The existence of the cavern had been known for a long time, but the depth and lack of ambient light, made any descent difficult, owing to the vertical descent, and delayed any real exploration. On 26 January 1893, the first descent, "...with the use of a simple rope, was accomplished by Cândido Corvelo and Luis Sequeira." The second descent was made in 1934, by Didier Couto, who produced the first rough map of the interior. This drawing, based on visual observations alone, turned out to be quite accurate. On 18 August 1963, a group of enthusiasts organized a descent using a "chair" platform suspended on a nylon line and, later, a harness. With the advent of portable lighting systems, it was possible to re-examine the observations first-hand, including the most remote and narrow sections of the cavern. The site was open to the public in the late 20th century, through weekly organized tours through the summer. Access to the site is also possible through the Montanheiros organization, the group responsible for matters associated with the Algar.
Toponymy
The word, algar, is a Portuguese word that denotes a natural cavity in the earth that, unlike most caves or caverns, is more vertical in its orientation, like a well. The Portuguese word derives from the Arabic word, al-Gar, which means "the crease", while Carvão means "coal" in Portuguese. The Algar do Carvão is not a source of coal, and the term carvão has also been used in the Portuguese vernacular akin to "blackened", "sooty" or "burnt", referring to the dark composition of the rocks.
Geography
Terceira is the site of four large volcanoes grouped along a basaltic fissure zone that transects the island from northwest to southeast. The Algar do Carvão is directly associated with the caldera of the Guilherme Moniz volcano, but it is part of the same complex as Santa Barbara to the west, Pico Alto to the north, and Guilherme Moniz, which is a short distance to the south of the Algar do Carvão site. Algar do Carvão is situated at above sea level. The extent was classified as a Regional National Monument due to its peculiar volcanological characteristics, in addition to its environmental ecosystem. The mouth of the Algar consists of a vertical passage to the interior, that reaches a ramp of debris and gravel. From here there is another decline to the clear waters of the interior pool, approximately from the level surface. The pool is supported by rainwater, and can reach as deep as depth or become dry in summer months, owing to little or no precipitation. The cave itself is remarkable for the unique mineralogical characteristics of its silicatestalactites.
