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Huaynaputina

Stratovolkan · Peru · 4679 m

Huaynaputina is a relatively inconspicuous volcano that was the source of one of the largest historical eruptions of the central Andes in 1600 CE.  The volcano has no prominent topographic expression.  This view is from the east into a 2.5-km-wide complex caldera that is breached widely to the east.  Three ash cones, one of which can be seen in the shadow at the right-center, are located on the floor of the caldera.  Light-colored ash deposits from the 1600 eruption can be seen mantling the caldera rim.
Huaynaputina is a relatively inconspicuous volcano that was the source of one of the largest historical eruptions of the central Andes in 1600 CE. The volcano has no prominent topographic expression. This view is from the east into a 2.5-km-wide complex caldera that is breached widely to the east. Three ash cones, one of which can be seen in the shadow at the right-center, are located on the floor of the caldera. Light-colored ash deposits from the 1600 eruption can be seen mantling the caldera rim. · Foto: Photo by Oscar González-Ferrán (University of Chile).
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.

Wikipedia · CC BY-SA · Baca artikel lengkap

Riwayat letusan

Ringkasan (VEI dari waktu ke waktu)
Klik pada bar untuk melihat letusan individu
7750 BCE~7438 BCE · 1 letusan · VEI maks. ?1288~1600 · 1 letusan · VEI maks. 67750 BCE5568 BCE3075 BCE893 BCE1288

Garis waktu rinci

  1. 1600VEI 6Teramati
    1600-02-17 – 1600-03-06
    Summit and south flank
  2. 7750 SM (±200 tahun)VEI ?Perkiraan geologi
    BCE 7750 – Berlangsung

Tautan eksternal

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