Volcanic activity is still in progress today, lava streams and smoke rising 2000 m were seen on images from December 2, 2013.
This new island emerged as a result of a Surtseyan eruption (volcanic eruption that takes place in shallow seas or lakes) on November 20, 2013, 500 m SE from the coast of Nishimo-shima. On November 21, when it was discovered, the new island was already about 300 x 200 m, and it developed a 150 m wide crater.
The Ogasawara Islands were formed around 48 million years ago. They are a part of the Izu-Bonin-Mariana Arc known geologically as a fore arc. They lie above a subduction zone between the Pacific Plate and the Philippine Sea Plate.
The Pacific Plate is subducting under the Philippine Sea Plate, which creates an oceanic trench to the east of the islands. The crust of the Ogasawara (Bonin) Islands was formed by volcanic activity when subduction began 45–50 million years ago, and is composed mostly of an andesitic volcanic rock called boninite, which is rich in magnesium oxide, chromium, and silicon dioxide.
The last time the volcanoes in that area are known to have erupted was in the mid-1970's. Much of the volcanic activity occurs under the sea, which extends thousands of meters deep along the Izu-Ogasawara-Marianas Trench.
From The Watchers
