fbpx
Wikipedia

Ch'eqofo River

Ch’eqofo is a river of the Nile basin. Rising in the mountains of Dogu’a Tembien in northern Ethiopia, it flows southwestward to empty finally in Giba and Tekezé River.[1]

Ch’eqofo
Ch’eqofo River in Dogu’a Tembien
Location
CountryEthiopia
RegionTigray Region
District (woreda)Dogu’a Tembien
Physical characteristics
Source 
 • locationAddilal
 • elevation2,330 m (7,640 ft)
MouthGiba River
 • location
Down from Miqmat’ Awra in Emni Ankelalu municipality
 • coordinates
13°40′26″N 39°24′40″E / 13.674°N 39.411°E / 13.674; 39.411Coordinates: 13°40′26″N 39°24′40″E / 13.674°N 39.411°E / 13.674; 39.411
 • elevation
1,825 m (5,988 ft)
Length13 km (8.1 mi)
Width 
 • average15 m (49 ft)
Basin features
River systemSeasonal/permanent river
TopographyMountains and deep gorges
The river in the radial drainage network of Dogu’a Tembien

Characteristics

It is a confined ephemeral river, locally meandering in its narrow alluvial plain, with an average slope gradient of 39 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 this river has however been decreased due to interventions in the catchment. On 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]

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.[8]

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 gorge and overnight in small caves. The gorges are particularly attractive as a transhumance destination zone, because there is water and good growth of semi-natural vegetation.[10]

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 24 follows the southern water divide, parallel to the river, and gives panoramic views over the Ch’eqofo valley. In the rainy season, flash floods may occur and it is advised not to follow the river bed.[13]

See also

References

  1. ^ 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 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.
  3. ^ 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.
  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". Soil and Tillage Research. 94 (1): 151–163. doi:10.1016/j.still.2006.07.011. hdl:1854/LU-378900.
  5. ^ 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. doi:10.1127/zfg/2015/0166.
  6. ^ 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.
  7. ^ 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. doi:10.1016/j.jhydrol.2016.12.019. hdl:1854/LU-8518957.
  8. ^ 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.
  9. ^ Moeyersons, J. and colleagues (2006). "Age and backfill/overfill stratigraphy of two tufa dams, Tigray Highlands, Ethiopia: Evidence for Late Pleistocene and Holocene wet conditions". Palaeogeography, Palaeoclimatology, Palaeoecology. 230 (1–2): 162–178. Bibcode:2006PPP...230..165M. doi:10.1016/j.palaeo.2005.07.013.
  10. ^ Nyssen, Jan; Descheemaeker, Katrien; Zenebe, Amanuel; Poesen, Jean; Deckers, Jozef; Haile, Mitiku (2009). "Transhumance in the Tigray highlands (Ethiopia)". Mountain Research and Development. 29 (3): 255–264. doi:10.1659/mrd.00033.
  11. ^ 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.
  12. ^ Public GPS traces tagged with nyssen-jacob-frankl | OpenStreetMap
  13. ^ Nyssen, Jan (2019). "Logistics for the Trekker in a Rural Mountain District of Northern Ethiopia". Geo-trekking in Ethiopia's Tropical Mountains. GeoGuide. Springer-Nature. pp. 537–556. doi:10.1007/978-3-030-04955-3_37. ISBN 978-3-030-04954-6.

eqofo, river, eqofo, river, nile, basin, rising, mountains, dogu, tembien, northern, ethiopia, flows, southwestward, empty, finally, giba, tekezé, river, eqofoch, eqofo, river, dogu, tembienlocationcountryethiopiaregiontigray, regiondistrict, woreda, dogu, tem. Ch eqofo is a river of the Nile basin Rising in the mountains of Dogu a Tembien in northern Ethiopia it flows southwestward to empty finally in Giba and Tekeze River 1 Ch eqofoCh eqofo River in Dogu a TembienLocationCountryEthiopiaRegionTigray RegionDistrict woreda Dogu a TembienPhysical characteristicsSource locationAddilal elevation2 330 m 7 640 ft MouthGiba River locationDown from Miqmat Awra in Emni Ankelalu municipality coordinates13 40 26 N 39 24 40 E 13 674 N 39 411 E 13 674 39 411 Coordinates 13 40 26 N 39 24 40 E 13 674 N 39 411 E 13 674 39 411 elevation1 825 m 5 988 ft Length13 km 8 1 mi Width average15 m 49 ft Basin featuresRiver systemSeasonal permanent riverTopographyMountains and deep gorges The river in the radial drainage network of Dogu a Tembien Contents 1 Characteristics 2 Flash floods and flood buffering 3 Boulders and pebbles in the river bed 4 Transhumance towards the gorge 5 Trekking along the river 6 See also 7 ReferencesCharacteristics EditIt is a confined ephemeral river locally meandering in its narrow alluvial plain with an average slope gradient of 39 metres per kilometre With its tributaries the river has cut a deep gorge 2 Flash floods and flood buffering EditRunoff 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 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 Boulders and pebbles in the river bed EditBoulders 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 8 Lower basalt Amba Aradam Formation Mekelle Dolerite Antalo Limestone Quaternary freshwater tufa 9 Transhumance towards the gorge EditTranshumance 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 gorge and overnight in small caves The gorges are particularly attractive as a transhumance destination zone because there is water and good growth of semi natural vegetation 10 Trekking along the river EditTrekking 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 24 follows the southern water divide parallel to the river and gives panoramic views over the Ch eqofo valley In the rainy season flash floods may occur and it is advised not to follow the river bed 13 See also EditList of Ethiopian riversReferences Edit 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 a b 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 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 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 Soil and Tillage Research 94 1 151 163 doi 10 1016 j still 2006 07 011 hdl 1854 LU 378900 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 fur Geomorphologie 59 4 477 493 doi 10 1127 zfg 2015 0166 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 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 doi 10 1016 j jhydrol 2016 12 019 hdl 1854 LU 8518957 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 Moeyersons J and colleagues 2006 Age and backfill overfill stratigraphy of two tufa dams Tigray Highlands Ethiopia Evidence for Late Pleistocene and Holocene wet conditions Palaeogeography Palaeoclimatology Palaeoecology 230 1 2 162 178 Bibcode 2006PPP 230 165M doi 10 1016 j palaeo 2005 07 013 Nyssen Jan Descheemaeker Katrien Zenebe Amanuel Poesen Jean Deckers Jozef Haile Mitiku 2009 Transhumance in the Tigray highlands Ethiopia Mountain Research and Development 29 3 255 264 doi 10 1659 mrd 00033 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 Public GPS traces tagged with nyssen jacob frankl OpenStreetMap Nyssen Jan 2019 Logistics for the Trekker in a Rural Mountain District of Northern Ethiopia Geo trekking in Ethiopia s Tropical Mountains GeoGuide Springer Nature pp 537 556 doi 10 1007 978 3 030 04955 3 37 ISBN 978 3 030 04954 6 Retrieved from https en wikipedia org w index php title Ch 27eqofo River amp oldid 1018863413, wikipedia, wiki, book, books, library,

article

, read, download, free, free download, mp3, video, mp4, 3gp, jpg, jpeg, gif, png, picture, music, song, movie, book, game, games.