Columnar Joints and Landscapes
Hinomisaki is located on the coast in the westernmost of Shimane Peninsula. Columnar joints developed in Neogene rhyolite and formed fine columns, the width of which is several centimeters. The very narrow columns are thought to result from rapid cooling in the sea because the rhyolitic lava spouted out from a submarine volcano. The cross sections represent distorted polygons. The landscape including fine columns and landforms subjected to long-term erosion makes a gentle impression unlike those of Tsumekizaki and the Jogasaki Coast.
Photo 18: Columnar jointing at Hinomisaki
Photo 19: Cross sections of columns
Location: Izumo City, Shimane Prefecture (On
the Google map)
1) Izumoshi Station on JR Sanin Main Line. Take a bus for Hinomisaki and get off the terminal stop (45 minutes from the station).
2) Izumotaishamae Station on Ichibata Densha Taisha Line. Take a bus for Hinomisaki and get off the terminal stop (25 minutes from the station).
[Names written in Japanese]
Izumo-shi (city), 出雲市
Izumoshi-eki (station), 出雲市駅
Izumotaisyamae-eki (station), 出雲大社前駅