Inda Anbesa
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| Inda Anbesa | |
|---|---|
 Inda Anbesa headwaters at Togogwa | |
  Inda Anbesa River in Dogu’a Tembien | |
| Etymology | "Lion home", after a local legend |
| Location | |
| Country | Ethiopia |
| Region | Tigray Region |
| District (woreda) | Dogu’a Tembien |
| Physical characteristics | |
| Source | May Togogwa |
| • location | Togogwa in Debre Nazret municipality |
| • elevation | 2,170 m (7,120 ft) |
| 2nd source | May Kebakebo |
| • location | Togogwa in Debre Nazret municipality |
| Mouth | Giba River |
• location | May Bilbil at the border of Dogu’a Tembien and Inderta |
• coordinates | 13°33′22″N 39°21′04″E / 13.556°N 39.351°E |
• elevation | 1,700 m (5,600 ft) |
| Length | 9 km (5.6 mi) |
| Width | |
| • average | 12 m (39 ft) |
| Basin features | |
| Progression | Giba→ Tekezé→ Atbarah→ Nile→ Mediterranean Sea |
| River system | Permanent river |
| Landmarks | Togogwa monastery |
| Topography | Mountains and deep gorges |
The Inda Anbesa is a river of the Nile basin. Rising in the mountains of Dogu’a Tembien in northern Ethiopia, it flows eastward to empty directly in the Giba and further in Tekezé River.[1]
The Inda Anbesa is a confined ephemeral river, locally meandering in its narrow alluvial plain, with an average slope gradient of 52 metres per kilometre. With its tributaries, the river has cut a deep gorge.[2]
Flash floods and flood buffering
Runoff mostly happens in the form of high runoff discharge events that occur in a very short period (called flash floods). These are related to the steep topography, often little vegetation cover and intense convective rainfall. The peaks of such flash floods have often a 50 to 100 times larger discharge than the preceding baseflow.[2] The magnitude of floods in this river has, however, been decreased due to interventions in the catchment. At Togogwa and on other steep slopes, exclosures have been established; the dense vegetation largely contributes to enhanced infiltration, less flooding and better baseflow.[3] Physical conservation structures such as stone bunds[4][5] and check dams also intercept runoff.[6][7]
Transhumance towards the gorge
Transhumance takes place in the summer rainy season, when the lands near the villages are occupied by crops. Young shepherds will take the village cattle down to the gorge and overnight in small caves. The gorges are particularly attractive as a transhumance destination zone, because there is water and good growth of semi-natural vegetation.[8]
Boulders and pebbles in the river bed
Boulders and pebbles encountered in the river bed can originate from any location higher up in the catchment. In the uppermost stretches of the river, only rock fragments of the upper lithological units will be present in the river bed, whereas more downstream one may find a more comprehensive mix of all lithologies crossed by the river. From upstream to downstream, the following lithological units occur in the catchment.[9]
- Antalo Limestone
- Quaternary freshwater tufa[10]