydroelectric power generation and supplies the Châtillon power plant in Châtillon as well as the Covalou power plant in Antey-Saint-André.
Notes
- "Implementazione della Direttiva Quadro sulle Acque sul territorio della Valle d'Aosta" (PDF) (in Italian). ARPA Valle d'Aosta. Retrieved 2024-12-25.
External links
Media related to Marmore (creek) at Wikimedia Commons