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Itoigawa UNESCO Global Geopark responds to increased activity of Mt. Yakeyama
Itoigawa UNESCO Global Geopark is located atop a massive fault line. This location, straddling the border between the Eurasian and North American continental plates, is the reason for Itoigawa Geopark’s extreme topography, where mountains nearly 3000 meters in height plunge into the Sea of Japan.
Many of these mountains are volcanic in origin, formed of andesite, granite, porphyrite, diorite and other rocks. The youngest of these volcanoes is Mt. Yakeyama (2400 m). Born only about 3000 years ago, Mt. Yakeyama remains active to this day. Its last magma and pyroclastic flow producing eruption occurred about 300 years ago, but it has continued to produce smaller eruption events and steam explosions since then. In 1974, a phreatic eruption (steam-blast eruption) launched volcanic bombs and ash, killing 3 university students conducting field research on the mountain. The mountain experienced another phreatic eruption in 1983, but has mostly remained quiet since.
In the exceptionally seismically active Japanese Islands, Geoparks serve an important role in educating the public about disaster preparedness and hazard reduction. The Itoigawa UNESCO Global Geopark continues to include this.