016
Hill in Tokachidake-Geopark area is a very Hokkaido’s scenery.
The hills consist of Biei Pyroclastic Flow Deposit and Pyroclastic Flow Deposit.
308
Miyama-toge Pass
This is a hilltop park from which you can see the rolling, wavelike hills which charac…
007
Block Slope on Central Cone Lava
Central Cone Lava shaped in eruption almost 500 years ago is called aa lava, which is …
201
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…
014
Unconformity between Ugetsuzawa Pyroclastic Flow Deposit and Bikai Formation
You can observe unconformity which is an overlapping joint between deposit in the shal…
Points of Interest
