Nishinoshima (Ogasawara)
Nishinoshima | |
---|---|
Nishinoshima in 1978 | |
Elevation | 38 m (125 ft) |
Location | |
Location | Volcano Islands, Japan |
Coordinates | 27°14′49″N 140°52′28″E / 27.24694°N 140.87444°ECoordinates: 27°14′49″N 140°52′28″E / 27.24694°N 140.87444°E |
Geology | |
Type | Caldera |
Last eruption | 2014 [1](ongoing) |
Nishi-no-shima (西之島, "western island") is a volcanic island that is part of the Volcano Islands arc. The island was enlarged in 1974 after fresh eruptions created a new section of the island. Its maximum height is 38 meters. It has also been known as Rosario Island.[2]
Morphology
Previous to 1974, Nishinoshima formed a small, green island which had no eruptions in the past 10,000 years. The volcano takes the form of a caldera. It has many large, submarine, satellite cones to the south, west and northeast. The southern cone rises to within 214 m of the surface, around 9 km SSE of Nishinoshima.
Eruptions
Prior to 1973, no eruptions had ever been recorded at Nishinoshima.
1973-1974 Eruption
On 30 May 1973 the crew of a passing ship noted that at around 11:00, white smoke rose east of the island to around 100 m in the air every few minutes. An aerial inspection the next day said that the eruption was taking place 400 m east of the island. A whirlpool was also seen. Yellow-green sea water and floating pumice were seen 5 km north of the site. Another crew discovered that two black rocks were rising from the sea.
In July the eruption continued to erupt water fountains every few minutes with white smoke rising to 100 m above sea level. An aerial inspection on 14 September noted that a new island had formed above the submarine eruption site, the island formed a cinder cone around 40 m high and 120 m across. The new island had a 70 m diameter crater that frequently ejected cinders to a maximum height of 300 m. But white smoke rose to a height around 1,500 m high.
In November a fissure eruption was noted on the new island with a chain of cinder cones running from southwest to northeast, the most recent cones were formed at the end of the chain, with the original cone being destroyed by the waves. The cones were erupting ash to a height of around 300 m.
In December the new island grew larger than "old" Nishinoshima. The island was 700 m long and 250 m wide; the new island had now developed a central crater that rose to a maximum height of 40 m. The cone was continuing to eject ash and cinders to a height of 100 m. A small craterlet on the new island was also emitting lava flows.
By February, 1974 the new island had developed two cinder cones at the western end of the new island, but only the eastern cinder cone was erupting. Observations on 11 January noted that the active eastern cinder cone was emitting a lava flow.
In March the new island was still erupting; by then the island had five cinder cones; one cinder cone was erupting red hot lava. Lava flows were still erupting from the new island's flanks. On March 1, the five cinder cones were quiet, but a large lava flow may have still been effusing from the island's flanks. After that, the eruption ended; wave movements then joined the new and old islands.
2013-2014 eruption
In November 2013, an eruption created a new, small island south-southeast off the shore of the volcano.[3][4][5][6] As of December 2013, the island had reached an area of 56,000 square meters (13.8 acres), three times the initial size. Its elevation was between 60 and 80 feet above sea level. The island was considered large enough to maintain a presence above sea level for at least several years.[7][8] By 20 December 2013, the island had grown fast enough that experts predicted that it would probably join up with Nishinoshima before the end of 2013, and cease to be a separate island.[9] On 26 December 2013, the Japanese Coast Guard confirmed that the two islands had joined.[10]
The island had not yet been given an official name but was merely referred to in Japanese reports as "atarashii shima" or "shintō" (新島),[11] which can also be read "niijima" (meaning simply, "new island"). Government officials had said the island would be named "after it is stable and it is clear it will remain".[12] But with the island having merged with Nishinoshima, "there is little possibility it will be named as a separate entity."[13]
References
- ↑ "Japan's new island grows in size after volcanic eruption". 24 January 2014. Retrieved 24 January 2014.
- ↑ Freeman, Otis W. (1951). Geography of the Pacific, pp. 229-235.
- ↑ "Volcano raises new island far south of Japan". Times of India. 21 November 2013. Retrieved 21 November 2013.
- ↑ "Volcano Eruption Creates New Island". International Business Times. 21 November 2013. Retrieved 22 November 2013. with pictures.
- ↑ Volcanic Blast Forms New Island Near Japan
- ↑ Netburn, Deborah. "Is Niijima here to stay? New image of the newest island on Earth". latimes.com. Retrieved 2013-12-20.
- ↑ "New volcanic island off Japan still growing in ongoing eruptions". UPI.com. Retrieved 2013-12-20.
- ↑ "Japan’s newly created island is actually growing". Salon.com. Retrieved 2013-12-20.
- ↑ "新島、年内につながる可能性 西之島まで百メートル切る". 47News (in Japanese). Retrieved 20 December 2013.
- ↑ "新島、西之島と一体化=海保が確認". Jiji.com (in Japanese). Jiji Tsūshinsha. Retrieved 26 December 2013.
- ↑ "しんとう". Hokkaidō Shinbun. 12 January 2014. Retrieved 16 January 2014.
- ↑ "名もなき新島、どんな運命 残れば領海わずかに拡大? 小笠原諸島". Asashi Shimbun. 26 November 2013.
- ↑ "Lava flow connects new islet with Nishinoshima island". Asahi Shimbun. 26 December 2013. Retrieved 27 December 2013.
External links
- Nishinoshima, Ogasawara by Geographical Survey Institute
- Global Volcanism Program
- Nishinoshima, Kaiiki Kazan Database, Japan Coast Guard (in Japanese)
- New Japanese Island Forming in Pacific Ocean: Photos, Nov 22, 2013
- New island at NASA's Earth Observatory website