There are two small subsidiary craters adjacent to the main cone and some lava flows resulting from the eruption; examination of the lava nearby shows quench features, typical of rapid cooling brought about by contact with seawater.
Lava nearby shows quench features, typical of rapid cooling brought about by contact with seawater. There are two small subsidiary craters adjacent to the main cone and some lava flows resulting from the eruption.
There are two small subsidiary craters adjacent to the main cone and some lava flows resulting from the eruption. Lava nearby shows quench features, typical of rapid cooling brought about by contact with seawater.
There are two small subsidiary craters adjacent to the main cone and some lava flows resulting from the eruption. Lava nearby shows quench features, typical of rapid cooling brought about by contact with seawater.