Emni Ankelalu is a tabia or municipality in the Dogu'a Tembien district of the Tigray Region of Ethiopia. The tabia centre is in Mitslal Afras village, located approximately 20 km to the east of the woreda town Hagere Selam.
The tabia a hilly limestone area, along Giba River, north and away from the main road. The highest peak is Miqmat' Awra hill that occupies the centre (2195 m a.s.l.) and the lowest place at the outlet of May Qarano to Giba river (1750 m a.s.l.).
The rainfall pattern shows a very high seasonality with 70 to 80% of the annual rain falling in July and August. Mean temperature in Mitslal Afras is 20.8 °C, oscillating between average daily minimum of 12.4 °C and maximum of 30.8 °C. The contrasts between day and night air temperatures are much larger than seasonal contrasts.[5]
In this area with rains that last only for a couple of months per year, the only permanent water is in Giba river. There are hardly any springs.[6] Hence, reservoirs of different sizes allow harvesting runoff from the rainy season for further use in the dry season.[7]
There are traditional surface water harvesting ponds, particularly in places without permanent springs, called rahaya, and also horoyo, household ponds, recently constructed through campaigns.[8]
A major change is the construction of Lake Giba, a 350 million m3 reservoir on the Giba river that will occupy the whole lower eastern side of the tabia. The reservoir is mainly intended to provide water to Mekelle. The lithology of the dam building site is Antalo Limestone.[9] Part of its water is anticipated to be lost through seepage;[10] the positive side-effect is that this will contribute to groundwater recharge and river baseflow in the downstream areas, which largely belong to tabiasAddi Azmera and Debre Nazret.[7] The lower villages of Emni Ankelalu will see their environment changed from dryland to lakeshore villages.
The tabia centre Mitslal Afras holds a few administrative offices, a health post, a primary school, and some small shops. There are a few more primary schools across the tabia. The main other populated places are:[11]
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.[12] The farmers have adapted their cropping systems to the spatio-temporal variability in rainfall.[13]
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 is Kndahafti Mezegebe's inn at Mitslal Afras.[6]
Almost all children of the tabia are schooled,[14] though in some schools there is lack of classrooms, directly related to the large intake in primary schools over the last decades.[15] Schools in the tabia include Mitslal Afras school.
The high variability of geological formations and the rugged topography invites for geological and geographic tourism or "geotourism".[17] Geosites in the tabia include:
Confluence of Sulluh and Genfel rivers, inside deep gorges, called "Shugu'a Shugu'i"
May Qarano tufa dam (now occupied by the Giba dam building works)
Birdwatching (for the species, see the main Dogu'a Tembien page) can be done particularly in exclosures and forests. The following bird-watching sites have been inventoried[18] in the tabia and mapped.[11]
Trekking route 24 has been established in this tabia.[19] It follows the Giba and Suluh gorges upstream along the rivers, and then continues westbound over Miqmat' Awra hill. Once the Lake Giba will be filled, it will be impossible to visit these gorges. The track is not marked on the ground but can be followed using downloaded .GPX files.[20]
The facilities are very basic.[21] 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.
^Tefera, M.; Chernet, T.; Haro, W. Geological Map of Ethiopia (1:2,000,000). Addis Ababa, Ethiopia: Ethiopian Institute of Geological Survey.
^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.
^Gebremedhin Berhane, and colleagues (2013). "Geological challenges in constructing the proposed Geba dam site, northern Ethiopia". Bulletin of Engineering Geology and the Environment. 72 (3–4): 339–352. doi:10.1007/s10064-013-0480-9. S2CID128713402. ProQuest1655734342.
^Gebremedhin Berhane, and colleagues (2013). "Water leakage investigation of micro-dam reservoirs in Mesozoic sedimentary sequences in Northern Ethiopia". Journal of African Earth Sciences. 79: 98–110. Bibcode:2013JAfES..79...98B. doi:10.1016/j.jafrearsci.2012.10.004.
^Naudts, J (2002). Les Hautes Terres de Tembien, Tigré, Ethiopie; Résistance et limites d'une ancienne civilisation agraire; Conséquences sur la dégradation des terres [MSc dissertation]. CNEARC, Montpellier, France.
^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, ISBN978-1-4614-2179-5, retrieved 2023-10-13