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Kobi-sho volcano

Stratovolcano 117 m / 384 ft
Japan, 25.92°N / 123.68°E
Current status: (probably) extinct (0 out of 5) | Reports
Kobi-sho volcano books
Typical eruption style: unspecified
Kobi-sho volcano eruptions: None during the past 10,000 years
Less than few million years ago (Pleistocene) No recent earthquakes
TimeMag. / DepthDistanceLocation
No recent earthquakes

Background:

Kobi-sho is a stratovolcano, the top of which breaches the surface of the East China Sea to form a small 1-km-wide island. A few craters are present, but thin basalt flows make up the majority of the island. These basalts are typically porphyritic, characterized by phenocrysts of plagioclase (dominant), olvine, and clinopyroxene (Shinjo, 1998). It was probably active less than a few tens of thousand years ago, but is generally less than 0.2 million years old (Nakano et al., 2001; Shinjo, 1998).
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Source: Smithsonian / GVP volcano information


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