To install click the Add extension button. That's it.

The source code for the WIKI 2 extension is being checked by specialists of the Mozilla Foundation, Google, and Apple. You could also do it yourself at any point in time.

4,5
Kelly Slayton
Congratulations on this excellent venture… what a great idea!
Alexander Grigorievskiy
I use WIKI 2 every day and almost forgot how the original Wikipedia looks like.
Live Statistics
English Articles
Improved in 24 Hours
Added in 24 Hours
Languages
Recent
Show all languages
What we do. Every page goes through several hundred of perfecting techniques; in live mode. Quite the same Wikipedia. Just better.
.
Leo
Newton
Brights
Milds

From Wikipedia, the free encyclopedia

Addi Amharay
A lake with a rocky and green foreshore
Addi Amharay is located in Ethiopia
Addi Amharay
Addi Amharay
Coordinates13°24′18″N 39°34′24″E / 13.40500132°N 39.5733461°E / 13.40500132; 39.5733461
TypeReservoir
Basin countriesEthiopia
Surface area0.315 km2 (0.122 sq mi)
Water volume0.957×10^6 m3 (776 acre⋅ft)
Surface elevation2,320 m (7,610 ft)
SettlementsKwiha

Addi Amharay is a reservoir located in the Inderta woreda of the Tigray Region in Ethiopia. The earthen dam that holds the reservoir was built in 1997 by SAERT.[1]

Dam characteristics

  • Dam height: 14.7 metres
  • Dam crest length: 128 metres
  • Spillway width: 17 metres

Capacity

  • Original capacity: 957,000 m³
  • Dead storage: 175,000 m³
  • Reservoir area: 31.5 ha

In 2001, the life expectancy of the reservoir before it is filled with sediment was estimated at only 33 years.[1]

Irrigation

  • Designed irrigated area: 60 ha
  • Actual irrigated area in 2001: 5 ha

Environment

The catchment of the reservoir is 4.92 km2, with a perimeter of 9.62 km and a length of 3560 metres. The reservoir suffers from rapid siltation.[2] [3] The lithology of the catchment is Antalo Limestone 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]

References

  1. ^ a b c De Wit, Joke (2003). Stuwmeren in Tigray (Noord-Ethiopië): kenmerken, sedimentatie en sediment-bronnen. Unpub. M.Sc. thesis. Department of Geography, K.U.Leuven.
  2. ^ 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.
  3. ^ 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.
  4. ^ 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.
This page was last edited on 30 March 2024, at 09:19
Basis of this page is in Wikipedia. Text is available under the CC BY-SA 3.0 Unported License. Non-text media are available under their specified licenses. Wikipedia® is a registered trademark of the Wikimedia Foundation, Inc. WIKI 2 is an independent company and has no affiliation with Wikimedia Foundation.