Search results
Results from the WOW.Com Content Network
Volcanic island, an island of volcanic origin; Taal Volcano, an island volcano in the Philippines; Volcano Islands, a group of volcanic islands near Japan; Vulcano Island, a small volcanic island in the Tyrrhenian Sea
The Volcano Islands (火山列島, Kazan Rettō) or Iwo Islands (硫黄列島, Iō-rettō) are a group of three Japanese-governed islands in Micronesia. They lie south of the Ogasawara Islands and belong to the municipality of Ogasawara, Tokyo , Tokyo Metropolis , Japan.
With 677.7 square kilometres (261.7 sq mi) of surface area, it is the fifth largest island in the country. The summit at the centre of the island is dominated by a desert-like caldera, which covers an area of 100 square kilometres (39 sq mi). [1] With the exception of human settlements, the rest of the island is covered by a dense jungle. [5]
Nishinoshima (Japanese: 西之島, "western island") is a volcanic island located around 940 km (584 mi) south-southeast of Tokyo that is part of the Volcano Islands arc. . Nishinoshima is located about 130 km to the west of the nearest inhabited Ogasawara islands, Chichijima Island, hence the name; the other Ogasawara island groups are aligned more to the north–
Ahyi can be found in the southeast of the island. Ahyi is a submarine volcano which can be found in the northern portion of the Mariana Arc. The structure of the volcano consists of a 12 km (7 mi)-wide stratovolcanic cone that rises from around 2,000 m (6,562 ft) depth to 75 m (246 ft).
The island had three volcanoes. Perboewatan (410 ft) and Danan (1,480 ft) were destroyed during the eruption, and Rakata (2,667 ft) was half destroyed and the surviving half remains above sea level. In 1928, a new volcano called Anak Krakatoa (1,063 ft) grew above sea level, forming a new island by Rakata's island. 4 Volcán de Fuego [25] Guatemala
The Jeju Volcanic Island and Lava Tubes (Korean: 제주 화산섬과 용암 동굴) is a World Heritage Site in South Korea. [1] It was inscribed as one of the UNESCO World Heritage Sites in 2007 because of the Geomunoreum Lava Tube System and the exhibition of diverse and accessible volcanic features which are considered to demonstrate a distinctive and valuable contribution to the ...
Sakurajima's activity became more prominent in 1955, and the volcano has been erupting almost constantly ever since. Thousands of small explosions happen each year, throwing ash to heights of up to a few kilometers above the mountain. The Sakurajima Volcano Observatory was set up in 1960 to monitor these eruptions. [11]