Chirinkotan

Chirinkotan (Russian: Чиринкотан; Japanese 知林古丹島; Chirinkotan-tō) is an uninhabited volcanic island located in the centre of the Kuril Islands chain in the Sea of Okhotsk in the northwest Pacific Ocean. Its name is derived from the Ainu language for "mudslide". It is located 3 kilometres (1.9 miles) west of Ekarma, its nearest neighbor.

Chirinkotan
Native name:
Чиринкотан
知林古丹島
NASA picture of Chirinkotan Island
Geography
LocationSea of Okhotsk
Coordinates48.98°N 153.48°E / 48.98; 153.48
ArchipelagoKuril Islands
Area6 km2 (2.3 sq mi)
Highest elevation742 m (2,434 ft)
Highest pointMasaochi Peak volcano (last eruption 2013 to 2014)
Administration
Russia
Demographics
Population0

Geology

Chirinkotan is at the far end of a volcanic chain extending nearly 50 km west of the central part of the main Kuril Islands arc. The island is the top of a partially submerged stratovolcano rising approximately 3,000 metres (9,800 feet) from the floor of the Sea of Okhotsk, and is roughly circular with an area of 6 square kilometres (2.3 square miles).[1] The island's highest point ("Masaochi" in Ainu) is 742 metres (2,434 feet) high, is still active volcano with major eruptions recorded in 1760, 1884, 1900, 1979, 1986, 2004, and 2013. Reports of a 1955 eruption are unconfirmed. The caldera is approximately one kilometre (0.62 miles) wide, with a depth of 300 to 400 metres (980–1,310 feet), and is breached on its south-east side. The shores of the island are steep cliffs, making landing by small boat impossible.

History

Chirinkotan has had no permanent habitation. Claimed by the Empire of Russia, sovereignty was passed to the Empire of Japan per the Treaty of Saint Petersburg along with the rest of the Kuril Islands. The island was formerly administered as part of Shumushu District of Nemuro Subprefecture of Hokkaidō. After World War II, the island came under the control of the Soviet Union, and is now administered as part of the Sakhalin Oblast of the Russian Federation.

Fauna

In the spring and early summer crested, whiskered, and parakeet auklet nest on the island.[2]

gollark: So that's how people have homes in various secret GTech™ facilities.
gollark: Of course. They could also use a way to synchronize multiple tape drives better, and/or sync them with ticks.
gollark: It reminds me of the plethora portable keyboard thing.
gollark: I never actually did this, but it might have been cool to.
gollark: A nice thing about DFPWM is that you could theoretically encode it from CC, since the codec was very simple.

See also

References
  • "Chirinkotan". Global Volcanism Program. Smithsonian Institution.
  • "Oceandots entry". Archived from the original on December 23, 2010. Retrieved December 5, 2009.CS1 maint: BOT: original-url status unknown (link)

Further reading
  • Gorshkov, G. S. Volcanism and the Upper Mantle Investigations in the Kurile Island Arc. Monographs in geoscience. New York: Plenum Press, 1970. ISBN 0-306-30407-4
  • Krasheninnikov, Stepan Petrovich, and James Greive. The History of Kamtschatka and the Kurilski Islands, with the Countries Adjacent. Chicago: Quadrangle Books, 1963.
  • Rees, David. The Soviet Seizure of the Kuriles. New York: Praeger, 1985. ISBN 0-03-002552-4
  • Takahashi, Hideki, and Masahiro Ōhara. Biodiversity and Biogeography of the Kuril Islands and Sakhalin. Bulletin of the Hokkaido University Museum, no. 2-. Sapporo, Japan: Hokkaido University Museum, 2004.

Notes
  1. "International Kuril Island Project（IKIP）". University of Washington Fish Collection or the respective authors. Archived from the original on 2013-07-23. Retrieved 2009-12-05.
  2. Kondratyev, A. Y., Litvinenko, N. M., Shibaev, Y. V., Vyatkin, P. S., & Kondratyeva, L. F. (2000). "The breeding seabirds of the Russian Far East". Seabirds of the Russian Far East, 37-81.


This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.