Geological formation in Kenya
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 deposited due to formation of the Rift valley .
References
Categories :
Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
**DISCLAIMER** We are not affiliated with Wikipedia, and Cloudflare.
The information presented on this site is for general informational purposes only and does not constitute medical advice.
You should always have a personal consultation with a healthcare professional before making changes to your diet, medication, or exercise routine.
AI helps with the correspondence in our chat.
We participate in an affiliate program. If you buy something through a link, we may earn a commission 💕
↑
