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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…
304
San-ai-no-Oka View Park
This is a hilltop park from which you can see the rolling, wavelike hills which charac…
014
Unconformity between Ugetsuzawa Pyroclastic Flow Deposit and Bikai Formation
You can observe unconformity which is an overlapping joint between deposit in the shal…
007
Block Slope on Central Cone Lava
Central Cone Lava shaped in eruption almost 500 years ago is called aa lava, which is …
305
Shin-ei-no-Oka View Park
This is a hilltop park from which you can see the rolling, wavelike hills which charac…
015
Ohachidaira Caldera Pyroclastic Flow Deposit at Ten’ninkyo Gorge
Welded tuff spreads from lake Chubetsu to Ten'ninkyo Hot Spring. Lake Chubetsu is also…
Points of Interest
