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São Vicente Caves
The São Vicente Caves (Grutas de São Vicente in Portuguese) are caves located in the parish and county of São Vicente, Madeira. Entrance is charged at €8 for adults, but have been closed since March 2020. History These caves were formed around 890,000 years ago from a volcanic eruption in Paul da Serra that ran down to the sea. Thus, the outside, exposed to lower temperatures solidified rapidly while the inner liquid continued to run with many gases, forming a series of lava tubes, which today constitute the caves of São Vicente. They were first discovered in 1885, by local people who informed James Yate Johnson an English naturalist in Madeira who explored the caves further. The caves were opened to the public on 1 of October 1996, being one of the first caves of volcanic origins to be opened to the public in Portugal. See also *Furnas do Cavalum The Furnas do Cavalum (Caves of Cavalum in English) are a group of four caves located in Machico Machico () is a muni ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
São Vicente, Madeira
São Vicente () is a municipality along the north-west coast of the island of Madeira. History The first human visitors to São Vicente appeared in the middle of the 15th century, colonizing the area much later than the settlers in the southern part of the island, owing to its fertility. This area of the island, due to its steep escarpments and deep river-valleys made early settlement difficult. The first settlers appeared in the areas of São Vicente and Ponta Delgada, respectively. The progressive growth of its population led to dis-annexation of São Vicente from the Captaincy of Machico, and elevation to municipal seat by royal charter on 23 August 1774. At that time the parishes of Porto Moniz, Seixal, Arco de São Jorge and São Jorge where under the administration of the municipal authority. In 1835, the restructuring of municipal government under the Liberal reformer Mouzinho da Silveira lead to the creation of two new municipalities (Santana and Porto Moniz) along the nor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lava Tube
A lava tube, or pyroduct, is a natural conduit formed by flowing lava from a volcanic vent that moves beneath the hardened surface of a lava flow. If lava in the tube empties, it will leave a cave. Formation A lava tube is a type of lava cave formed when a low-viscosity lava flow develops a continuous and hard crust, which thickens and forms a roof above the still-flowing lava stream. Tubes form in one of two ways: either by the crusting over of lava channels, or from pāhoehoe flows where the lava is moving under the surface. Lava usually leaves the point of eruption in channels. These channels tend to stay very hot as their surroundings cool. This means they slowly develop walls around them as the surrounding lava cools and/or as the channel melts its way deeper. These channels can get deep enough to crust over, forming an insulating tube that keeps the lava molten and serves as a conduit for the flowing lava. These types of lava tubes tend to be closer to the lava erupt ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Basalt
Basalt (; ) is an aphanite, aphanitic (fine-grained) extrusive igneous rock formed from the rapid cooling of low-viscosity lava rich in magnesium and iron (mafic lava) exposed at or very near the planetary surface, surface of a terrestrial planet, rocky planet or natural satellite, moon. More than 90% of all volcanic rock on Earth is basalt. Rapid-cooling, fine-grained basalt is chemically equivalent to slow-cooling, coarse-grained gabbro. The eruption of basalt lava is observed by geologists at about 20 volcanoes per year. Basalt is also an important rock type on other planetary bodies in the Solar System. For example, the bulk of the plains of volcanism on Venus, Venus, which cover ~80% of the surface, are basaltic; the lunar mare, lunar maria are plains of flood-basaltic lava flows; and basalt is a common rock on the surface of Mars. Molten basalt lava has a low viscosity due to its relatively low silica content (between 45% and 52%), resulting in rapidly moving lava flo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stalactites
A stalactite (, ; from the Greek 'stalaktos' ('dripping') via ''stalassein'' ('to drip') is a mineral formation that hangs from the ceiling of caves, hot springs, or man-made structures such as bridges and mines. Any material that is soluble and that can be deposited as a colloid, or is in suspension, or is capable of being melted, may form a stalactite. Stalactites may be composed of lava, minerals, mud, peat, pitch, sand, sinter, and amberat (crystallized urine of pack rats). A stalactite is not necessarily a speleothem, though speleothems are the most common form of stalactite because of the abundance of limestone caves. The corresponding formation on the floor of the cave is known as a stalagmite. Mnemonics have been developed for which word refers to which type of formation; one is that ''stalactite'' has a C for "ceiling", and ''stalagmite'' has a G for "ground". Another example is that ''stalactites'' "hang on ''T''ight" and ''stalagmites'' "''M''ight grow up" ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stalagmites
A stalagmite (, ; from the Greek , from , "dropping, trickling") is a type of rock formation that rises from the floor of a cave due to the accumulation of material deposited on the floor from ceiling drippings. Stalagmites are typically composed of calcium carbonate, but may consist of lava, mud, peat, pitch, sand, sinter, and amberat (crystallized urine of pack rats). The corresponding formation hanging down from the ceiling of a cave is a stalactite. Mnemonics have been developed for which word refers to which type of formation; one is that ''stalactite'' has a C for "ceiling", and ''stalagmite'' has a G for "ground", another is that, as with ants in the pants, the mites go up and the tights (tites) come down. Formation and type Limestone stalagmites The most common stalagmites are speleothems, which usually form in limestone caves. Stalagmite formation occurs only under certain pH conditions within the cavern. They form through deposition of calcium carbonate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Paul Da Serra
Paul da Serra in the municipal county of Ponta do Sol, Madeira, is the largest and most extensive plateau of Madeira, at about , with an altitude averaging about . Its highest point is the peak pico do Paul at from where the length of the entire plateau can be viewed. On days with good visibility, both the south and north coasts are visible. Paul da Serra is considered the most important area of the islands groundwater recharge, and their planar structure facilitates the infiltration of a significant part of high rainfall year, while slowing the runoff towards the sea. The ground cover in almost all the Paul da Serra is composed of underbrush, reminiscent of its former use as grazing site, stressing among other the Feiteira ('' Pteridium aquilinum''), highland bent, (''Agrostis castellana''), broom ('' Cytisus scoparius'' ssp. ''scoparius'', '' C. striatus'' and '' C. multiflorus)'', the gorse ('' Ulex europaeus'' ssp. ''latebracteatus'' and ''U. minor ''Ulmus minor'' Mil ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lava Tubes
A lava tube, or pyroduct, is a natural conduit formed by flowing lava from a volcanic vent that moves beneath the hardened surface of a lava flow. If lava in the tube empties, it will leave a cave. Formation A lava tube is a type of lava cave formed when a low-viscosity lava flow develops a continuous and hard crust, which thickens and forms a roof above the still-flowing lava stream. Tubes form in one of two ways: either by the crusting over of lava channels, or from pāhoehoe flows where the lava is moving under the surface. Lava usually leaves the point of eruption in channels. These channels tend to stay very hot as their surroundings cool. This means they slowly develop walls around them as the surrounding lava cools and/or as the channel melts its way deeper. These channels can get deep enough to crust over, forming an insulating tube that keeps the lava molten and serves as a conduit for the flowing lava. These types of lava tubes tend to be closer to the lava erupt ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
James Yate Johnson
James Yate Johnson (1820, in Kendal, Westmorland – 2 February 1900, in Funchal) was an English naturalist. Johnson lived in Madeira from around 1851, studied marine fish, crustacea, sea anemones and sponges and terrestrial spiders, flowering plants and mosses. He collected specimens for other naturalists; for instance, George Busk, who in 1859 wrote "Zoophytology: On some Madeiran Polyzoa." Collected by J. Yates Johnson, Esq. in the ''Quarterly Journal of Microscopical Science'', vol. 7, pp. 65–67. He discovered '' Halargyreus johnsonii'' and ''Melanocetus johnsonii'' during his time in Madeira. Johnson explored the São Vicente Caves after being informed of their existence by locals on Madeira in 1885. The caves were opened to the public on 1 October 1996, being one of the first caves of volcanic origins to be opened to the public in Portugal. He was the son of John Henry Johnson and Ann Yate, also brother of John Henry Johnson (patent attorney). Works Partial list ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Furnas Do Cavalum
The Furnas do Cavalum (Caves of Cavalum in English) are a group of four caves located in Machico Machico () is a municipality, parish and city in the southeast part of the island of Madeira, in the Autonomous Region of Madeira. The easternmost municipality on the island, it is also the third-most populous area with a population of 21,828 in ..., Madeira. Named after a local legend about a demon called Cavalum, who was imprisoned in the cave. These lava tubes are of great importance allowing a view on the volcanic history of the now inactive island of Madeira, they have also biologic importance as there are several troglobionts living in the cave, including crustaceans, spiders and flies. At least fourteen invertebrates live in these tubes and at least three of them are endemic on Madeira island, one of them exists only in this cave. Furnas do Cavalum are also part of the cultural heritage of the islanders, as numerous legends are told about the caves. Despite the stories ab ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Caves Of Madeira
A cave or cavern is a natural void in the ground, specifically a space large enough for a human to enter. Caves often form by the weathering of rock and often extend deep underground. The word ''cave'' can refer to smaller openings such as sea caves, rock shelters, and grottos, that extend a relatively short distance into the rock and they are called ''exogene'' caves. Caves which extend further underground than the opening is wide are called ''endogene'' caves. Speleology is the science of exploration and study of all aspects of caves and the cave environment. Visiting or exploring caves for recreation may be called ''caving'', ''potholing'', or ''spelunking''. Formation types The formation and development of caves is known as '' speleogenesis''; it can occur over the course of millions of years. Caves can range widely in size, and are formed by various geological processes. These may involve a combination of chemical processes, erosion by water, tectonic forces, microorgani ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Show Caves In Madeira
Show or The Show may refer to: Competition, event, or artistic production * Agricultural show, associated with agriculture and animal husbandry * Animal show, a judged event in the hobby of animal fancy ** Cat show ** Dog show ** Horse show ** Specialty show, a dog show which reviews a single breed *Show, an artistic production, such as: ** Concert ** Radio show ** Talk show ** Television show ** Theatre production * Trade fair or trade show Arts, entertainment, and media Films * ''The Show'' (1922 film), starring Oliver Hardy * ''The Show'' (1927 film), directed by Tod Browning * ''The Show'' (1995 film), a hip hop documentary * ''The Show'' (2017 film), an American satirical drama * ''The Show'' (2020 film), a British mystery film Album * ''Show'' (The Cure album), 1993 * ''Show'' (The Jesus Lizard album), 1994 * ''The Show'' (album), a 2008 album by eMC Songs * "The Show" (Doug E. Fresh song) * "The Show" (Girls Aloud song) * "The Show" (Lenka song ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanism Of Madeira
Volcanism, vulcanism or volcanicity is the phenomenon of eruption of molten rock (magma) onto the surface of the Earth or a solid-surface planet or moon, where lava, pyroclastics, and volcanic gases erupt through a break in the surface called a vent. It includes all phenomena resulting from and causing magma within the crust or mantle of the body, to rise through the crust and form volcanic rocks on the surface. Magmas, that reach the surface and solidify, form extrusive landforms. Volcanic processes Magma from the mantle or lower crust rises through the crust towards the surface. If magma reaches the surface, its behavior depends on the viscosity of the molten constituent rock. Viscous (thick) magma produces volcanoes characterised by explosive eruptions, while non-viscous (runny) magma produce volcanoes characterised by effusive eruptions pouring large amounts of lava onto the surface. In some cases, rising magma can cool and solidify without reaching the surface. Instead, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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