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Volcán Apoyeque

Apoyeque

Kaldera · Nicaragua · 518 m

Apoyeque stratovolcano forms the large Chiltepe Peninsula in central Lake Managua.  A 2.8-km wide, 500-m-deep caldera truncates the volcano's summit, below and to the left of the airplane wing.  Laguna de Jiloa, the large lake in the foreground, lies immediately SE of Apoyeque.  The age of the latest eruption of Apoyeque is not known, but human footprints underlie pumice deposits thought to originate from Apoyeque volcano or a nearby vent beneath Lake Managua.  Momotombo volcano is visible in the distance to the NW across Lake Managua.
Apoyeque stratovolcano forms the large Chiltepe Peninsula in central Lake Managua. A 2.8-km wide, 500-m-deep caldera truncates the volcano's summit, below and to the left of the airplane wing. Laguna de Jiloa, the large lake in the foreground, lies immediately SE of Apoyeque. The age of the latest eruption of Apoyeque is not known, but human footprints underlie pumice deposits thought to originate from Apoyeque volcano or a nearby vent beneath Lake Managua. Momotombo volcano is visible in the distance to the NW across Lake Managua. · Foto: Photo by Jaime Incer, 1981. · Wikimedia Commons
Tipe
Kaldera
Negara
Nicaragua
Wilayah
Middle America-Caribbean Volcanic Regions / Central America Volcanic Arc
Ketinggian
518 m
Koordinat
12.242, -86.342
Letusan terakhir
-50
Kondisi tektonik
Subduction zone / Continental crust (> 25 km)
Bentuk lahan
Caldera
Batuan utama
Dacite
Ringkasan geologi

The Apoyeque volcanic complex occupies the broad Chiltepe Peninsula, which extends into south-central Lake Managua. The peninsula is part of the Chiltepe pyroclastic shield volcano, one of three large ignimbrite shields on the Nicaraguan volcanic front. A 2.8-km wide, 400-m-deep, lake-filled caldera whose floor lies near sea level truncates the low Apoyeque edifice, which rises only about 500 m above the lake shore. The caldera was the source of a thick deposit of dacitic pumice that covers the surrounding area. The 2.5 x 3 km lake-filled Xiloá (Jiloá) maar is located immediately SE of Apoyeque. The Talpetatl lava dome was constructed between Laguna Xiloá and Lake Managua. Pumiceous pyroclastic flows from Laguna Xiloá were erupted about 6,100 years ago and overlie deposits of comparable age from the Masaya Plinian eruption.

Ringkasan Wikipedia

Ringkasan Inggris

Apoyeque is a pyroclastic shield, located in the Chiltepe Peninsula Natural Reserve in Nicaragua. It has a 2.8-km wide, 400-m-deep, lake-filled caldera.

Wikipedia · CC BY-SA · Baca artikel lengkap

Riwayat letusan

Ringkasan (VEI dari waktu ke waktu)
Klik pada bar untuk melihat letusan individu
4160 BCE~3964 BCE · 1 letusan · VEI maks. 52594 BCE~2399 BCE · 1 letusan · VEI maks. 51224 BCE~1029 BCE · 1 letusan · VEI maks. 4246 BCE~50 BCE · 1 letusan · VEI maks. 64160 BCE3181 BCE2203 BCE1224 BCE246 BCE

Garis waktu rinci

  1. 50 SM (±100 tahun)VEI 6Perkiraan geologi
    BCE 50 – Berlangsung
    Apoyeque
  2. 1050 SM (±1000 tahun)VEI 4Perkiraan geologi
    BCE 1050 – Berlangsung
  3. 2550 SM (±1500 tahun)VEI 5Perkiraan geologi
    BCE 2550 – Berlangsung
    W Chiltepe Peninsula
  4. 4160 SM (±30 tahun)VEI 5Perkiraan geologi
    BCE 4160 – Berlangsung
    Laguna Xiloá

Tautan eksternal

⚠ Untuk referensi saja. Bukan untuk tanggap darurat.