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Geological Formation

Algar do Carvao

Volcanic Formations

Algar do Carvao is a volcanic cave on Terceira Island in the Azores, Portugal, formed within the Pico Alto volcanic system as a combined volcanic chimney and lava tube. After an eruption fed magma up through the vent, much of the molten rock later drained back downward, leaving behind a near-vertical shaft roughly 45 meters deep opening into a wide underground chamber. The lower part of the cave is flooded by a small lake, and its walls are lined with unusual stalactite-like mineral formations built from silica rather than the calcium carbonate typical of limestone caves, a rare feature that makes it one of the few volcanic caves in the world known for this kind of speleothem.

Facts
Classification
Protected Status
Locally or Regionally Protected 1
Connections

Associated With

Basalt, Materials
Source Algar do Carvao (Wikipedia)

Caused By

Volcanism, Processes
Source Algar do Carvao (Wikipedia)

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Found In

Also in Geography Atlas: where this subject is found.

Sources
1. Algar do Carvao (Wikipedia)
  • Protection section
    The 40.5 hectares (4,360,000 ft2) extent was classified as a Regional National Monument
  • Caused By: Volcanism, Lead, process Volcanism
    The Algar do Carvão (Cavern of Coal) is an ancient lava tube or volcanic vent located in the central part of the island of Terceira in the Portuguese archipelago of the Azores.
  • Associated With: Basalt, Infobox: geology
    Lava tube, Basalt
View the Source
Wikidata: Algar do Carvao
Wikidata Q4723949, class allow-list match (w-wdresolver-0926)View the Source
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