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About: Ngenyn

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Ngenyn is a Late Stone Age and/or a Savanna Pastoral Neolithic archaeological site located in the Kapthurin River Basin, which is part of the Tugen Hills, west of Lake Baringo. It falls within the Baringo County (part of the former Rift Valley Province) in north central Kenya. The occupied area is situated on the floodplain of the River Ndau's confluence with the Sekutionnen River, on a widespread terrace called the Low Terrace, the top of which is about 3m above the level of the modern river. The site was initially discovered by Louis Leakey in 1969. It was visible as a large exposure of bones, stone tools and pottery eroding out of the terrace. The site was excavated in the late 1970s as part of Francoise Hivernel's PhD research. Ngenyn remains the only Late Holocene site excavated in th

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  • Ngenyn is a Late Stone Age and/or a Savanna Pastoral Neolithic archaeological site located in the Kapthurin River Basin, which is part of the Tugen Hills, west of Lake Baringo. It falls within the Baringo County (part of the former Rift Valley Province) in north central Kenya. The occupied area is situated on the floodplain of the River Ndau's confluence with the Sekutionnen River, on a widespread terrace called the Low Terrace, the top of which is about 3m above the level of the modern river. The site was initially discovered by Louis Leakey in 1969. It was visible as a large exposure of bones, stone tools and pottery eroding out of the terrace. The site was excavated in the late 1970s as part of Francoise Hivernel's PhD research. Ngenyn remains the only Late Holocene site excavated in the Lake Baringo Basin and in general very little archaeological work has been done on the Late Holocene within the Baringo County. (en)
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  • Ngenyn is a Late Stone Age and/or a Savanna Pastoral Neolithic archaeological site located in the Kapthurin River Basin, which is part of the Tugen Hills, west of Lake Baringo. It falls within the Baringo County (part of the former Rift Valley Province) in north central Kenya. The occupied area is situated on the floodplain of the River Ndau's confluence with the Sekutionnen River, on a widespread terrace called the Low Terrace, the top of which is about 3m above the level of the modern river. The site was initially discovered by Louis Leakey in 1969. It was visible as a large exposure of bones, stone tools and pottery eroding out of the terrace. The site was excavated in the late 1970s as part of Francoise Hivernel's PhD research. Ngenyn remains the only Late Holocene site excavated in th (en)
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  • Ngenyn (en)
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