HOME

TheInfoList



OR:

The Caldeira Volcano ( Portuguese: ) is the highest mountain, massive
stratovolcano A stratovolcano, also known as a composite volcano, is a typically conical volcano built up by many alternating layers (strata) of hardened lava and tephra. Unlike shield volcanoes, stratovolcanoes are characterized by a steep profile with ...
and the largest geomorphological structure that forms the island of Faial. The mountain's highest point, Cabeço Gordo, reaches above sea level. One of the most notable features of this volcano is its two kilometer wide
caldera A caldera ( ) is a large cauldron-like hollow that forms shortly after the emptying of a magma chamber in a volcanic eruption. An eruption that ejects large volumes of magma over a short period of time can cause significant detriment to the str ...
, that is in depth below the crater rim.


History

Along the western edge of the Ribeirinha Volcano, the Central Volcanic Complex formed about 410,000 years ago, along with several structures that arose from tectonics. Evidence of this process has not been preserved due to subsidence, but it is generally believed that two formations (an Upper and Lower group) reflecting a geochemical variation that occurred about 16,000 years ago. The Lower group (from 410,000 years ago), was marked by the predominance of a Hawaiian/Strombolian eruptive process, that was composed of basaltic and benmoreitic rocks. The secondary, Upper group, was a highly explosive period (sub-Plinian in character), which produced a series of twelve deposits of pumice and surge deposits (pyroclastic flows of trachytic and benmoreitic). The volcano was reduced by around in height due to an eruption that occurred around 1000 years ago. This was one of the last major explosive events recorded in the Azores. Although the central volcano has not been active within the past two centuries, it has seen activity related to the eruption of Capelinhos (1957–58). During this period, fumaroles in the caldera became active, and the minor lakes/swamps were dried-up by excessive heat. The volcano, due to its central nature, is part of each parish on the island (except for Matriz, Conceição and Angustias).


Geography

The Caldeira Volcano is the main geomorphological unit, corresponding to a polygenetic volcano two kilometers at the top and one kilometer at the base. The walls of the crater rim are abrupt, although their slopes increase with altitudes. The superficial cover of the volcano is covered in pyroclastic material, such as pumice rock, phreatic and phreatomagmatic deposits, evidence of pyroclastic flows and lahars. The flanks of the stratovolcano also include the Morro de Castelo Branco and peninsula of denser material that have resisted erosion.


References

;Notes ;Sources * * * *{{cite journal, url=http://e-terra.geopor.pt/artigos/cong_geoq/machado.pdf, last=Machado, first=Adriane, author2=Azevedo, José M. M., author3=Alemeida, Delia P.M., author4=Farid Chemale Jr., title=Geochemistry of Volcanic Rocks from Faial Island (Azores), publisher=e-Terra, GEOTIC – Sociedade Geológica de Portugal, location=Lisbon, volume=5, 1, year=2008, pages=1–14, access-date=2010-08-22, archive-url=https://web.archive.org/web/20110511135248/http://e-terra.geopor.pt/artigos/cong_geoq/machado.pdf, archive-date=2011-05-11, url-status=dead Stratovolcanoes of Portugal Calderas of Portugal Geology of the Azores Faial Island