Kuchinoerabu Island
Kuchinoerabujima
Stratovolkan · Japan · 657 m

- Tipe
- Stratovolkan
- Negara
- Japan
- Wilayah
- Western Pacific Volcanic Regions / Ryukyu Volcanic Arc
- Ketinggian
- 657 m
- Koordinat
- 30.443, 130.217
- Letusan terakhir
- 2020
- Kondisi tektonik
- Subduction zone / Oceanic crust (< 15 km)
- Bentuk lahan
- Composite
- Batuan utama
- Andesite / Basaltic Andesite
Ringkasan geologi
A group of young stratovolcanoes forms the eastern end of the irregularly shaped island of Kuchinoerabujima in the northern Ryukyu Islands, 15 km W of Yakushima. The Furudake, Shindake, and Noikeyama cones were erupted from south to north, respectively, forming a composite cone with multiple craters. All historical eruptions have occurred from Shindake, although a lava flow from the S flank of Furudake that reached the coast has a very fresh morphology. Frequent explosive eruptions have taken place from Shindake since 1840; the largest of these was in December 1933. Several villages on the 4 x 12 km island are located within a few kilometers of the active crater and have suffered damage from eruptions.
Ringkasan Wikipedia
Ringkasan InggrisKuchinoerabu-jima , is one of the Satsunan Islands, usually classed with the Ōsumi Islands belonging to Kagoshima Prefecture, Japan. The island, 38.04 km2 (14.69 sq mi) in area, has a population of 147. The island can only be reached by boat as it has no airport. There is regular ferry service with Yakushima, which is about 15 km to the east. Travel time is approximately 1 hour. The islanders are dependent mainly on fishing, agriculture and seasonal tourism. The entire island is within the borders of the Kirishima-Yaku National Park.
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Riwayat letusan
Garis waktu rinci
- 2020VEI 3Teramati2020-01-11 – 2020-05-13
- 2020VEI 1Teramati2020-08-29 – 2020-08-29
- 2018VEI 3Teramati2018-10-21 – 2019-02-03Shindake Crater
- 2015VEI 3Teramati2015-05-29 – 2015-06-19Shindake crater
- 2014VEI 1Teramati2014-08-03 – 2014-08-03Shindake
- 1980VEI 2Teramati1980-09-28 – 1980-09-28NNE-SSW fissure on E side of Shindake
- 1976VEI 2Teramati1976-04-02 – 1976-04-02Shindake
- 1974VEI 1Teramati1974-06-03 – 1974-06-03Shindake
- 1973VEI 2Teramati1973-11-05 – 1973-11-19Shindake
- 1972VEI 2Teramati1972-09-02 – 1972-09-02Shindake
- 1968VEI 3Teramati1968-12-21 – 1969-03-10Shindake
- 1966VEI 2Teramati1966-11-22 – 1966-11-22Shindake
- 1945VEI 2Teramati1945-11-03 – 1945-11-03NNE-SSW fissure on E side of Shindake
- 1933VEI 4Teramati1933-12-23 – 1934-01-12Shindake
- 1932VEI 1Perkiraan geologi1932-07-23 – 1932-07-23Shindake
- 1931VEI 3Teramati1931-04-02 – 1931-06-22SW flank of Shindake
- 1914VEI 2Teramati1914-01-05 – BerlangsungShindake
- 1906VEI ?Perkiraan geologi1906 – 1907Shindake
- 1841VEI 2Teramati1841-05-23 – 1841-08-01Shindake
- 1840VEI 2Teramati1840 – BerlangsungShindake
- 1560 (±100 tahun)VEI ?Perkiraan geologi1560 – BerlangsungFurudake
- 1470 (±50 tahun)VEI ?Perkiraan geologi1470 – BerlangsungFurudake
- 1440 (±50 tahun)VEI ?Perkiraan geologi1440 – BerlangsungShindake
- 1110 (±75 tahun)VEI ?Perkiraan geologi1110 – BerlangsungFurudake
- 1100 (±100 tahun)VEI ?Perkiraan geologi1100 – BerlangsungShindake
- 970 (±75 tahun)VEI ?Perkiraan geologi970 – BerlangsungFurudake
- 600 (±75 tahun)VEI ?Perkiraan geologi600 – BerlangsungShindake
- 1140 SM (±150 tahun)VEI ?Perkiraan geologiBCE 1140 – BerlangsungFurudake
- 1450 SM (±75 tahun)VEI ?Perkiraan geologiBCE 1450 – BerlangsungShindake
- 3480 SM (±150 tahun)VEI ?Perkiraan geologiBCE 3480 – BerlangsungFurudake
- 9520 SM (±300 tahun)VEI ?Perkiraan geologiBCE 9520 – BerlangsungFurudake
Tautan eksternal
⚠ Untuk referensi saja. Bukan untuk tanggap darurat.