Mika'el Abiy
From Wikipedia the free encyclopedia
Mika’el Abiy | |
---|---|
Coordinates: 13°37′N 39°12′E / 13.617°N 39.200°E | |
Country | Ethiopia |
Region | Tigray |
Zone | Debub Misraqawi (Southeastern) |
Woreda | Dogu’a Tembien |
Area | |
• Total | 33.76 km2 (13.03 sq mi) |
Elevation | 2,320 m (7,610 ft) |
Population (2007) | |
• Total | 5,698 |
• Density | 169/km2 (440/sq mi) |
Time zone | UTC+3 (EAT) |
Mika’el Abiy is a tabia or municipality in the Dogu’a Tembien district of the Tigray Region of Ethiopia. The tabia centre is in Megesta village, located approximately 7 km to the southeast of the woreda town Hagere Selam.
Geography
[edit]The tabia stretches down south of the main road towards Rubaksa, which is a wider area with several springs and traditional irrigation. The highest peak is Gumawta (2815 m a.s.l.) on the Tsatsen plateau and the lowest place Rubaksa (1920 m a.s.l.).
Geology and soils
[edit]Geological formations
[edit]From the higher to the lower locations, the following geological formations are present:[1]
- Upper basalt
- Interbedded lacustrine deposits
- Lower basalt
- Amba Aradam Formation
- Antalo Limestone
- Quaternary alluvium and freshwater tufa[2]
Soilscape
[edit]The main geomorphic units, with corresponding soil types are:[3][4]
- Hagere Selam Highlands, along the basalt and sandstone ridge
- Associated soil types
- Inclusions
- Rock outcrops and very shallow soils (Lithic Leptosol)
- Rock outcrops and very shallow soils on limestone (Calcaric Leptosol)
- Deep dark cracking clays with very good natural fertility, waterlogged during the wet season (Chromic Vertisol, Pellic Vertisol)
- Shallow stony dark loams on calcaric material (Calcaric Regosol, Calcaric Cambisol)
- Brown loamy soils on basalt with good natural fertility (Luvisol)
- Gently rolling Antalo Limestone plateau, holding cliffs and valley bottoms on limestone
- Associated soil types
- Inclusions
- Rock outcrops and very shallow soils (Lithic Leptosol)
- Shallow very stony loamy soil on limestone (Skeletic Calcaric Cambisol)
- Deep dark cracking clays with very good natural fertility, waterlogged during the wet season (Chromic Vertisol, Pellic Vertisol)
- Brown to dark sands and silt loams on alluvium (Vertic Fluvisol, Eutric Fluvisol, Haplic Fluvisol) and colluvium (Calcaric Regosol)
Springs
[edit]As there are no permanent rivers, the presence of springs is of utmost importance for the local people. The following are the main springs in the tabia:[5]
- May Zahla in Dingilet
- May Ayni in Rubaksa
Livelihood
[edit]The population lives essentially from crop farming, supplemented with off-season work in nearby towns. The land is dominated by farmlands which are clearly demarcated and are cropped every year. Hence the agricultural system is a permanent upland farming system, and the population are not nomads.[6]
Population
[edit]The tabia centre Megesta holds a few administrative offices and some small shops. The villages close to Hagere Selam (Dingilet and Harena) have established a new settlement, at the margin of Hagere Selam, where the inhabitants benefit from the proximity of the town.[5] The main other populated places in the tabia are:[7]
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Religion and churches
[edit]Most inhabitants are Orthodox Christians. The following churches are located in the tabia:
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Legends and myths
[edit]In Megesta, there is a strong story about the Queen of Sheba who was transformed in a snake; the track of the snake is represented by a line of trees up to now. In the northern part of Harena, called Argak'a, there is a large rock of more than 50 m2 - the story goes that a certain Ilias transported it up to there.[8]
History
[edit]The history of the tabia is strongly confounded with the history of Tembien.
Roads and communication
[edit]The main road Mekelle – Hagere Selam – Abiy Addi runs at the north and west of the tabia. Inhabitants mostly move on foot to Hagere Selam from where they can travel further. A rural access road links Hagere Selam to the main villages of Mika’el Abiy.
Schools
[edit]Almost all children of the tabia are schooled,[9] though in some schools there is lack of classrooms, directly related to the large intake in primary schools over the last decades.[10] Schools in the tabia include Selam Seret school.
Tourism
[edit]Its mountainous nature and proximity to Mekelle makes the tabia fit for tourism.[11]
Touristic attractions
[edit]- Dingilet waterfall
- Rubaksa irrigated gardens
- Gumawta peak
Geotouristic sites
[edit]The high variability of geological formations and the rugged topography invites for geological and geographic tourism or "geotourism".[12] Geosites in the tabia include:
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Trekking routes
[edit]Trekking routes have been established in this tabia.[13] The tracks are not marked on the ground but can be followed using downloaded .GPX files.[14]
- Route 10, from Haddush Addi, through T’eshi to Rubaksa (8 km, from the highest to the lowest places in the tabia)
- Route 11, from Megesta, through Harena to Hagere Selam (8 km)
- Route 16, from Rubaksa to Togogwa (7 km)
Inda Siwa, the local beer houses
[edit]In the main villages, there are traditional beer houses (Inda Siwa), often in unique settings, which are a good place for resting and chatting with the local people. Most renown in the tabia are[5]
- Letesillasie Gebrecherkos in Megesta village
- Amit Gebregziabher in Megesta village
- Tsehaynesh Tesfay in Megesta village
Accommodation and facilities
[edit]The facilities are very basic.[15] One may be invited to spend the night in a rural homestead or ask permission to pitch a tent. Hotels are available in Hagere Selam and Mekelle.
More detailed information
[edit]For more details on environment, agriculture, rural sociology, hydrology, ecology, culture, etc., see the overall page on the Dogu’a Tembien district.
Gallery
[edit]- A farmer ploughing at Haddush Addi.
- View towards Dingilet from Mt Gumawta.
- Waterfall in Dingilet.
References
[edit]- ^ 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, J.; Naudts, J.; De Geyndt, K.; Haile, Mitiku; Poesen, J.; Moeyersons, J.; Deckers, J. (2008). "Soils and land use in the Tigray highlands (Northern Ethiopia)". Land Degradation and Development. 19 (3): 257–274. doi:10.1002/ldr.840. S2CID 128492271.
- ^ Nyssen, Jan; Tielens, Sander; Gebreyohannes, Tesfamichael; Araya, Tigist; Teka, Kassa; Van De Wauw, Johan; Degeyndt, Karen; Descheemaeker, Katrien; Amare, Kassa; Haile, Mitiku; Zenebe, Amanuel; Munro, Neil; Walraevens, Kristine; Kindeya Gebrehiwot; Poesen, Jean; Frankl, Amaury; Tsegay, Alemtsehay; Deckers, Jozef (2019). "Understanding spatial patterns of soils for sustainable agriculture in northern Ethiopia's tropical mountains". PLOS ONE. 14 (10): e0224041. Bibcode:2019PLoSO..1424041N. doi:10.1371/journal.pone.0224041. PMC 6804989. PMID 31639144.
- ^ a b c What do we hear from the farmers in Dogu'a Tembien? [in Tigrinya]. Hagere Selam, Ethiopia. 2016. p. 100.
{{cite book}}
: CS1 maint: location missing publisher (link) - ^ Nyssen, J.; Naudts, J.; De Geyndt, K.; Haile, Mitiku; Poesen, J.; Moeyersons, J.; Deckers, J. (2008). "Soils and land use in the Tigray highlands (Northern Ethiopia)". Land Degradation and Development. 19 (3): 257–274. doi:10.1002/ldr.840. S2CID 128492271.
- ^ 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.
- ^ Seifu Gebreselassie; Lanckriet, S. (2019). Local myths in relation to the natural environment of Dogu'a Tembien. In: Geo-Trekking in Ethiopia's Tropical Mountains, the Dogu'a Tembien District. SpringerNature. ISBN 978-3-030-04954-6.
- ^ Socio-demographic profile, food insecurity and food-aid based response. In: Geo-trekking in Ethiopia's Tropical Mountains - The Dogu'a Tembien District. GeoGuide. SpringerNature. 2019. doi:10.1007/978-3-030-04955-3. ISBN 978-3-030-04954-6. S2CID 199294303.
- ^ Hartjen, Clayton A.; Priyadarsini, S. (2012), Hartjen, Clayton A.; Priyadarsini, S. (eds.), "Denial of Education", The Global Victimization of Children: Problems and Solutions, Boston, MA: Springer US, pp. 271–321, doi:10.1007/978-1-4614-2179-5_8, ISBN 978-1-4614-2179-5, retrieved 2023-10-12
- ^ Geo-trekking in Ethiopia's Tropical Mountains - The Dogu'a Tembien District. GeoGuide. SpringerNature. 2019. doi:10.1007/978-3-030-04955-3. ISBN 978-3-030-04954-6. S2CID 199294303.
- ^ Miruts Hagos and colleagues (2019). "Geosites, Geoheritage, Human-Environment Interactions, and Sustainable Geotourism in Dogu'a Tembien". Geo-trekking in Ethiopia's Tropical Mountains. GeoGuide. SpringerNature. pp. 3–27. doi:10.1007/978-3-030-04955-3_1. ISBN 978-3-030-04954-6. S2CID 199095921.
- ^ Nyssen, Jan (2019). "Description of Trekking Routes in Dogu'a Tembien". Geo-trekking in Ethiopia's Tropical Mountains. GeoGuide. Springer-Nature. pp. 557–675. doi:10.1007/978-3-030-04955-3_38. ISBN 978-3-030-04954-6. S2CID 199271514.
- ^ "Public GPS Traces tagged with nyssen-jacob-frankl".
- ^ 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. S2CID 199198251.