Gereb Awso Explained
Gereb Awso |
Coords: | 13.4296°N 39.5534°W |
Type: | Freshwater artificial lake |
Basin Countries: | Ethiopia |
Area: | 0.0212km2 |
Volume: | 0.119e6m3 |
Elevation: | 2290m (7,510feet) |
Pushpin Map: | Ethiopia |
Pushpin Label Position: | right |
Cities: | Kwiha |
Gereb Awso is a reservoir located in the Inderta woreda of the Tigray Region in Ethiopia. The earthen dam that holds the reservoir was built in 1998 by SAERT.[1]
Dam characteristics
- Dam height: 10.5 metres
- Dam crest length: 196 metres
- Spillway width: 3 metres
Capacity
- Original capacity: 118944 m3
- Dead storage: 3944 m3
- Reservoir area: 2.12 ha
Irrigation
- Designed irrigated area: 9 ha
- Actual irrigated area in 2002: 5 ha
Environment
The catchment of the reservoir is 1.21 km2 large, with a perimeter of 4.62 km and a length of 1780 metres. The reservoir suffers from rapid siltation.[2] [3] The lithology of the catchment is Agula Shale.[1] Part of the water that could be used for irrigation is lost through seepage; the positive side-effect is that this contributes to groundwater recharge.[4]
Notes and References
- Book: De Wit . Joke . Stuwmeren in Tigray (Noord-Ethiopië): kenmerken, sedimentatie en sediment-bronnen. Unpub. M.Sc. thesis . 2003 . Department of Geography, K.U.Leuven.
- Nigussie Haregeweyn . and colleagues . Reservoirs in Tigray: characteristics and sediment deposition problems . Land Degradation and Development . 2006 . 17 . 211–230 . 10.1002/ldr.698 . 129834993 . free .
- Book: Vanmaercke. M. and colleagues . Geo-trekking in Ethiopia's Tropical Mountains . Sediment Yield and Reservoir Siltation in Tigray . GeoGuide . 2019 . Springer Nature . Cham (CH) . 345–357. 10.1007/978-3-030-04955-3_23 . 978-3-030-04954-6 . 199112876 . https://link.springer.com/chapter/10.1007/978-3-030-04955-3_23.
- Nigussie Haregeweyn . and colleagues . Sediment yield variability in Northern Ethiopia: A quantitative analysis of its controlling factors . Catena . 2008 . 75 . 1 . 65–76 . 10.1016/j.catena.2008.04.011 . 2008Caten..75...65H .