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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…
010
Wind cave on the talus slope under the “Monster Rock”
There is a steep cliff on the northwest in Mt.Kamihorokamettoku, and Mt.Kamifuranodak…
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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 …
304
San-ai-no-Oka View Park
This is a hilltop park from which you can see the rolling, wavelike hills which charac…
011
Taisho Mudflow Deposit at Kusawake
A volcanic eruption occurred at Mt.Tokachidake on 24th May 1926 caused mudflow. Mudflo…
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Outcrop of Central Cone Lava
An outcrop of Central Cone Lava is the newest lava, which is spouted by volcanic activ…
Points of Interest
