BANDAISAN GEOPARK > J.The Northeastern Corst Area of the LakeInawashiro

J.The Northeastern Corst Area of the LakeInawashiro

The shallow lakefront where the swan comes flying.Vast dislocation crossing the Tohoku district, Kawageta dislocation

The Kawageta dislocation which is an extension of the vast dislocation running through Japan runs to the north and south. The development of the characteristic dislocation wall is seen along dislocation.Crystalline rock is exposed on the east side of the dislocation and may date back to the Paleozoic era hundreds of millions of years ago in the times of the stratum.

Kohiragata Tenman-gu Shrine in northeast bank "Tenjinhama" of LakeInawashiro is counted among Japan's three biggest Tenman-gu Shrine and enshrines God of the study "Sugawara Michizane".I come into the limelight again in the present age of the exam war, and many examinees visit here.In the Lake Inawashiro northern coast "Hakuchohama-beach"), wintering of the migratory bird including the swan is seen every year. In addition, there is appointed to the natural monument of the country with Mizusugi moss stock.

Access 5min. from Banetsu highway Inawashiro-Bandaikougen I.C. by car.


Activity in the area

Bandaisan Geopark Council

Kitashiobara Village Nature and Environmental Utilization Center
1093 Kengamine, Hibara,Kitashiobara-mura,Fukushima Prefecture 969-2701
Bandaisan Geopark Council
TEL 0241-32-3180 FAX 0241-32-2927