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Geological Formation

Menengai Crater

Volcanic Formations

Menengai Crater lies just north of the town of Nakuru in Kenya's Great Rift Valley, a large shield volcano whose summit collapsed into a caldera roughly twelve kilometers across, among the largest calderas in the world. The caldera formed following a massive eruption and subsequent collapse of the volcano's summit, leaving steep walls rising several hundred meters above the crater floor. The volcanic system beneath Menengai remains geothermally active, and its heat now powers the Menengai Geothermal Project, one of Kenya's major sources of geothermal electricity. This entity documents Menengai Crater specifically as a geological formation, a large Rift Valley caldera left by the collapse of a shield volcano and now the site of active geothermal power development.

Facts
Classification
Protected Status
UNESCO World Heritage Site 1
Connections

Caused By

Volcanism, Processes
Source Menengai (Wikipedia)

In Discipline

Geology, Disciplines

Wikidata P31 (Q3240715) mapped to discipline Geology via earth5 extended reviewed judgment map; source citation is this entity's own cited Wikidata item.

Source Wikidata: Menengai Crater
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Found In

Also in Geography Atlas: where this subject is found.

Source Wikidata: Menengai Crater
Sources
1. VolcanoDiscovery (data from the Smithsonian Global Volcanism Program): Menengai Volcano
VolcanoDiscovery (data from the Smithsonian Global Volcanism Program)Volcano protected-area line
Quote, Volcano protected-area line
This volcano is located within the Kenya Lake System in the Great Rift Valley, a UNESCO World Heritage property.
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Wikidata: Menengai Crater
Wikidata Q27194113, class allow-list match (w-wdresolver-0926)View the Source
Menengai (Wikipedia)
Caused By: Volcanism, Lead section (caused-by Volcanism)
Quote, Caused By: Volcanism, Lead section (caused-by Volcanism)
Menengai Crater is a massive shield volcano with one of the biggest calderas in the world, in the Great Rift Valley, Kenya.
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