Mount Bandai

Mount Bandai (Bandai-san) is a stratovolcano in Fukushima Prefecture that rises to about 1,816 metres and forms a distinctive landmark in the region. A major late 19th-century eruption reshaped its northern slopes and created a landscape of lakes, ponds and breached ridges.

Today’s visitors come for hiking routes, panoramic viewpoints and the colourful Goshikinuma ponds formed by mineral deposits in volcanic waters; a ropeway and local trails provide access to viewpoints and the Urabandai area. The volcanic terrain supports well-marked trails of varying difficulty and several lakeside and forested recreation areas.

The 1888 collapse and eruption are the defining geological events for Bandai, producing lakes such as Lake Hibara and the pond cluster; conservation and visitor facilities manage popular viewing spots and hiking access. The mountain lies north of Lake Inawashiro and near the towns of Inawashiro and Urabandai in central Fukushima.

• 1888 eruption: A catastrophic eruption in July 1888 caused the collapse of the mountain's north flank and created lakes and marshes now known as the Urabandai area, including Lake Hibara and the Goshikinuma ponds.

What to See #

• Summit cone: A volcanic cone rising to about 1,816 metres that dominates the surrounding Urabandai landscape and provides hiking routes to the summit rim.
• Goshikinuma ponds: The Goshikinuma cluster of mineral-rich ponds formed by the 1888 eruption; these small, multi-coloured pools are a major scenic attraction in the northern slopes and foothills.