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Shombole - Tuff Cone
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Shombole

description Shombole Overview

Shombole is an extinct volcanic mountain in southern Kenya, near the border with Tanzania. It is associated with the volcanic landscape of the East African Rift and is distinguished by prominent tuff-cone formations, which consist of consolidated volcanic ash and related fragmental material. These formations were produced during the Pleistocene, a period extending from about 2.58 million to 11,700 years ago.

help Shombole FAQ

Where is Shombole located?

Shombole is an extinct volcanic mountain in southern Kenya. It lies near the border with Tanzania.

What type of volcanic landform is Shombole associated with?

Shombole is associated with prominent tuff-cone formations. These cones are made from consolidated volcanic ash and related fragments.

Is Shombole an active volcano?

No. Shombole is described as an extinct volcanic mountain, meaning it is not regarded as an active volcano.

What region's geology includes Shombole?

Shombole belongs to the volcanic landscape of the East African Rift. Its location is in southern Kenya near Tanzania.

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