The May Sho’ate (also called Argak'a) is a river of the Nile basin. Rising in the mountains of Dogu’a Tembien in northern Ethiopia, it flows southward to empty finally in Giba and Tekezé River.[1]

May Sho’ate
The May Sho’ate River in its catchment
May Sho'ate is located in Ethiopia
May Sho'ate
May Sho’ate River in Dogu’a Tembien
Location
CountryEthiopia
RegionTigray Region
District (woreda)Dogu’a Tembien
Physical characteristics
SourceMay Ntebteb
 • locationZenaqo in Ayninbirkekin municipality
 • elevation2,500 m (8,200 ft)
MouthMay Zegzeg River
 • location
May Addi Abagie, at the border of Mika'el Abiy and Haddinnet municipalities
 • coordinates
13°38′38″N 39°11′38″E / 13.644°N 39.194°E / 13.644; 39.194
 • elevation
2,270 m (7,450 ft)
Length1.9 km (1.2 mi)
Width 
 • average5 m (16 ft)
Basin features
River systemSeasonal/permanent river
LandmarksIlias’ Stone
WaterfallsMay Ntebteb
TopographyMountains and deep gorges
The river in the radial drainage network of Dogu’a Tembien

Characteristics edit

It is a confined ephemeral river with an average slope gradient of 121 metres per kilometre. With its tributaries, the river has cut a deep gorge.[2]

May Zegzeg Integrated Catchment Management Project edit

As part of outreach accompanying research in Dogu'a Tembien, the May Zegzeg Integrated Catchment Management Project was set up in 2004 in the catchment of the May Zegzeg River by researchers in cooperation with ADCS, a local NGO. There was a particular focus on the May Sho’ate subcatchment. The project included the implementation of conservation techniques to increase water infiltration and conserve the soil. The objective was to improve the livelihood of the communities of Harena, Hech'i and Addi Qolqwal as well as to demonstrate and promote global catchment management in the district.[3] The results of the implementation of site-specific conservation techniques aimed at increasing water infiltration and conserving soil were particularly monitored in the headwaters at May Sho'ate: dry masonry stone bunds,[4] check dams in gullies,[5] and the set-aside of degraded rangelands which resulted in exclosures.[6]

Flash floods and flood buffering edit

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]

 
May Sho’ate catchment

The magnitude of floods in this river has however been decreased due to interventions in the catchment by the May Zegzeg project, and other community activities. On the steep slopes, exclosures have been established; the dense vegetation largely contributes to enhanced infiltration, less flooding and better baseflow.[7] Physical conservation structures such as stone bunds[8][9] and check dams also intercept runoff.[5][10]

Irrigated agriculture edit

 
May Sho’ate dam

Besides springs and reservoirs, irrigation is strongly dependent on the river's baseflow. Such irrigated agriculture is important in meeting the demands for food security and poverty reduction.[2] Irrigated lands near springs that became strong after conservation activities:[1]

  • Zenaqo in the upper catchment
  • May Addi Abagiè, near the confluence of May Sho’ate and May Harena
 
Irrigation near the confluence of May Sho’ate and May Harena

Boulders and pebbles in the river bed edit

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.[11]

Research catchment edit

Given its representativeness for the wider northern Ethiopian Highlands and the proximity to Hagere Selam town, various research undertakings took place along May Sho’ate and in its catchment. These studies were particularly related to:

Natural boundary edit

During its course, this river constitutes the borders between Ayninbirkekin and Mika'el Abiy municipalities|.[1]

Trekking along the river edit

 
Ilias’ stone along May Sho’ate river bed

Trekking routes have been established across and along this river.[36] The tracks are not marked on the ground but can be followed using downloaded .GPX files.[37]

  • Trek 12, across the river and its upper catchment near Addi Qolqwal village
  • Trek 12V, across the river and its lower catchment near Hech'i and Harena villages

See also edit

References edit

  1. ^ a b c Jacob, M. and colleagues (2019). Geo-trekking map of Dogu'a Tembien (1:50,000). In: Geo-trekking in Ethiopia's Tropical Mountains - The Dogu'a Tembien District. SpringerNature. ISBN 978-3-030-04954-6.
  2. ^ a b c Amanuel Zenebe, and colleagues (2019). The Giba, Tanqwa and Tsaliet rivers in the headwaters of the Tekezze basin. In: Geo-trekking in Ethiopia's Tropical Mountains - The Dogu'a Tembien District. SpringerNature. doi:10.1007/978-3-030-04955-3_14. ISBN 978-3-030-04954-6. S2CID 199099067.
  3. ^ Reubens, B. and colleagues (2019). Research-based development projects in Dogu'a Tembien. In: Geo-trekking in Ethiopia's Tropical Mountains - The Dogu'a Tembien District. SpringerNature. ISBN 978-3-030-04954-6.
  4. ^ Nyssen, Jan; Poesen, Jean; Gebremichael, Desta; Vancampenhout, Karen; d'Aes, Margo; Yihdego, Gebremedhin; Govers, Gerard; Leirs, Herwig; Moeyersons, Jan; Naudts, Jozef; Haregeweyn, Nigussie; Haile, Mitiku; Deckers, Jozef (2007). "Interdisciplinary on-site evaluation of stone bunds to control soil erosion on cropland in Northern Ethiopia" (PDF). Soil and Tillage Research. 94 (1): 151–163. doi:10.1016/j.still.2006.07.011. hdl:1854/LU-378900.
  5. ^ a b c Nyssen, J.; Veyret-Picot, M.; Poesen, J.; Moeyersons, J.; Haile, Mitiku; Deckers, J.; Govers, G. (2004). "The effectiveness of loose rock check dams for gully control in Tigray, Northern Ethiopia". Soil Use and Management. 20: 55–64. doi:10.1111/j.1475-2743.2004.tb00337.x. S2CID 98547102.
  6. ^ Descheemaeker, K. and colleagues (2006). "Sediment deposition and pedogenesis in exclosures in the Tigray Highlands, Ethiopia". Geoderma. 132 (3–4): 291–314. Bibcode:2006Geode.132..291D. doi:10.1016/j.geoderma.2005.04.027.
  7. ^ Descheemaeker, K. and colleagues (2006). "Runoff on slopes with restoring vegetation: A case study from the Tigray highlands, Ethiopia". Journal of Hydrology. 331 (1–2): 219–241. doi:10.1016/j.still.2006.07.011. hdl:1854/LU-378900.
  8. ^ Nyssen, Jan; Poesen, Jean; Gebremichael, Desta; Vancampenhout, Karen; d'Aes, Margo; Yihdego, Gebremedhin; Govers, Gerard; Leirs, Herwig; Moeyersons, Jan; Naudts, Jozef; Haregeweyn, Nigussie; Haile, Mitiku; Deckers, Jozef (2007). "Interdisciplinary on-site evaluation of stone bunds to control soil erosion on cropland in Northern Ethiopia" (PDF). Soil and Tillage Research. 94 (1): 151–163. doi:10.1016/j.still.2006.07.011. hdl:1854/LU-378900.
  9. ^ Gebeyehu Taye and colleagues (2015). "Evolution of the effectiveness of stone bunds and trenches in reducing runoff and soil loss in the semi-arid Ethiopian highlands". Zeitschrift für Geomorphologie. 59 (4): 477–493. Bibcode:2015ZGm....59..477T. doi:10.1127/zfg/2015/0166.
  10. ^ Etefa Guyassa and colleagues (2017). "Effects of check dams on runoff characteristics along gully reaches, the case of Northern Ethiopia". Journal of Hydrology. 545 (1): 299–309. Bibcode:2017JHyd..545..299G. doi:10.1016/j.jhydrol.2016.12.019. hdl:1854/LU-8518957.
  11. ^ Sembroni, A.; Molin, P.; Dramis, F. (2019). Regional geology of the Dogu'a Tembien massif. In: Geo-trekking in Ethiopia's Tropical Mountains — The Dogu'a Tembien District. SpringerNature. ISBN 978-3-030-04954-6.
  12. ^ Nyssen, Jan; Poesen, Jean; Haile, Mitiku; Moeyersons, Jan; Deckers, Jozef (2000). "Tillage erosion on slopes with soil conservation structures in the Ethiopian highlands". Soil and Tillage Research. 57 (3): 115–127. doi:10.1016/S0167-1987(00)00138-0.
  13. ^ Nyssen, J.; Haile, Mitiku; Poesen, J.; Deckers, J.; Moeyersons, J. (2006). "Removal of rock fragments and its effect on soil loss and crop yield, Tigray, Ethiopia". Soil Use and Management. 17 (3): 179–187. doi:10.1111/j.1475-2743.2001.tb00025.x. S2CID 98532199.
  14. ^ Nyssen, Jan; Moeyersons, Jan; Poesen, Jean; Deckers, Jozef; Mitiku Haile (2003). "The environmental significance of the remobilisation of ancient mass movements in the Atbara–Tekeze headwaters, Northern Ethiopia". Geomorphology. 49 (3–4): 303–322. Bibcode:2003Geomo..49..303N. doi:10.1016/S0169-555X(02)00192-7.
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  18. ^ Gebrernichael, Desta; Nyssen, J.; Poesen, J.; Deckers, J.; Haile, Mitiku; Govers, G.; Moeyersons, J. (2005). "Effectiveness of stone bunds in controlling soil erosion on cropland in the Tigray Highlands, northern Ethiopia". Soil Use and Management. 21 (3): 287–297. doi:10.1111/j.1475-2743.2005.tb00401.x. S2CID 95931760.
  19. ^ Nyssen, J.; Vandenreyken, H.; Poesen, J.; Moeyersons, J.; Deckers, J.; Haile, Mitiku; Salles, C.; Govers, G. (2005). "Rainfall erosivity and variability in the Northern Ethiopian Highlands". Journal of Hydrology. 311 (1–4): 172–187. Bibcode:2005JHyd..311..172N. doi:10.1016/j.jhydrol.2004.12.016.
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  36. ^ Description of trekking routes in Dogu'a Tembien. In: Geo-trekking in Ethiopia's Tropical Mountains - The Dogu'a Tembien District. SpringerNature. 2019. ISBN 978-3-030-04954-6.
  37. ^ Public GPS traces tagged with nyssen-jacob-frankl | OpenStreetMap