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Kerichwa Valley Tuff

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The Kerichawa Valley Tuff series is a group of pumice-rich trachytic tuffs and agglomerates. They are younger than the Nairobi Trachyte, found in Nairobi as part of the sediments that were depositied due to formation of the Rift valley.[1]

References

  1. ^ "A STUDY ON THE ENGINEERING BEHAVIOUR OF NAIROBI SUBSOIL" (PDF). 7 July 2011. {{cite web}}: line feed character in |title= at position 41 (help)
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