Kidane Mihret River Explained

Kidane Mihret River
Name Etymology:after the homonymous church
Pushpin Map:Ethiopia
Pushpin Map Caption:Kidane Mihret River in Dogu’a Tembien
Subdivision Type1:Country
Subdivision Name1:Ethiopia
Subdivision Type2:Region
Subdivision Name2:Tigray Region
Subdivision Type3:District (woreda)
Subdivision Name3:Dogu’a Tembien
Length:4.5km (02.8miles)
Width Avg:10m (30feet)
Source1:Waseiya
Source1 Location:Mahbere Sillasie municipality
Source1 Elevation:2280m (7,480feet)
Mouth:Tsaliet River
Mouth Location:near Ksad Korowya
Mouth Coordinates:13.699°N 39.1145°W
Mouth Elevation:1820m (5,970feet)
River System:Permanent river
Basin Landmarks:Awhi Dur forest
Waterfalls:Numerous rapids
Custom Label:Topography
Custom Data:Mountains and deep gorges

The Kidane Mihret 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 Wari and Tekezé River.[1]

Characteristics

It is a confined bedrock river, with an average slope gradient of 102 metres per kilometre. With its tributaries, the river has cut a deep gorge.[2]

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 to a certain extent buffered by the presence of the large Awhi Dur forest in its catchment. Also, 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]

Transhumance towards the gorge

Transhumance takes place in the summer rainy season, when the lands near the villages are occupied by crops. Young shepherds will take the village cattle down to the lower valley and overnight in small caves. The valley bottom is particularly attractive as a transhumance destination zone, because there is water and good growth of semi-natural vegetation.[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.[10] The tracks are not marked on the ground but can be followed using downloaded .GPX files.[11]

In the rainy season, flash floods may occur and it is advised not to follow the river bed. At times it may be impossible to cross the river in the rainy season.[12]

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 . 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 . 2019 . SpringerNature . 978-3-030-04954-6 . 10.1007/978-3-030-04955-3_14 .
  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. 2015ZGm....59..477T .
  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.
  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. 2017JHyd..545..299G . 1854/LU-8518957 . free .
  8. Transhumance in the Tigray highlands (Ethiopia) . Mountain Research and Development . 2009 . 29 . 3 . 255–264 . 10.1659/mrd.00033 . Nyssen . Jan . Descheemaeker . Katrien . Zenebe . Amanuel . Poesen . Jean . Deckers . Jozef . Haile . Mitiku . free . 1854/LU-854326 . free .
  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. Book: Description of trekking routes in Dogu'a Tembien. In: Geo-trekking in Ethiopia's Tropical Mountains – The Dogu'a Tembien District . 2019 . SpringerNature . 978-3-030-04954-6 .
  11. Web site: Public GPS Traces tagged with nyssen-jacob-frankl. OpenStreetMap.
  12. Book: Logistics for the Trekker in a Rural Mountain District of Northern Ethiopia. 2019 . Springer-Nature . 537–556 . 10.1007/978-3-030-04955-3_37 . Geo-trekking in Ethiopia's Tropical Mountains . GeoGuide . Nyssen . Jan . 978-3-030-04954-6 .

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