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Geological Formation

Kegon Falls

Volcanic Formations

Kegon Falls drops 97 meters over a width of 7 meters in Nikko National Park, Tochigi Prefecture, on the Japanese island of Honshu, fed by water flowing out of Lake Chuzenji. The falls exist because lava flows once rerouted the Daiya River, damming its path and forcing the water over the resulting volcanic rock face in a single plunge; roughly twelve smaller cascades run alongside and behind the main falls, leaking through cracks between the mountain and the old lava flows. Kegon Falls was named one of Japan's Eight Views in 1927 and was later included on the Ministry of the Environment's Japan's Top 100 Waterfalls list in 1990, and it draws large numbers of visitors especially during the autumn foliage season. This entity documents Kegon Falls specifically as a geological formation, a waterfall created where lava flows rerouted and dammed a river.

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National Park or Reserve 1
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Source Wikidata: Kegon Falls
Sources
1. Kegon Falls (Wikipedia)
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Quote, Lead section
Kegon Falls (華厳滝, Kegon no Taki) is located at Lake Chūzenji (source of the Oshiri River) in Nikkō National Park near the city of Nikkō, Tochigi Prefecture, Japan. The falls were formed when the Daiya River was rerouted by lava flows.
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Wikidata: Kegon Falls
Wikidata Q37580, class allow-list match (w-wdresolver-0926)View the Source
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