Mount Kinpu was added to Your Favorites!

Chichibu-Tama-Kai NP, Yamanashi / Nagano
Claim this place to tell your story your way.
Mount Kinpu’s main sanctuary is a rock, not a building: the roughly 15-metre Gojoiwa. Shugendō tradition says Zaō Gongen was brought here from Yoshino; Kanazakura Shrine below serves as the mountain’s foothill shrine.
Until after World War II, villagers and Shugendō practitioners gathered at Dainichi Hall every August 14, then set off in darkness to reach Kinpu’s summit at dawn. A local report’s author remembered joining the climb in 1934.
Gojoiwa yielded crystal beads and clay horses, linking summit worship to at least the 10th century. A Kawakami chronicle records a rainmaking belief: emptying pooled water from a hollow on the rock would bring rain.
Old records list 9 pilgrimage routes from Kai and another from Shinano. Edo-period artist Utagawa Hiroshige walked the Mitake Gedo approach to Kanazakura Shrine and sketched its curious rocks.
Quartz from Kinpu’s foothills helped spark Kofu’s jewelry trade. In the Edo period, a Kyoto crystal worker came to buy local rough and introduced polishing skills that grew into Koshu crystal craft.
At nearby Kurohira, pegmatite pockets in Kinpu’s granite belt yielded smoky quartz from pale brown to nearly black, often with feldspar clusters. Amethyst appears there, too—though only occasionally.
A verse attributed to retired Emperor Juntoku links Kinpu with the Chikuma River: spring water runs clear as snow disappears from Ikuhi Peak, an old name that local records identify with this mountain.
Cross the Yamanashi–Nagano border and 金峰山 changes pronunciation: Kinpu-san in Yamanashi, Kinpō-san in Nagano. Older records also call it Kōshū Ontake-yama and Kanamaru-yama.
Chichibu-Tama-Kai National Park has no volcanoes at all. Kinpu sits in its western granite belt, where weathering and erosion leave dramatic rock towers such as summit Gojoiwa.
Near Kinpu’s summit, dense conifer forest gives way to low mats of dwarf pine and yellow-flowered rhododendron. This striking change appears above 2,500 metres, where the park’s high-ridge vegetation begins.