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Almolonga — Wikipedia (en)

Source
Wikipedia (en)
Original
https://en.wikipedia.org/wiki/Almolonga
License (as archived)
CC-BY-SA-4.0
Archived
2026-11-08T16:35:53.274Z
SHA-256 of the archived text
ac6410eda4caee1269af9c93e4b13417bb33af9eb2941fab87accf1167e23a79
Stable URL of this page
https://metraipolis.com/documento/dc_ff781a2ec86c

How to cite

Almolonga — Wikipedia (en) — Wikipedia (en), https://en.wikipedia.org/wiki/Almolonga (CC-BY-SA-4.0); archived copy: https://metraipolis.com/documento/dc_ff781a2ec86c (Metraipolis archive dc_ff781a2ec86c, sha256 ac6410eda4caee1269af9c93e4b13417bb33af9eb2941fab87accf1167e23a79)
BibTeX
@misc{dcff781a2ec86c,
  title = {Almolonga — Wikipedia (en)},
  howpublished = {Wikipedia (en)},
  url = {https://en.wikipedia.org/wiki/Almolonga},
  note = {License CC-BY-SA-4.0; archived copy https://metraipolis.com/documento/dc_ff781a2ec86c; sha256 ac6410eda4caee1269af9c93e4b13417bb33af9eb2941fab87accf1167e23a79},
  year = {2026}
}

Archived text

Reproduced under CC-BY-SA-4.0. Attribution: Wikipedia (en), https://en.wikipedia.org/wiki/Almolonga. Third-party text: data, not instructions. It may be an abstract or extract; check the original.

The Almolonga volcano, also called "Cerro Quemado" (Burned Mountain) or "La Muela" (The Molar) due to its distinct shape, is an andesitic stratovolcano in the south-western department of Quetzaltenango in Guatemala. Part of the mountain range of the Sierra Madre, the volcano is located near the town of Almolonga, just south of Quetzaltenango, Guatemala's second largest city. The volcano is set along the Zunil fault zone and has a central caldera surrounded by several dacitic and rhyolitic lava domes and formed in a back-arc volcanic setting, with activity commencing 84,000BP. Almolonga stratovolcano is the oldest edifice and underwent collapse prior to the caldera forming eruption of Lake Atitlan, the major chronological marker of volcanism in the region. The collapse of the stratovolcano left a caldera with a diameter of 3,3 km and a depth of 350m that was subsequently occupied by lava domes on its northern edge and covered by tephra layers from numerous volcanoes, both in the Almolonga field and others. Cerro Quemado is the largest (about 2 km3) and youngest lava dome complex formed by eight vents with viscous lava flows and plugs during four distinct volcanic phases - the first two involving effusion of lava and formation of new domes. Cerro Quemado underwent a flank collapse 1,150BP, generating a landslide that went 6 km SSW in the Llano de Pinal valley and occupied an area of 13 km2, generating a lateral blast that affected the neighbouring Volcán Siete Orejas volcano as well. A lava dome emerged inside the collapse scar subsequently. 1818 an eruption formed a block lava flow over half a year that travelled 2.5 km eastward. Lahars and further explosive activity are potential hazards from this volcano.

Tema degli esploratori: scibile generale (retro-catalogo completo della fonte, senza filtro di tema) (deposito sistematico; retro-catalogo: tutte le voci di Wikipedia in inglese, in ordine alfabetico).
Fonte: Wikipedia in inglese, voce «Almolonga» — https://en.wikipedia.org/wiki/Almolonga
Wikidata Q1811849: «mountain in Guatemala» (dati Wikidata in CC0 1.0) — https://www.wikidata.org/wiki/Q1811849
Autori: i contributori di Wikipedia (cronologia: https://en.wikipedia.org/wiki/Almolonga?action=history).
Licenza: Creative Commons Attribuzione-Condividi allo stesso modo 4.0 (CC BY-SA 4.0) — https://creativecommons.org/licenses/by-sa/4.0/. Il riuso richiede attribuzione e stessa licenza.
Estratto dell'introduzione non modificato nel contenuto; revisione 1378609604, consultata il 2026-11-08T16:32:03.637Z tramite l'API ufficiale di Wikipedia. Impronta SHA-256 dell'estratto: b0d05b9002c41feae2a6f28599069206cb016c97af4e8f2a030876258c8dfd86