Saha ( Spanish: Río Saja ) - a river in northern Spain , flowing through the territory of the autonomous community of Cantabria . It originates on the northern slope of the Sierra del Cordel (mankomunidat Campoo-Kabuerniga) [1] . It flows into the Bay of Biscay , forming the mouth of the San Martín de la Arena.
| Saha | |
|---|---|
| Spanish Río Saja | |
| Characteristic | |
| Length | 67 km |
| Swimming pool | 442 km² |
| Watercourse | |
| Source | river confluence: Cobra and Diablo |
| • Location | Sierra del cordel |
| • Height | 800 m |
| • Coordinates | |
| Mouth | Bay of Biscay |
| • Location | Suances , Ria San Martín de la Arena |
| • Height | 0 m |
| • Coordinates | |
| Location | |
| A country |
|
| Region | Cantabria |
General characteristics
The river is 67 km long [2] . It flows through the territory of the province of Cantabria, forming the valley of Kabuerniga and Cabezon de la Sal. The area of the Sakha Basaya basin is about 1025.5 km² [1] , which makes it the largest in the autonomous community (occupies about 20% of the territory).
Sahi River Basin (442 km², before confluence with the Besaia River)
Saha Bessaya Basin
Current
The Sakha River is formed on the northern slope of the Sierra del Cordel, as a result of the confluence of two rivers, Cobra and Diablo, at an altitude of about 800 m above sea level [1] . In the area of the settlement of El Toho, the Argos River flows into it. Near Cabezona de la Sal, it turns east, where on the territory of Torrelavega it unites with the river Besaia. Then it moves north, flowing into the Bay of Biscay in the Suances area, forming the Ria San Martín de la Arena [3] .
Notes
- ↑ 1 2 3 1.1. Características generales de la cuenca (Spanish) (link not available) . dma.medioambientecantabria.es. Date of treatment September 16, 2013. Archived October 29, 2013.
- ↑ Río Saja (Spanish) (unavailable link) . chcantabrico.es. Date of treatment September 16, 2013. Archived on October 5, 2013.
- ↑ Río Saja (Spanish) (unavailable link) . portalcantabria.e. Date of treatment September 16, 2013. Archived October 2, 2013.