Mika’el Abiy is a ''tabia'' or municipality in the
Dogu’a Tembien district of the
Tigray Region
The Tigray Region, officially the Tigray National Regional State, is the northernmost regional state in Ethiopia. The Tigray Region is the homeland of the Tigrayan, Irob, and Kunama people. Its capital and largest city is Mekelle. Tigray ...
of
Ethiopia
Ethiopia, , om, Itiyoophiyaa, so, Itoobiya, ti, ኢትዮጵያ, Ítiyop'iya, aa, Itiyoppiya officially the Federal Democratic Republic of Ethiopia, is a landlocked country in the Horn of Africa. It shares borders with Eritrea to the ...
. The ''tabia'' centre is in Megesta village, located approximately 7 km to the southeast of the ''woreda'' town
Hagere Selam.
Geography
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
Geological formations
From the higher to the lower locations, the following geological formations are present:
*
Upper basalt
*
Interbedded lacustrine deposits
*
Lower basalt
*
Amba Aradam Formation
*
Antalo Limestone
The Antalo Limestone, also known as the Antalo Sequence, is a geological formation in Ethiopia. It is between 300 and 800 metres thick and comprises fossiliferous limestones and marls that were deposited in a reef. Marine microfossils have shown ...
*
Quaternary alluvium
Alluvium (from Latin ''alluvius'', from ''alluere'' 'to wash against') is loose clay, silt, sand, or gravel that has been deposited by running water in a stream bed, on a floodplain, in an alluvial fan or beach, or in similar settings. ...
and freshwater
tufa
Tufa is a variety of limestone formed when carbonate minerals precipitate out of water in unheated rivers or lakes. Geothermally heated hot springs sometimes produce similar (but less porous) carbonate deposits, which are known as travertin ...
Soilscape
The main
geomorphic
Geomorphology (from Ancient Greek: , ', "earth"; , ', "form"; and , ', "study") is the scientific study of the origin and evolution of topographic and bathymetric features created by physical, chemical or biological processes operating at or ...
units, with corresponding soil types are:
* Hagere Selam Highlands, along the basalt and sandstone ridge
** Associated soil types
*** shallow soils with high stone contents (Skeletic
Cambisol
A Cambisol in the World Reference Base for Soil Resources (WRB) is a soil in the beginning of soil formation. The horizon differentiation is weak. This is evident from weak, mostly brownish discolouration and/or structure formation in the soil pr ...
, Leptic
Cambisol
A Cambisol in the World Reference Base for Soil Resources (WRB) is a soil in the beginning of soil formation. The horizon differentiation is weak. This is evident from weak, mostly brownish discolouration and/or structure formation in the soil pr ...
, Skeletic
Regosol
A Regosol in the World Reference Base for Soil Resources (WRB) is very weakly developed mineral soil in unconsolidated materials. Regosols are extensive in eroding lands, in particular in arid and semi-arid areas and in mountain regions. Internat ...
)
*** moderately deep dark stony
clay
Clay is a type of fine-grained natural soil material containing clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4).
Clays develop plasticity when wet, due to a molecular film of water surrounding the clay par ...
s with good natural fertility (Vertic
Cambisol
A Cambisol in the World Reference Base for Soil Resources (WRB) is a soil in the beginning of soil formation. The horizon differentiation is weak. This is evident from weak, mostly brownish discolouration and/or structure formation in the soil pr ...
)
*** deep, dark cracking
clay
Clay is a type of fine-grained natural soil material containing clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4).
Clays develop plasticity when wet, due to a molecular film of water surrounding the clay par ...
s, temporarily
waterlogged during the wet season (Pellic
Vertisol
A vertisol, or vertosol, is a soil type in which there is a high content of expansive clay minerals, many of them known as montmorillonite, that form deep cracks in drier seasons or years. In a phenomenon known as argillipedoturbation, alternate ...
)
** Inclusions
*** Rock outcrops and very shallow soils (Lithic
Leptosol
A Leptosol in the World Reference Base for Soil Resources (WRB) is a very shallow soil over hard rock or a deeper soil that is extremely gravelly and/or stony. Leptosols cover approximately 1.7 billion hectares of the Earth's surface. They are ...
)
*** Rock outcrops and very shallow soils on limestone (Calcaric
Leptosol
A Leptosol in the World Reference Base for Soil Resources (WRB) is a very shallow soil over hard rock or a deeper soil that is extremely gravelly and/or stony. Leptosols cover approximately 1.7 billion hectares of the Earth's surface. They are ...
)
*** Deep dark cracking
clay
Clay is a type of fine-grained natural soil material containing clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4).
Clays develop plasticity when wet, due to a molecular film of water surrounding the clay par ...
s with very good natural fertility,
waterlogged during the wet season (Chromic
Vertisol
A vertisol, or vertosol, is a soil type in which there is a high content of expansive clay minerals, many of them known as montmorillonite, that form deep cracks in drier seasons or years. In a phenomenon known as argillipedoturbation, alternate ...
, Pellic
Vertisol
A vertisol, or vertosol, is a soil type in which there is a high content of expansive clay minerals, many of them known as montmorillonite, that form deep cracks in drier seasons or years. In a phenomenon known as argillipedoturbation, alternate ...
)
*** Shallow stony dark
loams on calcaric material (Calcaric
Regosol
A Regosol in the World Reference Base for Soil Resources (WRB) is very weakly developed mineral soil in unconsolidated materials. Regosols are extensive in eroding lands, in particular in arid and semi-arid areas and in mountain regions. Internat ...
, Calcaric
Cambisol
A Cambisol in the World Reference Base for Soil Resources (WRB) is a soil in the beginning of soil formation. The horizon differentiation is weak. This is evident from weak, mostly brownish discolouration and/or structure formation in the soil pr ...
)
*** Brown
loamy soils on basalt with good natural fertility (
Luvisol
Luvisols are a group of soils, comprising one of the 32 Reference Soil Groups in the international system of soil classification, the World Reference Base for Soil Resources The World Reference Base for Soil Resources (WRB) is an international so ...
)
* Gently rolling
Antalo Limestone
The Antalo Limestone, also known as the Antalo Sequence, is a geological formation in Ethiopia. It is between 300 and 800 metres thick and comprises fossiliferous limestones and marls that were deposited in a reef. Marine microfossils have shown ...
plateau, holding cliffs and valley bottoms on limestone
** Associated soil types
*** shallow stony soils with a dark surface horizon overlying calcaric material (Calcaric
Leptosol
A Leptosol in the World Reference Base for Soil Resources (WRB) is a very shallow soil over hard rock or a deeper soil that is extremely gravelly and/or stony. Leptosols cover approximately 1.7 billion hectares of the Earth's surface. They are ...
)
*** moderately deep dark stony
clay
Clay is a type of fine-grained natural soil material containing clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4).
Clays develop plasticity when wet, due to a molecular film of water surrounding the clay par ...
s with good natural fertility (Vertic
Cambisol
A Cambisol in the World Reference Base for Soil Resources (WRB) is a soil in the beginning of soil formation. The horizon differentiation is weak. This is evident from weak, mostly brownish discolouration and/or structure formation in the soil pr ...
)
*** deep, dark cracking
clay
Clay is a type of fine-grained natural soil material containing clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4).
Clays develop plasticity when wet, due to a molecular film of water surrounding the clay par ...
s on calcaric material (Calcaric
Vertisol
A vertisol, or vertosol, is a soil type in which there is a high content of expansive clay minerals, many of them known as montmorillonite, that form deep cracks in drier seasons or years. In a phenomenon known as argillipedoturbation, alternate ...
, Calcic
Vertisol
A vertisol, or vertosol, is a soil type in which there is a high content of expansive clay minerals, many of them known as montmorillonite, that form deep cracks in drier seasons or years. In a phenomenon known as argillipedoturbation, alternate ...
)
** Inclusions
*** Rock outcrops and very shallow soils (Lithic
Leptosol
A Leptosol in the World Reference Base for Soil Resources (WRB) is a very shallow soil over hard rock or a deeper soil that is extremely gravelly and/or stony. Leptosols cover approximately 1.7 billion hectares of the Earth's surface. They are ...
)
*** Shallow very stony
loamy soil on limestone (Skeletic Calcaric
Cambisol
A Cambisol in the World Reference Base for Soil Resources (WRB) is a soil in the beginning of soil formation. The horizon differentiation is weak. This is evident from weak, mostly brownish discolouration and/or structure formation in the soil pr ...
)
*** Deep dark cracking
clay
Clay is a type of fine-grained natural soil material containing clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4).
Clays develop plasticity when wet, due to a molecular film of water surrounding the clay par ...
s with very good natural fertility,
waterlogged during the wet season (Chromic
Vertisol
A vertisol, or vertosol, is a soil type in which there is a high content of expansive clay minerals, many of them known as montmorillonite, that form deep cracks in drier seasons or years. In a phenomenon known as argillipedoturbation, alternate ...
, Pellic
Vertisol
A vertisol, or vertosol, is a soil type in which there is a high content of expansive clay minerals, many of them known as montmorillonite, that form deep cracks in drier seasons or years. In a phenomenon known as argillipedoturbation, alternate ...
)
*** Brown to dark
sand
Sand is a granular material composed of finely divided mineral particles. Sand has various compositions but is defined by its grain size. Sand grains are smaller than gravel and coarser than silt. Sand can also refer to a textural class o ...
s and
silt loam
Loam (in geology and soil science) is soil composed mostly of sand (particle size > ), silt (particle size > ), and a smaller amount of clay (particle size < ). By weight, its mineral composition is about 40–40–20% concentration of sand–sil ...
s on
alluvium
Alluvium (from Latin ''alluvius'', from ''alluere'' 'to wash against') is loose clay, silt, sand, or gravel that has been deposited by running water in a stream bed, on a floodplain, in an alluvial fan or beach, or in similar settings. ...
(Vertic
Fluvisol
A fluvisol in the World Reference Base for Soil Resources (WRB) is a genetically young soil in alluvial deposits . Apart from river sediments, they also occur in lacustrine and marine deposits.
Fluvisols correlate with fluvents and fluvaquents ...
, Eutric
Fluvisol
A fluvisol in the World Reference Base for Soil Resources (WRB) is a genetically young soil in alluvial deposits . Apart from river sediments, they also occur in lacustrine and marine deposits.
Fluvisols correlate with fluvents and fluvaquents ...
, Haplic
Fluvisol
A fluvisol in the World Reference Base for Soil Resources (WRB) is a genetically young soil in alluvial deposits . Apart from river sediments, they also occur in lacustrine and marine deposits.
Fluvisols correlate with fluvents and fluvaquents ...
) and
colluvium
Colluvium (also colluvial material or colluvial soil) is a general name for loose, unconsolidated sediments that have been deposited at the base of hillslopes by either rainwash, sheetwash, slow continuous downslope creep, or a variable combinati ...
(Calcaric
Regosol
A Regosol in the World Reference Base for Soil Resources (WRB) is very weakly developed mineral soil in unconsolidated materials. Regosols are extensive in eroding lands, in particular in arid and semi-arid areas and in mountain regions. Internat ...
)
Springs
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:
* May Zahla in Dingilet
* May Ayni in Rubaksa
Livelihood
The population lives essentially from crop farming, supplemented with off-season work in nearby towns. The land is dominated by
farmland
Agricultural land is typically land ''devoted to'' agriculture, the systematic and controlled use of other forms of lifeparticularly the rearing of livestock and production of cropsto produce food for humans. It is generally synonymous with bo ...
s which are clearly demarcated and are cropped every year. Hence the
agricultural system
Agriculture or farming is the practice of cultivating plants and livestock. Agriculture was the key development in the rise of sedentary human civilization, whereby farming of domesticated species created food surpluses that enabled people to ...
is a permanent upland
farming system
Agriculture or farming is the practice of cultivating plants and livestock. Agriculture was the key development in the rise of sedentary human civilization, whereby farming of domesticated species created food surpluses that enabled people to ...
, and the population are not nomads.
Population
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.
The main other populated places in the ''tabia'' are:
Religion and churches
Most inhabitants are
Orthodox Christians. The following churches are located in the ''tabia'':
Legends and myths
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 m
2 - the story goes that a certain Ilias transported it up to there.
History
The history of the ''tabia'' is strongly confounded with the
history of Tembien
Tembien ( Tigrigna: ተምቤን) is a historic region in Tigray Region and former provinces of Ethiopia. It is a mountainous area of that country. During the reforms in 1994–95, the old provinces were replaced with regions, zones and woredas. ...
.
Roads and communication
The main road
Mekelle
Mekelle ( ti, መቐለ, am, መቀሌ, mäqälle, mek’elē) or Mekele is a special zone and capital of the Tigray Region of Ethiopia. Mekelle was formerly the capital of Enderta awraja in Tigray. It is located around north of the Ethiopi ...
–
Hagere Selam –
Abiy Addi
Abiy Addi (also spelled Abi Addi; Tigrigna ዓብዪ ዓዲ "Big town") is a town in central Tigray, Ethiopia. Abiy Addi is at the southeastern edge of the Kola Tembien woreda, of which it is the capital.
Overview
The town is divided into t ...
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
Almost all children of the ''tabia'' are schooled,
though in some schools there is lack of classrooms, directly related to the large intake in primary schools over the last decades. Schools in the ''tabia'' include Selam Seret school.
Tourism
Its mountainous nature and proximity to
Mekelle
Mekelle ( ti, መቐለ, am, መቀሌ, mäqälle, mek’elē) or Mekele is a special zone and capital of the Tigray Region of Ethiopia. Mekelle was formerly the capital of Enderta awraja in Tigray. It is located around north of the Ethiopi ...
makes the ''tabia'' fit for tourism.
Touristic attractions
* Dingilet waterfall
* Rubaksa irrigated gardens
* Gumawta peak
Geotouristic sites
The high variability of geological formations and the rugged topography invites for geological and geographic tourism or “geotourism”. Geosites in the ''tabia'' include:
Trekking routes
Trekking routes have been established in this ''tabia''. The tracks are not marked on the ground but can be followed using downloaded .GPX files.
* 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
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
* Letesillasie Gebrecherkos in Megesta village
* Amit Gebregziabher in Megesta village
* Tsehaynesh Tesfay in Megesta village
Accommodation and facilities
The facilities are very basic.
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
Mekelle ( ti, መቐለ, am, መቀሌ, mäqälle, mek’elē) or Mekele is a special zone and capital of the Tigray Region of Ethiopia. Mekelle was formerly the capital of Enderta awraja in Tigray. It is located around north of the Ethiopi ...
.
More detailed information
For more details on environment, agriculture, rural sociology, hydrology, ecology, culture, etc., see the overall page on the
Dogu’a Tembien district.
Gallery
File:Alaji_Basalts_provide_fertile_soils.jpg, A farmer ploughing at Haddush Addi.
File:Alaji Basalts near the peak of Gumawta Mt. in Dogu'a Tembien.jpg, View towards Dingilet from Mt Gumawta.
File:DingiletWaterfall.jpg, Waterfall in Dingilet.
References
{{ Tabias (municipalities) of Dogu’a Tembien
Dogu'a Tembien
Populated places in the Tigray Region