Lewati ke konten utama
Kembali ke peta
BandingkanLihat di peta

Cile · Kaldera

Calabozos

Tipe
Kaldera
Ketinggian
3508 m
Letusan terakhir
Tidak diketahui
The 26 x 14 km late-Pleistocene Calabozos caldera contains several post-caldera vents of Holocene age. The Descabezado Chico group (mid right-center) was constructed over the buried western rim of the caldera. The Cerro de Medio group (mid extreme-right) grew within the southern part of the caldera. No historical eruptions are known, but hot-spring clusters occur within the caldera.
The 26 x 14 km late-Pleistocene Calabozos caldera contains several post-caldera vents of Holocene age. The Descabezado Chico group (mid right-center) was constructed over the buried western rim of the caldera. The Cerro de Medio group (mid extreme-right) grew within the southern part of the caldera. No historical eruptions are known, but hot-spring clusters occur within the caldera. · Foto: Photo by Hugo Moreno (University of Chile).
Tipe
Kaldera
Negara
Cile
Wilayah
Amerika Selatan / Southern Andean Volcanic Arc
Ketinggian
3508 m
Koordinat
-35.558, -70.496
Letusan terakhir
Tidak diketahui
Kondisi tektonik
Zona subduksi / Kerak benua (> 25 km)
Bentuk lahan
Komposit
Batuan utama
Dasit

Ringkasan geologi

Teks asli bahasa Inggris

The composite late-Pleistocene Calabozos caldera (14 x 26 km) produced major rhyodacitic-to-dacitic ashflow sheets of ~200-500 km3 each, collectively referred to as the Loma Seca Tuff, at 800,000, 300,000, and 150,000 years ago.

Kutipan dari Global Volcanism Program, Smithsonian Institution · Baca ringkasan lengkap di GVP →

Ringkasan Wikipedia

Ringkasan Inggris

Calabozos is a Holocene caldera in central Chile's Maule Region.

Wikipedia · CC BY-SA · Lanjutkan membaca di Wikipedia bahasa Inggris →

Riwayat letusan

Glosarium

Garis waktu rinci

Tidak ada catatan letusan.

Gunung api terdekat

Tautan eksternal

⚠ Untuk referensi saja. Bukan untuk tanggap darurat.