Shimbula
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| Shimbula | |
|---|---|
  Shimbula River in Dogu’a Tembien | |
| Location | |
| Country | Ethiopia |
| Region | Tigray Region |
| District (woreda) | Dogu’a Tembien |
| Physical characteristics | |
| Source | |
| • location | Mesenqoy in Addi Azmera municipality |
| • elevation | 2,312 m (7,585 ft) |
| Mouth | Hurura River |
• location | Tukhul in Addi Azmera municipality |
• coordinates | 13°38′10″N 39°19′41″E / 13.636°N 39.328°E |
• elevation | 1,915 m (6,283 ft) |
| Length | 10.5 km (6.5 mi) |
| Width | |
| • average | 10 m (33 ft) |
| Basin features | |
| Progression | Hurura→ Giba→ Tekezé→ Atbarah→ Nile→ Mediterranean Sea |
| River system | Seasonal river |
| Bridges | Tukhul |
| Topography | Mountains and deep gorges |
The Shimbula is a river of the Nile basin. Rising in the mountains of Dogu’a Tembien in northern Ethiopia, it flows southwestward to empty finally in Giba and Tekezé River.[1]
It is a confined ephemeral river, locally meandering in its narrow alluvial plain, with an average slope gradient of 38 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. On 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]
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.[8]
- Lower basalt
- Amba Aradam Formation
- Mekelle Dolerite
- Antalo Limestone
- Quaternary freshwater tufa[9]