Английская Википедия:Aogashima
Шаблон:Short description Шаблон:About Шаблон:Infobox Islands
Шаблон:Nihongo is a volcanic island to the south of Japan in northernmost Micronesia. It is the southernmost and most isolated inhabited island of the Izu Islands. The islands border the northeast Philippine Sea and lie north of the Ogasawara Islands.[1][2] The island lies approximately Шаблон:Convert south of mainland Tokyo and Шаблон:Convert south of Hachijō-jima.
The island is administered by the village of Aogashima, which is subordinate to the Hachijō Subprefecture, which itself is governed by the City of Tokyo. The island has an area of Шаблон:Convert, and, Шаблон:As of, its population is a mere 170 people. This means that the village of Aogashima has the smallest population of any municipality in Japan. Aogashima is also part 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 Шаблон:Nihongo with a diameter of 1.5 km. The caldera dominates the island, with one point on its southern ridge, Шаблон:Nihongo with a height of Шаблон:Convert, as the island's highest point. The caldera is occupied by a secondary cone named Шаблон:Nihongo. 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. It is located along the Izu–Bonin–Mariana Arc.
-
Maruyama is the central cone in the caldera
-
Maruyama in a close view
Important Bird Area
The island has been recognised as an Important Bird Area (IBA) by BirdLife International because it supports populations of Japanese woodpigeons, Pleske's grasshopper warblers, Ijima's leaf-warblers and Izu thrushes.[3]
History
The history of human settlement on Aogashima is uncertain. Most of the people on Aogashima are Japanese. The island is mentioned in Edo period records kept at Hachijō-jima, which recorded volcanic activity in 1652, and from 1670 to 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
External links
- Aogashima Village Official Website
- Aogashima - Japan Meteorological Agency Шаблон:In lang
- Шаблон:Cite web - Japan Meteorological Agency
- Aogashima - Geological Survey of Japan
- Шаблон:Cite gvp
Шаблон:Tokyo Шаблон:Authority control
- ↑ 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.
- ↑ Nussbaum, Louis-Frédéric. (2005). "Izu Shotō," Japan Encyclopedia, p. 412.
- ↑ Шаблон:Cite web
- Страницы с неработающими файловыми ссылками
- Английская Википедия
- Izu Islands
- Active volcanoes
- Islands of Tokyo
- VEI-5 volcanoes
- Calderas of Japan
- Important Bird Areas of the Nanpo Islands
- Страницы, где используется шаблон "Навигационная таблица/Телепорт"
- Страницы с телепортом
- Википедия
- Статья из Википедии
- Статья из Английской Википедии