Chalacot
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Chalacot or Chelekot is a village in the
Tigray Region The Tigray Region (or simply Tigray; officially the Tigray National Regional State) is the northernmost Regions of Ethiopia, regional state in Ethiopia. The Tigray Region is the homeland of the Tigrayan, Irob people, Irob and Kunama people. I ...
of
Ethiopia Ethiopia, officially the Federal Democratic Republic of Ethiopia, is a landlocked country located in the Horn of Africa region of East Africa. It shares borders with Eritrea to the north, Djibouti to the northeast, Somalia to the east, Ken ...
. Located in the Enderta woreda (district) of the Debub Misraqawi (Southeastern) Zone, 10 kilometers north of
Antalo Hintalo (), also called Antalo, was Administrative Center of Enderta’s historical wereda of Gabat Melash, is a small town located in the Debub Misraqawi (Southeastern) Zone of the Tigray Region of Ethiopia. It lies on a plateau with an elevati ...
and 17 kilometers south of
Mek'ele Mekelle (), or Mek'ele, 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 Awrajja, awraja in Tigray Province, Tigray. It is locate ...
, the village has an approximate elevation of 2100 meters above sea level. The
Central Statistical Agency The Central Statistical Agency, also known as the Ethiopian Statistical Service (ESS; Amharic: የኢትዮጵያ ስታቲስቲክስ አገልግሎት), is an Ethiopian government agency designated to provide all surveys and censuses for that ...
has not published an estimate for this village's 2005 population.


Geology and soils

The following geological formations are present in this locality: *
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 as ...
* Agula Shale * Mekelle
Dolerite Diabase (), also called dolerite () or microgabbro, is a mafic, holocrystalline, subvolcanic rock equivalent to volcanic basalt or plutonic gabbro. Diabase dikes and sills are typically shallow intrusive bodies and often exhibit fine-grain ...
*
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 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), as well as the current and most recent of the twelve periods of the ...
alluvium Alluvium (, ) 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. Alluvium is also sometimes called alluvial deposit. Alluvium is ...
and freshwater
tufa Tufa is a variety of limestone formed when carbonate minerals precipitation (chemistry), precipitate out of water in ambient temperature, unheated rivers or lakes. hot spring, Geothermally heated hot springs sometimes produce similar (but less ...
The main
geomorphic Geomorphology () is the scientific study of the origin and evolution of topography, topographic and bathymetry, bathymetric features generated by physical, chemical or biological processes operating at or near Earth#Surface, Earth's surface. Ge ...
units, with corresponding soil types are: * 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 continuous rock or a deeper soil that is extremely rich in coarse fragments (gravelly and/or stony). Leptosols cover approximately 1.7 billion hectares o ...
) *** moderately deep dark stony
clay Clay is a type of fine-grained natural soil material containing clay minerals (hydrous aluminium phyllosilicates, e.g. kaolinite, ). Most pure clay minerals are white or light-coloured, but natural clays show a variety of colours from impuriti ...
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 pro ...
) *** deep, dark cracking
clay Clay is a type of fine-grained natural soil material containing clay minerals (hydrous aluminium phyllosilicates, e.g. kaolinite, ). Most pure clay minerals are white or light-coloured, but natural clays show a variety of colours from impuriti ...
s on calcaric material (Calcaric
Vertisol A vertisol is a Soil Order in the USDA soil taxonomy and a Reference Soil Group in the World Reference Base for Soil Resources (WRB). It is also defined in many other soil classification systems. In the Australian Soil Classification it is c ...
, Calcic
Vertisol A vertisol is a Soil Order in the USDA soil taxonomy and a Reference Soil Group in the World Reference Base for Soil Resources (WRB). It is also defined in many other soil classification systems. In the Australian Soil Classification it is c ...
) ** 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 continuous rock or a deeper soil that is extremely rich in coarse fragments (gravelly and/or stony). Leptosols cover approximately 1.7 billion hectares o ...
) *** Shallow very stony
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–si ...
y 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 pro ...
) *** Deep dark cracking
clay Clay is a type of fine-grained natural soil material containing clay minerals (hydrous aluminium phyllosilicates, e.g. kaolinite, ). Most pure clay minerals are white or light-coloured, but natural clays show a variety of colours from impuriti ...
s with very good natural fertility, waterlogged during the wet season (Chromic
Vertisol A vertisol is a Soil Order in the USDA soil taxonomy and a Reference Soil Group in the World Reference Base for Soil Resources (WRB). It is also defined in many other soil classification systems. In the Australian Soil Classification it is c ...
, Pellic
Vertisol A vertisol is a Soil Order in the USDA soil taxonomy and a Reference Soil Group in the World Reference Base for Soil Resources (WRB). It is also defined in many other soil classification systems. In the Australian Soil Classification it is c ...
) *** Brown to dark
sand Sand is a granular material composed of finely divided mineral particles. Sand has various compositions but is usually defined by its grain size. Sand grains are smaller than gravel and coarser than silt. Sand can also refer to a textural ...
s and silt loams on
alluvium Alluvium (, ) 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. Alluvium is also sometimes called alluvial deposit. Alluvium is ...
(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 ...
)


History

Chalacot is mentioned in a charter written in 1794, when Emperor
Tekle Giyorgis Tekle Giyorgis may refer to * Tekle Giyorgis I (c. 1751–1817), Emperor of Ethiopia * Tekle Giyorgis II (died 1873), Emperor of Ethiopia {{hndis, Giyorgis, Tekle ...
made a grant to Meqdese Selassie Church in the village; the document mentions seven properties."Local History in Ethiopia"
(pdf) The Nordic Africa Institute website (accessed 21 April 2008)
Ras
Wolde Selassie Wolde Selassie (; c.1736 – 28 May 1816) was Ras of the Tigray province between 1788 and 1816, and Regent of the Ethiopian Empire between 1797 and 1800. John J. Halls, in his ''Life and Correspondence of Henry Salt'', preserves a description of ...
made Chalacot his capital, and received Henry Salt there in 1810. The Ras built a palace in the village, as well as houses for his wives and the church Chelekot Selassie, which Philips Briggs described as an "architecturally impressive example of the circular ''tikul'' styles of paintings" and "covered in beautiful 19th-century paintings". When Wolde Selassie died in Chalacot (1816), his nephew Walda Rufa'el sacked it. The town had recovered its former prosperity by the 1840s when Ferret and Galiner visited it; they described it as "one of the principal towns" of Ethiopia, with a population of 3,000 living in well-constructed houses and well-kept gardens. However, a little more than a generation later Chalacot had declined;
Guglielmo Massaia Guglielmo Massaia, OFM Cap. (born Lorenzo; 9 June 1809 - 6 August 1889) was an Italian cardinal of the Catholic Church who served as a missionary and a Capuchin friar. Pope Francis named him Venerable on 1 December 2016. Life Guglielmo Massa ...
found only 200 houses with about 1,000 inhabitants and in the 1880s Augustus B. Wylde reported he counted only 80 houses there. The town suffered further losses during the
First Italo–Ethiopian War The First Italo-Ethiopian War, also referred to as the First Italo-Abyssinian War, or simply known as the Abyssinian War in Italy (), was a military confrontation fought between Kingdom of Italy, Italy and Ethiopian Empire, Ethiopia from 1895 to ...
according to Richard Pankhurst, who included Chalacot in a list of northern Ethiopian towns affected by the "disturbed conditions of the times."Richard Pankhurst, ''Economic History of Ethiopia'' (Addis Ababa: Haile Sellasie I University, 1968), pp. 691f


Notable inhabitants

Chelekot is the birthplace of Ras Araya Dimtsu, the chief crown
councillor A councillor, alternatively councilman, councilwoman, councilperson, or council member, is someone who sits on, votes in, or is a member of, a council. This is typically an elected representative of an electoral district in a municipal or re ...
to Emperor
Yohannes IV Yohannes IV ( Tigrinya: ዮሓንስ ፬ይ ''Rabaiy Yōḥānnes''; horse name Abba Bezbiz also known as Kahśsai; born ''Lij'' Kahssai Mercha; 11 July 1837 – 10 March 1889) was Emperor of Ethiopia from 1871 to his death in 1889 at the ...
of Ethiopia from 1867 to 1889. Ras Araya held significant influence as the governor of
Tigray The Tigray Region (or simply Tigray; officially the Tigray National Regional State) is the northernmost Regions of Ethiopia, regional state in Ethiopia. The Tigray Region is the homeland of the Tigrayan, Irob people, Irob and Kunama people. I ...
and Akale Guzay. He lost his life at the Battle of Metema in March 1889 while fighting against the Mahdists of
Sudan Sudan, officially the Republic of the Sudan, is a country in Northeast Africa. It borders the Central African Republic to the southwest, Chad to the west, Libya to the northwest, Egypt to the north, the Red Sea to the east, Eritrea and Ethiopi ...
, alongside Emperor Yohannes. Notably, Ras Araya was Emperor Yohannes's maternal uncle. Another noteworthy figure from Chelekot is Emperor Yohannes's mother, Amate Silas Dimtsu, who was born there. Her father, Dejazmach Dimtsu Debbab of Enderta, served as a hereditary chief of Enderta in the 1820s and 1830s. Chelekot also serves as the burial place of Empress
Tiruwork Wube Tiruwork Wube (died 16 May 1868), also known as Queen Terunesh, was Empress consort of Ethiopia as the second spouse of Emperor Tewodros II of Ethiopia. Origin She was the daughter of Dejazmatch Wube Hayle Maryam, an ethnic Amhara, and the prin ...
, the granddaughter of Ras Wolde Selassie and the widow of Emperor Tewodros II. During his journey to the Battle of Adwa, Emperor Menelik II visited the churches in Chelekot. As a gesture of gratitude for his victory over the Italians, he bestowed his robes of state upon the Church of the Holy Trinity (Mekdese Selassie), where they are still prominently displayed.


Notes

{{reflist Populated places in the Tigray Region