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Owakudani - Fumarole
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Owakudani

description Owakudani Overview

Owakudani is a volcanic valley in the Hakone area of Kanagawa Prefecture, Japan, formed around 3,000 years ago following an eruption of Mount Hakone. The area contains active sulfur vents, hot springs, and fumaroles. Visitors can reach it via the Hakone Ropeway and commonly purchase eggs boiled in the sulfurous water, whose shells turn black from the minerals. Access is sometimes restricted when volcanic gas levels rise.

insights Ranking position

Owakudani ranks #35 of 304 in the Fumarole ranking, behind Stefanos Crater, ahead of Piton de la Fournaise fumaroles.

help Owakudani FAQ

What are Owakudani's famous black eggs?

They are ordinary chicken eggs cooked in naturally hot volcanic water, which turns the shells black through reactions involving sulfur and iron. The inside remains similar to a conventional hard-boiled egg.

Can visitors see Mount Fuji from Owakudani?

Yes, Mount Fuji is visible from parts of Owakudani when weather and cloud cover cooperate. The Hakone Ropeway also provides elevated views across the volcanic landscape.

Is Owakudani safe to visit during volcanic activity?

Access can be restricted when volcanic gas concentrations or seismic activity increase. Visitors should check current Hakone Ropeway and local authority notices, especially if they have respiratory or heart conditions.

How was the Owakudani valley formed?

The valley was formed by volcanic activity at Hakone roughly 3,000 years ago. Active fumaroles still release steam and sulfurous gases from the ground.

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