Aoyate drought

Last updated

The Aoyate drought was an acute meteorological drought that according to Turkana tradition affected much of the Rift Valley region of Kenya during the late 18th century or early 19th century. [1] [2]

18th century Century

The 18th century lasted from January 1, 1701 to December 31, 1800. During the 18th century, elements of Enlightenment thinking culminated in the American, French, and Haitian revolutions. This was an age of violent slave trading, and global human trafficking. The reactions against monarchical and aristocratic power helped fuel the revolutionary responses against it throughout the century.

19th century Century

The 19th (nineteenth) century was a century that began on January 1, 1801, and ended on December 31, 1900. It is often used interchangeably with the 1800s, though the start and end dates differ by a year.

Contents

Naming

The word aoyate is from the Turkana language and means long dry time. It is the word that the Turkana use to describe this dry period in their history. [1]

Turkana is the language of the Turkana people of Kenya. It is spoken in northwestern Kenya, primarily in Turkana County, which lies west of Lake Turkana. It is one of the Eastern Nilotic languages, and is closely related to Karamojong, Jie and Teso of Uganda, to Toposa spoken in the extreme southeast of South Sudan, and to Nyangatom in the South Sudan/Ethiopia Omo valley borderland; these languages together form the cluster of Teso–Turkana languages.

Turkana people ethnic group of Africa

The Turkana are a Nilotic people native to the Turkana County in northwest Kenya, a semi-arid climate region bordering Lake Turkana in the east, Pokot, Rendille and Samburu people to the south, Uganda to the west, and South Sudan and Ethiopia to the north. They refer to their land as Turkan.

Periodization

Lamphear (1988) noted that chronological reckonings based on the Turkana age-set system suggested a date in the late eighteenth or early nineteenth centuries. He notes that concurrent drought traditions suggested in the chronological reconstruction of neighboring communities indicates that the drought affected much of the Rift Valley region. [1]

Records of Nile River flood stages date back to the 7th century AD and an analysis of the flood patterns and comparison with water levels in Lake Chad revealed a correlation between high Nile discharge and greater rainfall in equatorial East Africa. The analysis of Nile flood stages indicates a 'Minor Low' for the period 1800 to 1830, this was preceded by a 'Minor High' during the years 1725 to 1800 and was followed by a 'Minor High' which lasted between 1830 and 1870. [3]

Lake Chad lake in Africa

Lake Chad is a historically large, shallow, endorheic lake in Africa, which has varied in size over the centuries. According to the Global Resource Information Database of the United Nations Environment Programme, it shrank by as much as 95% from about 1963 to 1998, but "the 2007 (satellite) image shows significant improvement over previous years." Lake Chad is economically important, providing water to more than 30 million people living in the four countries surrounding it on the edge of the Sahara. It is the largest lake in the Chad Basin.

Studies in Ethiopia by Pankhurst indicated major famines in 1880–1881, 1835 and in 1829. These studies are significant in that the country of Ethiopia borders present-day Turkana county. Meanwhile, Samburu historians interviewed by Straight et. al (2016) state that the Samburu separated from a society known as Burkineji in the wake of the 1830s Mutai. [4] According to a Samburu Laibon interviewed by Fratkin (2011), the Sambur 'Il Kipkeku' age-set were warriors during the period c.1837-1851. [5]

The various narratives, records and reports thus point to a long dry period starting about 1800 seemingly peaking with an intensely arid time during the mid-1830s. This would be congruent with Krapf's (1860) mention of a "great famine of 1836". [6]

Prelude

There are a number of oral traditions from various communities across much of southern Africa that point to the region having experienced declining rainfall levels from about 1800 to about 1830. This saw the progressive desiccation of lakes, rivers and springs, a phenomenon observed by an employee of the East India Company in the 1820s who noted;

...in many parts of the interior of the country the springs and rivulets are drying up and annual rains become more scanty and irregular. The traveler often meets with houses and farms that have been deserted by their owners on account of a permanent failure in the supply of water which they once enjoyed.

Quoted in Clifton Crais, Poverty, War, and Violence in South Africa [7]

Effects of the drought

Diminished carrying capacity for livestock

The drought decimated the herds of the Chemwal, thought to have been cervicothoraic-humped Sanga crossbreeds, leading to the disintegration of the community. [8]

Famine

Sengwer folklore has it that, "It became dry and there was great hunger. The Siger went away to the east to Moru Eris, where most of them died of heat and starvation. So many died that there is still a place there called Kabosan (the rotten place)". [1]

War

Full scale war flared up between the Turkana and Chemwal. Bands of Turkana warriors forced some Chemwalin northwards to the head of Lake Turkana where they formed the Inkabelo section of the developing Dassanech community. Other Chemwalin were pushed back onto the Suk hills, to the south to be incorporated by the Chok leading to the rise of the ritually important Kachepkai clan while others yet were assimilated by the Turkana where some became a new clan known simply as Siger. The victorious Turkana took possession of the grazing and water resources of Moru Assiger.

Mass migration

Other Chemwalin were forced to abandon their highland abodes and fled eastwards where they ran into even drier conditions and a great many died. [1]

Aftermath

The Aoyate destroyed the lives and livelihoods of many inhabitants of the Rift Valley region.

Related Research Articles

Nile River in Africa and the longest river in the world

The Nile is a major north-flowing river in northeastern Africa, and is the longest river in Africa and the disputed longest river in the world, as the Brazilian government claims that the Amazon River is longer than the Nile. The Nile, which is about 6,650 km (4,130 mi) long, is an "international" river as its drainage basin covers eleven countries, namely, Tanzania, Uganda, Rwanda, Burundi, the Democratic Republic of the Congo, Kenya, Ethiopia, Eritrea, South Sudan, Republic of the Sudan and Egypt. In particular, the Nile is the primary water source of Egypt and Sudan.

The Samburu are a Nilotic people of north-central Kenya. They are a sub tribe of the Maasai. The Samburu are semi-nomadic pastoralists who herd mainly cattle but also keep sheep, goats and camels. The name they use for themselves is Lokop or Loikop, a term which may have a variety of meanings which Samburu themselves do not agree on. Many assert that it refers to them as "owners of the land" though others present a very different interpretation of the term. The Samburu speak the Samburu dialect of the Maa language, which is a Nilo-Saharan language. There are many game parks in the area, one of the most well known is Samburu National Reserve.The Samburu is the third largest in the Maa community of Kenya and Tanzania,after the Kisonko(Isikirari)of Tanzania and Purko of Kenya and Tanzania.

Lake Turkana Alkaline lake on the border of Ethiopia and Kenya

Lake Turkana, formerly known as Lake Rudolf, is a lake in the Kenyan Rift Valley, in northern Kenya, with its far northern end crossing into Ethiopia. It is the world's largest permanent desert lake and the world's largest alkaline lake. By volume it is the world's fourth-largest salt lake after the Caspian Sea, Issyk-Kul, and Lake Van, and among all lakes it ranks 24th.

The Kalenjin are an ethnolinguistic group indigenous to Kenya, residing mainly in what was formerly the Rift Valley Province. They are estimated to number a little over 4.9 million individuals as per the Kenyan 2009 census and are divided into the Kipsigis, Nandi, Keiyo, Marakwet, Sabaot, Pokots, Tugen, Terik and Ogiek. They speak the Kalenjin language, which belongs to the Nilotic group within the wider Nilo-Saharan family.

Sámuel Teleki Hungarian explorer

Count Sámuel Teleki de Szék was a Hungarian explorer who led the first expedition to Northern Kenya. He was the first European to see, and name, Lake Rudolf, though the existence of the lake was known in Europe long before Teleki arrived at the scene.

Afar Triangle A geological depression caused by the Afar Triple Junction

The Afar Triangle is a geological depression caused by the Afar Triple Junction, which is part of the Great Rift Valley in East Africa. The region has disclosed fossil specimens of the very earliest hominins, that is, the earliest of the human clade; and it is thought by some paleontologists to be the cradle of the evolution of humans, see Middle Awash, Hadar. The Depression overlaps the borders of Eritrea, Djibouti and the entire Afar Region of Ethiopia; and it contains the lowest point in Africa, Lake Asal, Djibouti, at 155 m below sea level.

Ateker peoples

Ateker, or ŋaTekerin, is a common name for the closely related Jie, Karamojong, Turkana, Toposa, Nyangatom and Teso peoples and their languages. These ethnic groups inhabit an area across Uganda and Kenya. Itung'a and Teso have been used among ethnographers, while the term Teso-Turkana is sometimes used for the languages, which are of Eastern Nilotic stock. Ateker means 'clan' or 'tribe' in the Teso language. In the Lango language, the word for clan is atekere.

Turkana County County in Kenya

Turkana County is a county in the former Rift Valley Province of Kenya. Turkana is the second largest, by land area, and also the northwesternmost county in Kenya. It is bordered by the countries of Uganda to the west; South Sudan and Ethiopia, including the disputed Ilemi Triangle, to the north and northeast; and Lake Turkana to the east. To the south and east, neighbouring counties in Kenya are West Pokot, Baringo and Samburu Counties, while Marsabit County is located on the opposite shore of Lake Turkana.

2010 Sahel famine

A large-scale, drought-induced famine occurred in Africa's Sahel region and many parts of the neighboring Sénégal River Area from February to August 2010. It is one of many famines to have hit the region in recent times.

The Kalenjin people are an ethnolinguistic group indigenous to East Africa with a presence, as dated by archaeology and linguistics, that goes back many centuries. Their history is therefore deeply interwoven with those of their neighboring communities as well as with the histories of Kenya, Uganda, Tanzania, South Sudan and Ethiopia.

Lake Suguta

Lake Suguta is a former lake in Africa. It formed in the Suguta Valley, which is part of the East African Rift, south of Lake Turkana during the Holocene African humid period.

The Sengwer people are an indigenous community who primarily live in the Embobut forest in the western highlands of Kenya and in scattered pockets across Trans Nzoia, West Pokot and Elgeyo-Marakwet counties. The Sengwer are sometimes portrayed as a component of the Marakwet people but are a distinct ethnic grouping.

The Loikop people, also known as Wakuafi, Kor, Mu-Oko, Muoko/Ma-Uoko and Mwoko, were a tribal confederacy who inhabited present-day Kenya in the regions north and west of Mount Kenya and east and south of Lake Turkana. The area is roughly conterminous with Samburu and Laikipia Counties and portions of Baringo, Turkana and (possibly) Meru Counties. The group spoke a common tongue related to the Maasai language, and typically herded cattle. The Loikop occasionally interacted with the Cushitic, Bantu, and Chok peoples. The confederacy had dispersed by the 21st century.

Mutai is a term used by the Maa-speaking communities of Kenya to describe a period of wars, usually triggered by disease and/or drought affecting widespread areas of the Rift Valley region of Kenya. According to Samburu and Maasai tradition, two periods of Mutai occurred during the nineteenth century. The second Mutai lasted from the 1870s to the 1890s.

The Iloikop wars were a series of wars between the Maasai and a community referred to as Kwavi and later between Maasai and alliance of reformed Kwavi communities. These were pastoral communities that occupied large tracts of East Africa's savanna's during the late 18th and 19th centuries. These wars occurred between c.1830 and 1880.

Mutai is a term used by the Maa speaking communities of Kenya to describe a period of wars, usually triggered by disease and/or drought and affecting widespread areas of the Rift Valley region of Kenya. According to Samburu and Maasai folklore, periods of Mutai occurred during the nineteenth century.

The Chemwal people were a Kalenjin-speaking society that inhabited regions of western and north-western Kenya as well as the regions around Mount Elgon at various times through to the late 19th century. The Nandi word Sekker was used by Pokot elders to describe one section of a community that occupied the Elgeyo escarpment and whose territory stretched across the Uasin Gishu plateau. This section of the community appears to have neighbored the Karamojong who referred to them as Siger, a name that derived from the Karimojong word esigirait. The most notable element of Sekker culture appears to have been a dangling adornment of a single cowrie shell attached to the forelock of Sekker women, at least as of the late 1700s and early 1800s.

The Ngaa people were a community that according to the traditions of many Kenyan communities inhabited regions of the Swahili coast and the Kenyan hinterland at various times times in history.

The Siger people were a community commonly spoken of in the folklore of a number of Kenyan communities that inhabited regions of north western Kenya at various points in history.

References

  1. 1 2 3 4 5 Lamphear, John (1988). "The People of the Grey Bull: The Origin and Expansion of the Turkana". The Journal of African History. 29 (1): 32–33. Retrieved August 15, 2019.
  2. Fukui, Katsuyoshi; Markakis, John (1994). Ethnicity & Conflict in the Horn of Africa. Oxford: James Currey Publishers. p. 67. ISBN   9780852552254.
  3. Hassan, Fekri. "Historical Nile Floods and their Implications for Climatic Change". Science. 212 (4499): 1142. Retrieved September 18, 2019.
  4. Straight, Bilinda; Lane, Paul; Hilton, Charles (2016). ""Dust people": Samburu perspectives on disaster, identity, and landscape". Journal of Eastern African Studies. 10 (1): 179. doi:10.1080/17531055.2016.1138638.
  5. Fratkin, Elliot M. (2011). Laibon: An Anthropologist's Journey with Samburu Diviners of Kenya. Smith College: Rowman Altamira. p. 20. ISBN   9780759120679.
  6. Krapf, Ludwig (1860). Travels, researches, and missionary labours, during an eighteen–year residence in Eastern Africa. London: Trübner and co. p. 142.
  7. Crais, Clifton (2011). Poverty, War, and Violence in South Africa. Cambridge: Cambridge University Press. p. 75-76. ISBN   9781139503563.
  8. Fukui, Katsuyoshi; Markakis, John (1994). Ethnicity & Conflict in the Horn of Africa. Oxford: James Currey Publishers. p. 67. ISBN   9780852552254.