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Hill in Tokachidake-Geopark area is a very Hokkaido’s scenery.
The hills consist of Biei Pyroclastic Flow Deposit and Pyroclastic Flow Deposit.

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Miyama-toge Pass
This is a hilltop park from which you can see the rolling, wavelike hills which charac…

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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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Biei Station
Biei Station was built in September 1899, as part of the Hokkaido Government Railway l…

011
Taisho Mudflow Deposit at Kusawake
A volcanic eruption occurred at Mt.Tokachidake on 24th May 1926 caused mudflow. Mudflo…

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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…