Lim'at
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Lim’at is a '' tabia'' in the
Dogu'a Tembien Dogu'a Tembien (, "Upper Tembien", sometimes transliterated as Degua Tembien) is a woreda in Tigray Region, Ethiopia. It is named in part after the former province of Tembien. Nowadays, the mountainous district is part of the Southeastern Tigray ...
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 is ...
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 Maygwa village, located approximately 8 km to the southwest of the ''woreda'' town Hagere Selam.


Geography

The ''tabia'' stretches down from the Tsatsen plateau (2810 m a.s.l.), across the main road towards Zeleqwa (Upper Tanqwa) river (2270 m a.s.l.).


Geology

From the higher to the lower locations, the following geological formations are present: * Upper basalt * Interbedded lacustrine deposits * Lower basalt *
Amba Aradam Formation The Amba Aradam Formation is a Cretaceous sandstone formation in Ethiopia. It is up to 200 metres thick, for instance in the Degua Tembien district. As fossils are absent, the age of the Amba Aradam Formation was interpreted based on the age of a ...
*
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 a ...
*
Quaternary The Quaternary ( ) is the current and most recent of the three periods of the Cenozoic Era in the geologic time scale of the International Commission on Stratigraphy (ICS). It follows the Neogene Period and spans from 2.58 million years ...
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. Alluv ...
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 travertine. ...


Geomorphology and soils

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 n ...
unit is the Hagere Selam Highlands. Corresponding soil types are: * 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, alternat ...
) * 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, alternat ...
, 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, alternat ...
) ** Shallow stony dark
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 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
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 ...
y 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 soi ...
)


Climate and hydrology


Climate and meteorology

The rainfall pattern shows a very high seasonality with 70 to 80% of the annual rain falling in July and August. Mean temperature in Maygwa is 17 °C, oscillating between average daily minimum of 9.4 °C and maximum of 24.4 °C. The contrasts between day and night air temperatures are much larger than seasonal contrasts.


Rivers

The Giba River's tributary, the Tanqwa is the most important river in the surroundings of the ''tabia''. It flows towards Tekezze River and further on to the
Nile The Nile, , Bohairic , lg, Kiira , Nobiin language, Nobiin: Áman Dawū is a major north-flowing river in northeastern Africa. It flows into the Mediterranean Sea. The Nile is the longest river in Africa and has historically been considered ...
. The rivers have incised deep gorges which characterise the landscape. The drainage network of the ''tabia'' is organised as follows: * Giba River ** Zeleqwa River, in ''tabias''
Melfa The Melfa is a river in Lazio, Italy. It rises in the Monti della Meta, flows south-west for about and joins the Liri near San Giovanni Incarico.''Carta stradale: Lazio 1:200000''. Istituto Geografico DeAgostini. . The source of the Melfa iss ...
and Lim’at, which becomes Ruba Dirho in
Aregen Aregen is a ''tabia'' or municipality in the Dogu'a Tembien district of the Tigray Region of Ethiopia. The ''tabia'' centre is in Addi Gotet village, located approximately to the west-southwest of the ''woreda'' town Hagere Selam. Geography ...
and
Degol Woyane Degol Woyane is a ''tabia'' or municipality in the Dogu'a Tembien district of the Tigray Region of Ethiopia. It includes Dabba Selama, the oldest monastery of Ethiopia, and the most inaccessible in the world. The ''tabia'' centre is in Zala villa ...
, and
Tanqwa Tanqwa is a river of northern Ethiopia. Rising in the mountains of Dogu’a Tembien (2510 metres above sea level), it flows westward to Giba River which empties finally in the Tekezé River. Hydrography It is a confined river, locally mea ...
River, in the ''woredas''
Kola Tembien Kola Tembien (, "Lower Tembien") is a woreda in Tigray Region, Ethiopia. It is named in part after the former province of Tembien. Part of the Mehakelegnaw Zone, Kola Tembien is bordered on the south by Abergele, on the west by the Tekezé River ...
and
Abergele (woreda) Tanqua Abergele ( ti, ጣንቋ ኣበርገለ, amh, አበርገሌ) is one of the Districts of Ethiopia, or ''woredas'', in the Tigray Region of Ethiopia. Part of the Mehakelegnaw Zone, Abergele is bordered on the south by the Wag Hemra Zone ...
***
Adawro River Adawro is a torrent of the Nile basin. Rising on the Ts’ats’en plateau of Dogu’a Tembien in northern Ethiopia, it flows northward to empty finally in Giba and Tekezé River. Characteristics It is a confined bedrock river, with an ave ...
, in ''tabia'' Lim’at ***
Arwadito Arwadito is a torrent of the Nile basin. Rising on the Ts’ats’en plateau of Dogu’a Tembien in northern Ethiopia, it flows northward to empty finally in Giba and Tekezé River. Characteristics It is a confined bedrock river, with an a ...
River, in ''tabia'' Lim’at ***
May Qoqah May Qoqah is a river of the Nile basin. Rising on the Ts’ats’en plateau of Dogu’a Tembien in northern Ethiopia, it flows northward to empty finally in Giba and Tekezé River. Characteristics It is a confined bedrock river, with an ave ...
, in ''tabia'' Lim’at Whereas they are (nearly) dry during most of the year, during the main rainy season, these rivers carry high runoff discharges, sometimes in the form of
flash flood A flash flood is a rapid flooding of low-lying areas: washes, rivers, dry lakes and depressions. It may be caused by heavy rain associated with a severe thunderstorm, hurricane, or tropical storm, or by meltwater from ice or snow flowing o ...
s. Especially at the begin of the rainy season they are brown-coloured, evidencing high soil
erosion Erosion is the action of surface processes (such as water flow or wind) that removes soil, rock, or dissolved material from one location on the Earth's crust, and then transports it to another location where it is deposited. Erosion is distin ...
rates.


Springs

As there are no permanent rivers, the presence of springs is of utmost importance for the local people. The main springs in the ''tabia'' are: * Mhtsab Alabu in Adawro * Hamute


Water harvesting

In this area with rains that last only for a couple of months per year, reservoirs of different sizes allow harvesting runoff from the rainy season for further use in the dry season. * Traditional surface water harvesting ponds, particularly in places without permanent springs, called ''rahaya'' * ''Horoyo'', household ponds, recently constructed through campaigns


Settlements

The ''tabia'' centre Maygwa holds a few administrative offices, a health post, a primary school, and some small shops. Saturday is the market day. There are a few more primary schools across the ''tabia''. The main other populated places are: * Addi Gerahti * Hahawti * Agerbi’a * Adawro * Ksad Adawro


Vegetation and exclosures

The ''tabia'' holds several
exclosure An exclosure, in an area being used extensively for grazing, is a limited area from which unwanted browsing animals, such as domestic cattle or wildlife such as deer, are excluded by fencing or other means. Environmental protection Most commonl ...
s, areas that are set aside for regreening, such as Adawro exclosure. Wood harvesting and livestock range are not allowed there. Besides effects on
biodiversity Biodiversity or biological diversity is the variety and variability of life on Earth. Biodiversity is a measure of variation at the genetic (''genetic variability''), species (''species diversity''), and ecosystem (''ecosystem diversity'') l ...
,
water infiltration Infiltration is the process by which water on the ground surface enters the soil. It is commonly used in both hydrology and soil sciences. The infiltration capacity is defined as the maximum rate of infiltration. It is most often measured in meter ...
, protection from flooding,
sediment Sediment is a naturally occurring material that is broken down by processes of weathering and erosion, and is subsequently transported by the action of wind, water, or ice or by the force of gravity acting on the particles. For example, sand an ...
deposition,
carbon sequestration Carbon sequestration is the process of storing carbon in a carbon pool. Carbon dioxide () is naturally captured from the atmosphere through biological, chemical, and physical processes. These changes can be accelerated through changes in land ...
, people commonly have economic benefits from these exclosures through grass harvesting, beekeeping and other
non-timber forest product Non-timber forest products (NTFPs) are useful foods, substances, materials and/or commodities obtained from forests other than timber. Harvest ranges from wild collection to farming. They typically include game animals, fur-bearers, nuts, seed ...
s. The local inhabitants also consider it as “land set aside for future generations”.


Agriculture and 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 bot ...
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 ...
. The farmers have adapted their
cropping system The term cropping system refers to the crops, crop sequences and management techniques used on a particular agricultural field over a period of years. It includes all spatial and temporal aspects of managing an agricultural system. Historically, cro ...
s to the spatio-temporal variability in rainfall.


History and culture


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. ...
.


Religion

Most inhabitants are
Orthodox Christians Orthodoxy (from Greek: ) is adherence to correct or accepted creeds, especially in religion. Orthodoxy within Christianity refers to acceptance of the doctrines defined by various creeds and ecumenical councils in Antiquity, but different Churc ...
.


''Inda Siwa'', the local beer houses

In the main villages, there are traditional beer houses ('' Inda Siwa''), often in unique settings, where people socialise. Well known in the ''tabia'' are * Amete Kiros at Agerbi’a * Tekien Gebresellasie at Maygua * Tekien Alemayehu at Maygua


Roads and communication

The main road
Mekelle Mekelle ( ti, መቐለ, am, መቀሌ, mäqälle, mek’elē) or Mekele is a List of zones of Ethiopia, special zone and capital city, capital of the Tigray Region of Ethiopia. Mekelle was formerly the capital of Enderta province, Enderta Awrajj ...
Hagere Selam
Abiy Addi Abiy Addi (also spelled Abi Addi; Tigrigna ዓብዪ ዓዲ "Big town") is a town in central Tigray Region, Tigray, Ethiopia. Abiy Addi is at the southeastern edge of the Kola Tembien woreda, of which it is the capital. Overview The town is di ...
runs across the ''tabia''. There are regular bus services to these towns.


Tourism

Its mountainous nature and proximity to
Mekelle Mekelle ( ti, መቐለ, am, መቀሌ, mäqälle, mek’elē) or Mekele is a List of zones of Ethiopia, special zone and capital city, capital of the Tigray Region of Ethiopia. Mekelle was formerly the capital of Enderta province, Enderta Awrajj ...
make the ''tabia'' fit for tourism. As compared to many other mountain areas in
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 villages are quite accessible, and during walks visitors may be invited for coffee, lunch or even for an overnight stay in a rural homestead.


Geotouristic sites

The high variability of geological formations and the rugged topography invite for geological and geographic tourism or "geotourism". Geosites in the ''tabia'' include: * May Qoqah river with permanent
baseflow Baseflow (also called drought flow, groundwater recession flow, low flow, low-water flow, low-water discharge and sustained or fair-weather runoff) is the portion of the streamflow that is sustained between precipitation events, fed to streams by d ...
and
gully A gully is a landform created by running water, mass movement, or commonly a combination of both eroding sharply into soil or other relatively erodible material, typically on a hillside or in river floodplains or terraces. Gullies resemble lar ...
control structures (log dams and check dams) * Views on
Melfa The Melfa is a river in Lazio, Italy. It rises in the Monti della Meta, flows south-west for about and joins the Liri near San Giovanni Incarico.''Carta stradale: Lazio 1:200000''. Istituto Geografico DeAgostini. . The source of the Melfa iss ...
, with
debris flow Debris flows are geological phenomena in which water-laden masses of soil and fragmented rock rush down mountainsides, funnel into stream channels, entrain objects in their paths, and form thick, muddy deposits on valley floors. They generally ...
s * Adawro Ch’erkos church forest, dominated by Euphorbia candelabra * Views from Tsatsen plateau to the wider surroundings


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. * Trek 7, across the ''tabia'' to
Debre Sema'it Debar ( mk, Дебaр ; Albanian: ''Dibër''/''Dibra'' or ''Dibra e Madhe;'' ) is a city in the western part of North Macedonia, near the border with Albania, off the road from Struga to Gostivar. It is the seat of Debar Municipality. Debar ha ...
rock church, and on to
Abiy Addi Abiy Addi (also spelled Abi Addi; Tigrigna ዓብዪ ዓዲ "Big town") is a town in central Tigray Region, Tigray, Ethiopia. Abiy Addi is at the southeastern edge of the Kola Tembien woreda, of which it is the capital. Overview The town is di ...
* Trek 8, at the southeastern edge of the ''tabia'' over the Tsatsen plateau through Inda Maryam Qorar to Zeyi cave and on the Giba River gorge * Trek 20 follows May Qoqah River and then the deep Zeleqwa gorge


See also

*
Dogu'a Tembien Dogu'a Tembien (, "Upper Tembien", sometimes transliterated as Degua Tembien) is a woreda in Tigray Region, Ethiopia. It is named in part after the former province of Tembien. Nowadays, the mountainous district is part of the Southeastern Tigray ...
district.


References

{{ Tabias (municipalities) of Dogu’a Tembien Populated places in the Tigray Region Dogu'a Tembien