Western Izu
Issiki
-
Pillow lava and magmatic dykes of the Nishina group
Most of the Nishina group of soil strata, which is the oldest strata found on the Izu Peninsula, is lava and subaqueous volcaniclastic flow ejected during the submarine volcanic phase.
When low-viscosity lava flows down the sea bed, it forms a pillow like shape due to surface tension and rapid cooling upon water contact. This is called ‘pillow lava’. In Isshiki, you can seecross-sections of multi-layered pillow lava.
Basic information
- Travel information
- Safety information
- Access
- From the parking lot is a 3-minute walk.
- Rest room
- Kiosk & Rest houses
- Parking information
Related sites of [ Geosite ]
-
Near the Omuroyama Lift Parking Area
・Eastern Izu
・Geosite
・Strata
-
Komoike pond and Shiratakikoen park
・Northern Izu
・Geosite
・Moving Earth
・Natural spring&Hot spring
-
Nakagi
・Southern Izu
・Geosite
・Submarine Volcano
・Columnar joints
-
Futo Coast
・Western Izu
・Geosite
・Submarine Volcano
・Columnar joints
- Choose from categories
- Choose from geology
- Choose from landforms
- Choose from regions
- Choose from sites
