Iettunup

Iettunup is a shield volcano on the Kamchatka Peninsula, defined by its broad, gently sloping sides that rise gradually from the surrounding land. The peak reaches approximately 1340 meters, with a wide dome-like shape that covers a large area of the landscape.

The volcano formed through repeated basaltic lava flows spread over long geological time periods. These successive layers from different eruption phases gradually built up the wide, dome-shaped structure visible today.

The volcano attracts geologists and researchers who want to understand the volcanic patterns of Kamchatka and the Russian Far East. Scientists value this location for learning how shield volcanoes form and develop in this remote region.

This location is very remote and requires special planning and regional permits to visit safely. Summer months offer the most accessible conditions for reaching the area and conducting observations.

This volcano stands out from most others in the region because it is one of the few shield volcanoes in an area dominated by stratovolcanoes. Its presence helps scientists understand the diverse volcanic processes that have shaped Kamchatka over time.