Jepang · Stratovolkan
Kuchinoerabu Island
Kuchinoerabujima
- Tipe
- Stratovolkan
- Ketinggian
- 657 m
- Letusan terakhir
- 2020
- Tipe
- Stratovolkan
- Negara
- Jepang
- Wilayah
- Pasifik Barat / Ryukyu Volcanic Arc
- Ketinggian
- 657 m
- Koordinat
- 30.443, 130.217
- Letusan terakhir
- 2020
- Kondisi tektonik
- Zona subduksi / Kerak samudra (< 15 km)
- Bentuk lahan
- Komposit
- Batuan utama
- Andesit / Andesit basaltik
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.
Wikipedia · CC BY-SA · Baca artikel lengkap →
Riwayat letusan
31 tercatatGlosariumGaris 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 1Metode tidak dinyatakan1932-07-23 – 1932-07-23Shindake
- 1931VEI 3Teramati1931-04-02 – 1931-06-22SW flank of Shindake
- 1914VEI 2Teramati1914-01-05 – akhir tidak diketahuiShindake
- 1906VEI ?Metode tidak dinyatakan1906-07-02 – 1907-07-02Shindake
- 1841VEI 2Teramati1841-05-23 – 1841-08-01Shindake
- 1840VEI 2Teramati1840-07-02 – akhir tidak diketahuiShindake
- 1560 (±100 tahun)VEI ?Perkiraan geologi1560 – akhir tidak diketahuiFurudake
- 1470 (±50 tahun)VEI ?Perkiraan geologi1470 – akhir tidak diketahuiFurudake
- 1440 (±50 tahun)VEI ?Perkiraan geologi1440 – akhir tidak diketahuiShindake
- 1110 (±75 tahun)VEI ?Perkiraan geologi1110 – akhir tidak diketahuiFurudake
- 1100 (±100 tahun)VEI ?Perkiraan geologi1100 – akhir tidak diketahuiShindake
- 970 (±75 tahun)VEI ?Perkiraan geologi970 – akhir tidak diketahuiFurudake
- 600 (±75 tahun)VEI ?Perkiraan geologi600 – akhir tidak diketahuiShindake
- 1140 SM (±150 tahun)VEI ?Perkiraan geologi1140 SM – akhir tidak diketahuiFurudake
- 1450 SM (±75 tahun)VEI ?Perkiraan geologi1450 SM – akhir tidak diketahuiShindake
- 3480 SM (±150 tahun)VEI ?Perkiraan geologi3480 SM – akhir tidak diketahuiFurudake
- 9520 SM (±300 tahun)VEI ?Perkiraan geologi9520 SM – akhir tidak diketahuiFurudake
Gunung api terdekat
Tautan eksternal
⚠ Untuk referensi saja. Bukan untuk tanggap darurat.