May Meqa Explained

May Meqa
Pushpin Map:Ethiopia
Pushpin Map Caption:May Meqa River in Dogu’a Tembien
Subdivision Type1:Country
Subdivision Type2:Region
Subdivision Name2:Tigray Region
Subdivision Type3:District (woreda)
Subdivision Name3:Dogu’a Tembien
Length:5.5km (03.4miles)
Width Avg:8m (26feet)
Source1:May Tsahli
Source1 Location:Miheno in Selam municipality
Source1 Elevation:2390m (7,840feet)
Mouth:Tinsehe River
Mouth Location:Tinsehe in Selam municipality
Mouth Coordinates:13.695°N 39.19°W
Mouth Elevation:2170m (7,120feet)
River System:Seasonal river
Bridges:Tinsehe (rural road)
Custom Label:Topography
Custom Data:Mountains and deep gorges

The May Meqa is a river of the Nile basin. Rising in the mountains of Dogu’a Tembien in northern Ethiopia, it flows northward to empty finally in the Weri’i and Tekezé River.[1]

Characteristics

It is a confined ephemeral river, locally meandering in its narrow alluvial plain, with an average slope gradient of 40 metres per kilometre.[2] The May Meqa changes names along is course: the upper part, in Miheno is called May Tsahli, the middle part in Addi Werho May Meqa, and the lower part, near the mouth May Mugda. The mouth is just 50 metres upstream from Tinsehe waterfall

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 other 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] Efforts have been done to establish biological control measurements (tree plantation) in the river bed.[8]

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.[9]

Trekking along the river

Trekking routes have been established across and along this river.[11] The tracks are not marked on the ground but can be followed using downloaded .GPX files.[12] Trek 23 follows the river over most of its length.

See also

Notes and References

  1. Book: Jacob . M. and colleagues . Geo-trekking map of Dogu'a Tembien (1:50,000). In: Geo-trekking in Ethiopia's Tropical Mountains - The Dogu'a Tembien District . 2019 . SpringerNature . 978-3-030-04954-6 .
  2. Book: Amanuel Zenebe . and colleagues . Geo-trekking in Ethiopia's Tropical Mountains . The Giba, Tanqwa and Tsaliet Rivers in the Headwaters of the Tekezze Basin . GeoGuide . 2019 . 215–230 . SpringerNature . 978-3-030-04954-6 . 10.1007/978-3-030-04955-3_14 . 199099067 .
  3. Descheemaeker. K. and colleagues. Runoff on slopes with restoring vegetation: A case study from the Tigray highlands, Ethiopia. . Journal of Hydrology . 2006 . 331 . 1–2 . 219–241 . 10.1016/j.still.2006.07.011. 1854/LU-378900 . free .
  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. Interdisciplinary on-site evaluation of stone bunds to control soil erosion on cropland in Northern Ethiopia. . Soil and Tillage Research . 2007 . 94 . 1 . 151–163 . 10.1016/j.still.2006.07.011. 1854/LU-378900. free.
  5. Gebeyehu Taye and colleagues. Evolution of the effectiveness of stone bunds and trenches in reducing runoff and soil loss in the semi-arid Ethiopian highlands. . Zeitschrift für Geomorphologie. 2015 . 59 . 4 . 477–493 . 10.1127/zfg/2015/0166.
  6. Nyssen. J.. Veyret-Picot. M.. Poesen. J.. Moeyersons. J.. Haile. Mitiku. Deckers. J.. Govers. G.. The effectiveness of loose rock check dams for gully control in Tigray, Northern Ethiopia. . Soil Use and Management . 2004 . 20 . 55–64 . 10.1111/j.1475-2743.2004.tb00337.x. 98547102.
  7. Etefa Guyassa and colleagues. Effects of check dams on runoff characteristics along gully reaches, the case of Northern Ethiopia. . Journal of Hydrology . 2017 . 545 . 1 . 299–309 . 10.1016/j.jhydrol.2016.12.019. 1854/LU-8518957 . free .
  8. Tree species selection for land rehabilitation in Ethiopia: from fragmented knowledge to an integrated multi-criteria decision approach https://link.springer.com/article/10.1007/s10457-011-9381-8
  9. Book: Sembroni . A. . Molin . P. . Dramis . F. . Regional geology of the Dogu'a Tembien massif. In: Geo-trekking in Ethiopia's Tropical Mountains — The Dogu'a Tembien District . 2019 . SpringerNature . 978-3-030-04954-6 .
  10. Moeyersons . J. and colleagues . Age and backfill/overfill stratigraphy of two tufa dams, Tigray Highlands, Ethiopia: Evidence for Late Pleistocene and Holocene wet conditions. . Palaeogeography, Palaeoclimatology, Palaeoecology . 2006 . 230 . 1–2 . 162–178 . 2006PPP...230..165M . 10.1016/j.palaeo.2005.07.013 .
  11. Book: Description of trekking routes in Dogu'a Tembien. In: Geo-trekking in Ethiopia's Tropical Mountains - The Dogu'a Tembien District . GeoGuide . 2019 . SpringerNature . 10.1007/978-3-030-04955-3 . 978-3-030-04954-6 . 199294303 .
  12. Web site: Public GPS Traces tagged with nyssen-jacob-frankl.

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