The Chyulu Hills are a mountain range in Makueni County in southeastern Kenya, forming a volcanic field roughly 100 kilometers long stretched along a northwest-to-southeast axis. Their highest peak reaches about 2,188 meters. This entity documents the Chyulu Hills specifically as a geological formation, a hundred-kilometer volcanic field in southeastern Kenya.
Facts
Classification
Protected StatusNational Park or Reserve 1 Connections
Caused By
Source Chyulu Hills (Wikipedia)
In Discipline
Source Chyulu Hills (Wikipedia)
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Sources
1. Chyulu Hills (Wikipedia)
- the Leviathan Cave in Chyulu Hills National Park; part of the Tsavo conservation area
Caused By: Volcanism, Lead, process Volcanism
It forms a 100 km (62 mi)-long volcanic field in an elongated northwest-southeast direction.
In Discipline: Speleology, Lead paragraph
The Chyulu Hills is a mountain range in Makueni County in southeastern Kenya
Caused By: Volcanism, Lead paragraph
It forms a 100 km (62 mi)-long volcanic field in an elongated northwest-southeast direction.
View the Source2. Smithsonian Institution Global Volcanism Program: Volcanoes of the World, Holocene volcanoes service
Smithsonian Institution Global Volcanism ProgramVolcanoes of the World, volcano 222130Quote, Volcanoes of the World, volcano 222130
"Volcano_Name": "Chyulu Hills" ... "Last_Eruption_Year": 1855
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