Sea Floor Landslide Remains of TorokuGeosite 27
When this area was still submerged in the sea, a slope was formed on the sea bed due to the bulging of mountains, and the sediments on the sea bed that had not solidified yet slid down due to earthquakes, resulting in a curved strata (slump fold) that can be observed here.
- Bus: Take the Seibu Kanko Bus bound for Kurio from Seibu Railway Seibu-Chichibu Station or Chichibu Railway Chichibu Station. Get off at Izumida and walk 25 minutes.
- Sites nearby/Base facility