Huaynaputina
Stratovolkan · Peru · 4679 m

- Tipe
- Stratovolkan
- Negara
- Peru
- Wilayah
- South America Volcanic Regions / Central Andean Volcanic Arc
- Ketinggian
- 4679 m
- Koordinat
- -16.614, -70.854
- Letusan terakhir
- 1600
- Kondisi tektonik
- Subduction zone / Continental crust (> 25 km)
- Bentuk lahan
- Composite
- Batuan utama
- Dacite
Ringkasan geologi
Huaynaputina (whose name means "new volcano") was the source of the largest historical eruption of South America in 1600 CE. It has no prominent topographic expression and lies within a 2.5-km-wide collapse depression and further excavated by glaciers within a Tertiary to Pleistocene edifice. Three overlapping ash cones with craters up to 100 m deep were constructed during the 1600 CE eruption on the floor of the older crater, whose outer flanks are heavily mantled by ash deposits from the 1600 eruption. This powerful fissure-fed eruption may have produced nearly 30 km3 of dacitic tephra, including pyroclastic flows and surges that traveled 13 km to the E and SE. Lahars reached the Pacific Ocean, 120 km away. The eruption caused substantial damage to the major cities of Arequipa and Moquengua.
Ringkasan Wikipedia
Huaynaputina adalah sebuah gunung berapi kerucut yang terletak di Peru selatan. Gunung berapi ini tidak memiliki profil gunung yang diidentifikasi, tetapi memiliki bentuk besar kawah gunung berapi. Pada tanggal 19 Februari 1600, gunung ini meletus dan mendapat skala 6 dalam Volcanic Explosivity Index. Letusan gunung ini merupakan letusan terbesar di Amerika Selatan.
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Riwayat letusan
Garis waktu rinci
- 1600VEI 6Teramati1600-02-17 – 1600-03-06Summit and south flank
- 7750 SM (±200 tahun)VEI ?Perkiraan geologiBCE 7750 – Berlangsung
Tautan eksternal
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