020
The Daisetsuzan Mountain Range Alpine Zone
From Mt. Hakuundake to Mt. Tomuraushiyama, at over 1700m above sea level, runs a conti…
014
Unconformity between Ugetsuzawa Pyroclastic Flow Deposit and Bikai Formation
You can observe unconformity which is an overlapping joint between deposit in the shal…
006
Outcrop of Central Cone Lava
An outcrop of Central Cone Lava is the newest lava, which is spouted by volcanic activ…
030
Tokachidake Hot Springs
Tokachidake Hot Springs take advantage of a main heat source of thermal activity at Nu…
101
The Forests along the White Birch Road
On the road leading from the Biei Town center to Shirogane Hot Spring, many white birc…
206
The Old Hakuginso Cabin
'I frequently remember my work with the snow of Mt. Tokachidake, and it seems as if I …
Points of Interest
