- Info & Contacts
The Global Volcanism Program has no activity reports for Kell.
The Global Volcanism Program has no Weekly Reports available for Kell.
The Global Volcanism Program has no Bulletin Reports available for Kell.
Kell volcano is a small Holocene stratovolcano constructed within the Pizrak caldera, immediately north of Zheltovsky volcano (Masurenkov, 1980). This remote volcanic complex consists of three partially nested 3-5 km wide calderas containing lava domes and several small stratovolcanoes, the largest of which is 900-m-high Kell volcano.
The Global Volcanism Program is not aware of any Holocene eruptions from Kell. If this volcano has had large eruptions (VEI >= 4) prior to 10,000 years ago, information might be found on the Kell page in the LaMEVE (Large Magnitude Explosive Volcanic Eruptions) database, a part of the Volcano Global Risk Identification and Analysis Project (VOGRIPA).
This compilation of synonyms and subsidiary features may not be comprehensive. Features are organized into four major categories: Cones, Craters, Domes, and Thermal Features. Synonyms of features appear indented below the primary name. In some cases additional feature type, elevation, or location details are provided.
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