| Godew | |
|---|---|
 | |
  Godew | |
| Coordinates | 13°26′38″N 39°32′43″E / 13.44388992°N 39.54534603°E |
| Type | Freshwater artificial lake |
| Basin countries | Ethiopia |
| Surface elevation | 2,280 m (7,480 ft) |
| Settlements | Ashegoda |
Godew is a reservoir located in the Inderta woreda of the Tigray Region in Ethiopia. The earthen dam that holds the reservoir was built in 1990 by the Tigray Bureau of Agriculture and Natural Resources. [1]
The catchment of the reservoir is 4 km2 large, with a perimeter of 10.45 km (of which 326 metres is occupied by the dam) and a length of 3260 metres. The reservoir suffers from rapid siltation. [2] [3] The lithology of the catchment is Mekelle Dolerite and 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]
- ^ a b De Wit, Joke (2003). Stuwmeren in Tigray (Noord-Ethiopië): kenmerken, sedimentatie en sediment-bronnen. Unpub. M.Sc. thesis. Department of Geography, K.U.Leuven.
- ^ Nigussie Haregeweyn, and colleagues (2006). "Reservoirs in Tigray: characteristics and sediment deposition problems". Land Degradation and Development. 17: 211–230. doi: 10.1002/ldr.698. S2CID 129834993.
- ^ Vanmaercke, M. and colleagues (2019). "Sediment Yield and Reservoir Siltation in Tigray". Geo-trekking in Ethiopia's Tropical Mountains. GeoGuide. Cham (CH): Springer Nature. pp. 345–357. doi: 10.1007/978-3-030-04955-3_23. ISBN 978-3-030-04954-6. S2CID 199112876.
- ^ Nigussie Haregeweyn, and colleagues (2008). "Sediment yield variability in Northern Ethiopia: A quantitative analysis of its controlling factors". Catena. 75 (1): 65–76. Bibcode: 2008Caten..75...65H. doi: 10.1016/j.catena.2008.04.011.
| Godew | |
|---|---|
|
| |
Godew | |
| Coordinates | 13°26′38″N 39°32′43″E / 13.44388992°N 39.54534603°E |
| Type | Freshwater artificial lake |
| Basin countries | Ethiopia |
| Surface elevation | 2,280 m (7,480 ft) |
| Settlements | Ashegoda |
Godew is a reservoir located in the Inderta woreda of the Tigray Region in Ethiopia. The earthen dam that holds the reservoir was built in 1990 by the Tigray Bureau of Agriculture and Natural Resources. [1]
The catchment of the reservoir is 4 km2 large, with a perimeter of 10.45 km (of which 326 metres is occupied by the dam) and a length of 3260 metres. The reservoir suffers from rapid siltation. [2] [3] The lithology of the catchment is Mekelle Dolerite and 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]
- ^ a b De Wit, Joke (2003). Stuwmeren in Tigray (Noord-Ethiopië): kenmerken, sedimentatie en sediment-bronnen. Unpub. M.Sc. thesis. Department of Geography, K.U.Leuven.
- ^ Nigussie Haregeweyn, and colleagues (2006). "Reservoirs in Tigray: characteristics and sediment deposition problems". Land Degradation and Development. 17: 211–230. doi: 10.1002/ldr.698. S2CID 129834993.
- ^ Vanmaercke, M. and colleagues (2019). "Sediment Yield and Reservoir Siltation in Tigray". Geo-trekking in Ethiopia's Tropical Mountains. GeoGuide. Cham (CH): Springer Nature. pp. 345–357. doi: 10.1007/978-3-030-04955-3_23. ISBN 978-3-030-04954-6. S2CID 199112876.
- ^ Nigussie Haregeweyn, and colleagues (2008). "Sediment yield variability in Northern Ethiopia: A quantitative analysis of its controlling factors". Catena. 75 (1): 65–76. Bibcode: 2008Caten..75...65H. doi: 10.1016/j.catena.2008.04.011.