305
Shin-ei-no-Oka View Park
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 …
014
Unconformity between Ugetsuzawa Pyroclastic Flow Deposit and Bikai Formation
You can observe unconformity which is an overlapping joint between deposit in the shal…
201
Biei Station
Biei Station was built in September 1899, as part of the Hokkaido Government Railway l…
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…
006
Outcrop of Central Cone Lava
An outcrop of Central Cone Lava is the newest lava, which is spouted by volcanic activ…
Points of Interest
