Aogashima

Aogashima
Native name: <span class="nickname" ">青ヶ島

Montage of Aogashima
Geography
Location Izu Islands
Coordinates 32°27′25.2″N 139°46′1.2″E / 32.457000°N 139.767000°E / 32.457000; 139.767000Coordinates: 32°27′25.2″N 139°46′1.2″E / 32.457000°N 139.767000°E / 32.457000; 139.767000
Archipelago Izu Islands
Area 8.75 km2 (3.38 sq mi)
Length 3.5 km (2.17 mi)
Width 2.5 km (1.55 mi)
Coastline 9 km (5.6 mi)
Highest elevation 423 m (1,388 ft)
Administration
Japan
Demographics
Population 170 (January 2014)

Aogashima (青ヶ島) is a volcanic Japanese island in the Philippine Sea.[1] The island is administered by Tokyo and located approximately 358 kilometres (222 mi) south of Tokyo and 64 kilometres (40 mi) south of Hachijō-jima. It is the southernmost and most isolated inhabited island of the Izu archipelago.[2]

The village of Aogashima administers the island under Hachijō Subprefecture of Tokyo Metropolis. The island's area is 8.75 km2 (3.38 sq mi) and, as of 2014, its population 170. Aogashima is also within the boundaries of the Fuji-Hakone-Izu National Park.

Geology

Aogashima is a complex Quaternary volcanic island 3.5 km in length with a maximum width of 2.5 km, formed by the overlapping remnants of at least four submarine calderas. The island is surrounded by very steep rugged cliffs of layered volcanic deposits. The southern coast also rises to a sharp ridge forming one edge of a caldera named Ikenosawa (池之沢) with a diameter of 1.5 km. The caldera dominates the island, with one point on its southern ridge, Otonbu (大凸部) with a height of 423 metres (1,388 ft), as the island's highest point. The caldera is occupied by a secondary cone named Maruyama (丸山). Still considered a Class-C active volcano by the Japan Meteorological Agency, the last eruption of Aogashima was during a four-year period from 1781–1785.

History

The history of human settlement on Aogashima is uncertain. Most of the people in Aogashima are Japanese. The island is mentioned in Edo period records kept at Hachijō-jima, which record volcanic activity in 1652, and from 1670–1680. An earthquake swarm in July 1780 was followed by steam rising from the lakes in the Ikenosawa Caldera. Further earthquakes in May 1781 led to an eruption. In April 1783, lava flows from the Maruyama cone resulted in the evacuation of all 63 households on the island. During a massive eruption in 1785, some 130–140 of the population of 327 islanders perished.

See also

References

  1. ↑ Nussbaum, Louis-Frédéric. (2005). "Izu Shotō," Japan Encyclopedia, p. 412.
  2. ↑ Gotoh, H. et al. (2010). "Infrastructure Maintenance and Disaster Prevention Measures on Isolated Islands: the Case of the Izu Islands near Tokyo" in Island Sustainability (Favro, S., editor), p. 187.

External links

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