Mount Washiba, Granite summit in Toyama, Japan
Mount Washiba is a granite summit located in the Hida Mountains within the Japanese Alps of central Honshu. The peak rises to approximately 2900 meters and forms part of a significant chain of mountains in this region.
The mountain formed through volcanic activity involving stratovolcanoes and lava dome formations in its geological past. The last eruption occurred approximately 12,000 years ago, shaping the landscape we see today.
The name translates to Eagle Wing Mountain, referring to the peak's distinctive silhouette visible from surrounding valleys. Climbers and locals use the mountain as a reference point in the landscape and gather at the summit to experience the panoramic views across the alpine region.
Visitors can find mountain hut accommodation nearby to support multi-day climbing expeditions in the area. The ascent requires proper gear and physical preparation, particularly during winter months when conditions are more challenging.
The peak straddles the border between two prefectures, connecting Nagano and Toyama geographically. This position makes it an unusual spot where visitors can stand between two administrative regions simultaneously.
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