Edaga Hamus, Ethiopia
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Idaga Hamus (also called Edaga Hamus and Sewha Sa'isi'e) is a town in the Saesi Tsaedaemba woreda of Misraqawi Zone 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 ...
. It is located 97 kilometers north of
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 ...
on "National Road 1" (now
Ethiopian Highway 2 The A2 Highway is a trunk road in Ethiopia. It connects the capital Addis Ababa with Mekelle, as well as with Wukro, Adigrat, Axum, Shire and Humera. Ethiopian the A2 has a length of . Route Towns and cities along the A2 include, from north ...
), between Freweyni and Adigrat.


Geology and soils

The following geological formations are present in this locality: * Adigrat Sandstone *
Enticho Sandstone The Enticho Sandstone is a geological formation in north Ethiopia. It forms the lowermost sedimentary rock formation in the region and lies directly on the basement rocks. Enticho Sandstone consists of arenite that is rich in quartz. The formation ...
The main geomorphic units, with corresponding soil types are: *
Enticho Sandstone The Enticho Sandstone is a geological formation in north Ethiopia. It forms the lowermost sedimentary rock formation in the region and lies directly on the basement rocks. Enticho Sandstone consists of arenite that is rich in quartz. The formation ...
plateau ** Associated soil types *** shallow sandy soils with an indurated layer which prevents rooting and drainage (Petric Plinthosol) *** moderately deep, (light) brown, loamy to loamy sandy soil (Chromic
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 ...
, Arenic Luvisol, Arenic Lixisol) ** Inclusions *** complex of rock outcrops, very stony and very shallow soils ((Lithic) Leptosol) *** shallow, stony, dark greyish brown clay loams and sandy loams (Eutric Regosol and
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 ...
) ***
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 of floodplains with very high
watertable The water table is the upper surface of the zone of saturation. The zone of saturation is where the pores and fractures of the ground are saturated with water. It can also be simply explained as the depth below which the ground is saturated. T ...
with moderate to good natural fertility (Eutric
Gleysol A gleysol is a wetland soil (hydric soil) that, unless drained, is saturated with groundwater for long enough to develop a characteristic colour pattern. The pattern is essentially made up of reddish, brownish, or yellowish colours at surfaces o ...
, Gleyic
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 ...
) * Idaga Hamus highlands ** Associated soil types *** shallow, very stony, silt loamy to loamy soils (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) *** shallow, stony, dark greyish brown clay loams and sandy loams (Eutric Regosol and
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 ...
) *** sandy clay loams to sands developed on sandy colluvium (Eutric Arenosol, Regosol, Cambisol) ** Inclusions *** complex of rock outcrops, very stony and very shallow soils ((Lithic) Leptosol) *** 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, Pellic Vertisol) *** moderately deep, brown silty loamy to loamy soils (Eutric Luvisol)


Monuments

A number of rock-hewn churches have been reported near this town which include: Debre Zakarios Giyorgis and Cherqos, a collapsed one at Dengelat, Guwahigot Yesus and Yohannes."Local History in Ethiopia"
(pdf) The Nordic Africa Institute website (accessed 6 May 2008)
The contemporary church of Maryam Techot in this town is located on the top of a stepped
Aksumite The Kingdom of Aksum ( gez, መንግሥተ አክሱም, ), also known as the Kingdom of Axum or the Aksumite Empire, was a kingdom centered in Northeast Africa and South Arabia from Classical antiquity to the Middle Ages. Based primarily in wha ...
platform about 2 meters high and with dressed-stone corner blocks. A monolithic pillar and other carved fragments in the area may have been salvaged from the Aksumite structure which originally stood on this platform.


History

Records at the Nordic Africa Institute website provide details of the primary school in 1968. Idaga Hamus sheltered a significant number of refugees during the Eritrean-Ethiopian War of 1998-2000. During the 2020-2021 Tigray War, attacks were carried out on Idaga Hamus by the joint Ethiopian and Eritrean armies. On 18 December 2020, an EEPA report stated that 37 civilians were killed by Eritrean troops in Mariam Dengelat. This follows further reports of Ethiopian ENDF soldiers shooting at unarmed civilians.Situation Report EEPA HORN No. 30 - 19 December
Europe External Programme with Africa
On 19 December 2020, killings occurred in Idaga Hamus. Eritrean soldiers killed approximately 150 civilians, including a priest and women seeking refuge in a church, located 4 km to the west of Marieam Dengelat. The town and some rural villages ( Maimegelta, Dengelat, Tsa'a and Hangoda) are under the control of Eritrean forces. The military is slaughtering the animals. People are starving to death.Situation Report EEPA HORN No. 31 - 20 December
Europe External Programme with Africa


Demographics

Based on figures from the
Central Statistical Agency The Central Statistical Agency (CSA; Amharic: ማዕከላዊ ስታቲስቲክስ ኤጀንሲ) is an agency of the government of Ethiopia designated to provide all surveys and censuses for that country used to monitor economic and social growth ...
in 2005, Idaga Hamus has an estimated total population of 8,474 of whom 3,962 are men and 4,512 are women.CSA 2005 National Statistics
, Table B.4
The 1994 census reported it had a total population of 4,883 of whom 2,110 were males and 2,773 were females. Together with Freweyni, it is one larger settlements in Saesi Tsaedaemba
woreda Districts of Ethiopia, also called woredas ( am, ወረዳ; ''woreda''), are the third level of the administrative divisions of Ethiopia – after ''zones'' and the '' regional states''. These districts are further subdivided into a number of ...
.


Notes

{{reflist Populated places in the Tigray Region