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The Daisetsuzan Mountain Range Alpine Zone
From Mt. Hakuundake to Mt. Tomuraushiyama, at over 1700m above sea level, runs a conti…

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San-ai-no-Oka View Park
This is a hilltop park from which you can see the rolling, wavelike hills which charac…

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Unconformity between Ugetsuzawa Pyroclastic Flow Deposit and Bikai Formation
You can observe unconformity which is an overlapping joint between deposit in the shal…

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Block Slope on Central Cone Lava
Central Cone Lava shaped in eruption almost 500 years ago is called aa lava, which is …

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Shin-ei-no-Oka View Park
This is a hilltop park from which you can see the rolling, wavelike hills which charac…

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Ohachidaira Caldera Pyroclastic Flow Deposit at Ten’ninkyo Gorge
Welded tuff spreads from lake Chubetsu to Ten'ninkyo Hot Spring. Lake Chubetsu is also…