In this article, we will delve into the fascinating world of Chirinkotan. We will explore its origins, its impact on current society and possible future developments related to this topic. From its inception to the present, Chirinkotan has aroused great interest in various areas, attracting both experts and people interested in better understanding its relevance. Throughout these pages, we will analyze its many facets and how it has influenced people's lives. Without a doubt, Chirinkotan is a topic that will not leave anyone indifferent, and we are sure that this article will be of great interest to all those who wish to learn more about it.
Native name: Чиринкотан 知林古丹島 | |
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![]() Astronaut photograph of Chirinkotan Island from the International Space Station | |
Geography | |
Location | Sea of Okhotsk |
Coordinates | 48°59′N 153°29′E / 48.98°N 153.48°E |
Archipelago | Kuril Islands |
Area | 6 km2 (2.3 sq mi) |
Highest elevation | 742 m (2434 ft) |
Highest point | Masaochi Peak volcano (last eruption 2013 to 2014) |
Administration | |
Russia | |
Demographics | |
Population | 0 |
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".[citation needed] It is located 3 kilometres (1.9 miles) west of Ekarma, its nearest neighbor.
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, and is still an 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.
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.
In the spring and early summer crested, whiskered, and parakeet auklet nest on the island.[2]