Oshima (Hokkaido)

Ōshima (大島) (means "big island") is an uninhabited island in the Sea of Japan, 50 kilometers (31 mi) to the west from Matsumae town and therefore the westernmost point of Hokkaido. It is part of the town of Matsumae in Oshima Subprefecture in Hokkaido, Japan. To distinguish Ōshima from other islands with the same name, it is sometimes known as Oshima Ōshima (渡島大島) or Matsumae Ōshima (松前大島).

Ōshima
Native name:
大島, Ōshima
Geography
LocationEast Asia
Coordinates41°30′N 139°23′E
ArchipelagoJapanese archipelago
Area9.73 km2 (3.76 sq mi)
Width4 km (2.5 mi)
Highest elevation732.4 m (2,402.9 ft)
Highest pointMount Era
Administration
Japan
PrefectureHokkaido
SubprefectureOshima Subprefecture
DistrictMatsumae District
TownMatsumae

At 9.73 square kilometers (3.76 sq mi), Ōshima is the largest uninhabited island under Japanese sovereignty. The island is a double caldera with a scoria hill rising in the middle. It is the peak of two overlapping stratovolcanoes and their associated calderas, Mount Higashi and Mount Nishi.[1] The highest peak, Mount Era (江良岳, Era-dake) at 737 meters (2,418 ft),[2] is part of a triple volcano. The peak rises close to 2,000 meters (6,600 ft) from the sea floor. The island consists of mafic alkali and non-alkali volcanic rock, less than 18,000 years old.[3]

On the south side of the island at Aidomari (北風泊, Aidomari), there is a lighthouse and a heliport operated by Japan Coast Guard.

Because of volcanic activity and nature conservation, landing on the island requires the approval of the Agency for Cultural Affairs.

History

Because of the island's isolation and volcanic activity there are almost no records of its past left behind. Mount Kanpo (寛保岳, Kanpo-dake) had a major eruption on 27 August 1741, which created a large horseshoe-shaped caldera breached to the north and extending from the summit down to the sea floor at the base of the volcano. This event produced a mostly submarine debris avalanche that traveled 16 km distance, and triggered a large tsunami. The tsunami devastated the coasts of Hokkaido, western Honshu, and as far as Korea, causing nearly 1500 deaths. The 1741 eruption was the largest in historical time at Ōshima and it ended with the construction of a basaltic cinder cone at the head of the breached caldera. No eruptions have occurred since the last eruption in 1790, but seismic unrest under the volcano occurred in 1996.

Flora and fauna

Ōshima is the northern limit of the breeding grounds for the streaked shearwater and is part of the Matsumae-Yakoshi Prefectural Natural Park. Baird's beaked whales are targets of commercial whaling in the nearby waters.[4]

gollark: Also, you indirectly contributed to potatOS.
gollark: I mean, how do you fix it and also not allow the weirdness?
gollark: That sounds weird and arbitrary, but whatever; how do you fix that?
gollark: Okay.
gollark: I don't see what you mean by "preventing tail calls" and somehow that putting it in the right place.

See also

References
  1. "Oshima-Oshima". Global Volcanism Program. Smithsonian National Museum of Natural History. Retrieved 2008-12-13.
  2. "OSHIMA O-SHIMA". Quaternary Volcanoes in Japan. Geological Survey of Japan, AIST. 2006. Retrieved 2008-12-13.
  3. "Hokkaido". Seamless Digital Geological Map of Japan. Geological Survey of Japan, AIST. Nov 2, 2007. Retrieved 2008-12-13.
  4. Kasuya T.(jp). 2017. Small Cetaceans of Japan: Exploitation and Biology. "13.3.2 Regional distribution and population structure". CRC Press. Retrieved on September 25, 2017

Sources
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