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Friday, May 19, 2023

05-19-2023-0149 - A cave dweller, or troglodyte, etc. (draft)

From Wikipedia, the free encyclopedia
Cave dwellings in Mellieħa, Malta
Cave dwellings, Spiti, India

A cave dweller, or troglodyte, is a human who inhabits a cave or the area beneath the overhanging rocks of a cliff.

Prehistory

Some prehistoric humans were cave dwellers, but most were not (see Homo and Human evolution). Such early cave dwellers, and other prehistoric peoples, are also called cave men (the term also refers to the stereotypical "caveman" stock character type from fiction and popular culture). Despite the name, only a small portion of humanity has ever dwelt in caves: caves are rare across most of the world; most caves are dark, cold, and damp; and other cave inhabitants, such as bears and cave bears, cave lions, and cave hyenas, often made caves inhospitable for people.

The Grotte du Vallonnet, a cave in the French Riviera, was used by people approximately one million years ago. Although stone tools and the remains of eaten animals have been found in the cave, there is no indication that people dwelt in it.

Since about 750,000 years ago, the Zhoukoudian cave system, in Beijing, China, has been inhabited by various species of human being, including Peking Man (Homo erectus pekinensis) and modern humans (Homo sapiens).

Starting about 170,000 years ago, some Homo sapiens lived in some cave systems in what is now South Africa, such as Pinnacle Point and Diepkloof Rock Shelter. The stable temperatures of caves provided a cool habitat in summers and a warm, dry shelter in the winter. Remains of grass bedding have been found in nearby Border Cave.[1]

About 100,000 years ago, some Neanderthals dwelt in caves in Europe and western Asia. Caves there also were inhabited by some Cro-Magnons, from about 35,000 years ago until about 8000 B.C. Both species built shelters, including tents, at the mouths of caves and used the caves’ dark interiors for ceremonies. The Cro-Magnon people also made representational paintings on cave walls.[2]

Also about 100,000 years ago, some Homo sapiens worked in Blombos Cave, in what became South Africa. They made the earliest paint workshop now known, but apparently did not dwell in the caves.[3]

Writers of the classical Greek and Roman period made several allusions to cave-dwelling tribes in different parts of the world. For details, see "Troglodytae".[4]

Historical

Cave dwellings in Amboise, France
Cave dwellings in Amboise, Loire Valley, France

Especially during war and other times of strife, small groups of people have lived temporarily in caves, where they have hidden or otherwise sought refuge. They also have used caves for clandestine and other special purposes while living elsewhere.

Perhaps fleeing the violence of Ancient Romans, people left the Dead Sea Scrolls in eleven caves near Qumran, in what is now an area of the West Bank managed by Qumran National Park, in Israel. The documents remained undisturbed there for about 2,000 years, until their discovery in the 1940s and 1950s.

The DeSoto Caverns, in what became Alabama in the United States, were a burial ground for local tribes; the same caves became a violent speakeasy in the 1920s. The Caves of St. Louis may have been a hiding-place along the Underground Railroad.

From about 1000 to about 1300, some Pueblo people lived in villages that they built beneath cliffs in what is now the Southwestern United States.

In Hirbet Tawani, near Yatta Village, in the Southern Hebron Hills, in an area contested by the Palestinian Authority and Israel, there are Palestinians living in caves. People also inhabited caves there during the time of the Ottoman Empire and of the British Mandate for Palestine. In recent years some have been evicted by the Israeli government and settlers.[5]

In her book Home Life in Colonial Days, Alice Morse Earle wrote of some of the first European settlers in New England, New York, and Pennsylvania living in cave dwellings, also known as "smoaky homes":

In Pennsylvania caves were used by newcomers as homes for a long time, certainly half a century. They generally were formed by digging into the ground about four feet in depth on the banks or low cliffs near the river front. The walls were then built up of sods or earth laid on poles or brush; thus half only of the chamber was really under ground. If dug into a side hill, the earth formed at least two walls. The roofs were layers of tree limbs covered over with sod, or bark, or rushes and bark. The chimneys were laid of cobblestone or sticks of wood mortared with clay and grass. The settlers were thankful even for these poor shelters, and declared that they found them comfortable. By 1685 many families were still living in caves in Pennsylvania, for the Governor's Council then ordered the caves to be destroyed and filled in.[6]

In the 1970s, several members of the Tasaday apparently inhabited caves near Cotabato, in the Philippines.

Caves at Sacromonte, near Granada, Spain, are home to about 3,000 Gitano people, whose dwellings range from single rooms to caves of nearly 200 rooms, along with churches, schools, and stores in the caves.

Some families have built modern homes in caves, and renovated old ones, as in Missouri;[7] Matera, Italy;[8][9] and Spain.[10]

At least 30,000,000 people in China live in cave homes, called yaodongs; because they are warm in the winter and cool in the summer, some people find caves more desirable than concrete homes in the city.[11]

In the Australian desert mining towns of Coober Pedy and Lightning Ridge, many families have carved homes into the underground opal mines, to escape the heat.

In the Loire Valley, abandoned caves are being privately renovated as affordable housing.[12]

In England, the rock houses at Kinver Edge were inhabited until the middle of the 20th century.[13]

In Greece, some Christian hermits and saints are known by the epithet "cave dweller" (Greek: Σπηλαιώτης, romanizedSpileótis) since they lived in cave dwellings; examples include Joseph the Cave Dweller (also known as Joseph the Hesychast) and Arsenios the Cave Dweller.[14]

In 2021-2023 Beatriz Flamini spent 500 days alone in a cave in Spain in an experiment on the effects of social isolation.[15][16]

See also

References


  • Wadley, Lyn; Esteban, Irene; de la Peña1, Paloma; Wojcieszak1, Marine (2020). "Fire and grass-bedding construction 200 thousand years ago at Border Cave, South Africa" (PDF). Science. 369 (6505): 863–866. Bibcode:2020Sci...369..863W. doi:10.1126/science.abc7239. PMID 32792402. S2CID 221113832.

  • Butzer, Karl W. (1983). "Cave dwellers". World Book Encyclopedia. Vol. 3. Chicago: World Book, Inc. p. 245.

  • Wilford, John Noble (13 October 2011). "In African Cave, Signs of an Ancient Paint Factory". The New York Times. Retrieved 3 June 2020.

  • Chisholm, Hugh, ed. (1911). "Troglodytes" . Encyclopædia Britannica. Vol. 27 (11th ed.). Cambridge University Press. pp. 298–299.

  • Cave dwellers defy Israeli eviction bid, September 24, 2004 (The Guardian website)

  • Earle, Alice Morse, ' 'Home Life in Colonial Days' ', Ch. 1, pp.2-3.

  • "Really Extreme Makeover". New York Times. n.d. Retrieved 3 June 2020.

  • Guiffrida, Angela (18 June 2017). "The miracle of Matera: from city of poverty and squalor to hip hub for cave-dwellers". The Guardian. Retrieved 3 June 2020.

  • Perrottet, Tony (February 2014). "How Matera Went From Ancient Civilization to Slum to a Hidden Gem". Smithsonian. Retrieved 3 June 2020.

  • Lewine, Edward (2 October 2008). "Cave Living? Cool!". New York Times. Retrieved 3 June 2020.

  • Demick, Barbara (18 March 2012). "In China, millions make themselves at home in caves". Los Angeles Times. Retrieved 3 June 2020.

  • Malone, Luke (22 July 2014). "This Converted Cave in France Cost $1.35". Vocativ. Retrieved 3 June 2020.

  • "Restored Kinver Rock House opens". BBC. 2 March 2012. Retrieved 3 June 2020.

  • Monk Joseph Dionysaitis. Elder Arsenios the Cave-dweller (1886–1983): Fellow Ascetic of Elder Joseph the Hesychast. Transl. Angela Georgiou. 2005.

  • "Beatriz Flamini: Athlete emerges after 500 days living in cave". BBC News. 14 April 2023. Retrieved 14 April 2023.

    1. Rodriguez, Elena (14 April 2023). "Spanish athlete emerges into daylight after 500 days in cave". Reuters.

    External links



    https://en.wikipedia.org/wiki/Cave_dweller

    From Wikipedia, the free encyclopedia
    Valentine Cave, a lava tube in Lava Beds National Monument, California shows the classic tube shape; the grooves on the wall mark former flow levels.
    Thurston Lava Tube in Hawaii Volcanoes National Park, Hawaii. The step mark, more visible on the right wall, indicates the depth at which the lava flowed for a period of time.
    Rare characteristics of lava tubes are lava pillars. This is the Manjanggul lava pillar located in the Manjanggul lava tubes, on the island of Jeju-do, Korea.
    Lavacicles on the ceiling of Mushpot Cave in Lava Beds National Monument
    Close-up of a skylight on a coastal plain, with lava stalactites forming on the roof of the tube, Hawaii Volcanoes National Park
    Entrance of a lava tube, Big island, Hawaii

    A lava tube, or pyroduct,[1] 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.[2]

    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 eruption point.

    Farther away from the eruption point, lava can flow in an unchanneled, fan-like manner as it leaves its source, which is usually another lava tube leading back to the eruption point. Called pāhoehoe flows, these areas of surface-moving lava cool, forming either a smooth or rough, ropy surface. The lava continues to flow this way until it begins to block its source. At this point, the subsurface lava is still hot enough to break out at a point, and from this point the lava begins as a new "source". Lava flows from the previous source to this breakout point as the surrounding lava of the pāhoehoe flow cools. This forms an underground channel that becomes a lava tube.[3]

    Characteristics

    A broad lava-flow field often consists of a main lava tube and a series of smaller tubes that supply lava to the front of one or more separate flows. When the supply of lava stops at the end of an eruption or lava is diverted elsewhere, lava in the tube system drains downslope and leaves partially empty caves.

    Such drained tubes commonly exhibit step marks on their walls that mark the various depths at which the lava flowed, known as flow ledges or flow lines depending on how prominently they protrude from the walls. Lava tubes generally have pāhoehoe floors, although this may often be covered in breakdown from the ceiling. A variety of speleothems may be found in lava tubes[4] including a variety of stalactite forms generally known as lavacicles, which can be of the splash, "shark tooth", or tubular varieties. Lavacicles are the most common of lava tube speleothems. Drip stalagmites may form under tubular lava stalactites, and the latter may grade into a form known as a tubular lava helictite. A runner is a bead of lava that is extruded from a small opening and then runs down a wall. Lava tubes may also contain mineral deposits that most commonly take the form of crusts or small crystals, and less commonly, as stalactites and stalagmites. Some stalagmites may contain a central conduit and are interpreted as hornitos extruded from the tube floor.[5]

    Lava tubes can be up to 14–15 metres (46–49 ft) wide, though are often narrower, and run anywhere from 1–15 metres (3 ft 3 in – 49 ft 3 in) below the surface. Lava tubes can also be extremely long; one tube from the Mauna Loa 1859 flow enters the ocean about 50 kilometers (31 mi) from its eruption point, and the Cueva del Viento–Sobrado system on Teide, Tenerife island, is over 18 kilometers (11 mi) long, due to extensive braided maze areas at the upper zones of the system.

    A lava tube system in Kiama, Australia, consists of over 20 tubes, many of which are breakouts of a main lava tube. The largest of these lava tubes is 2 meters (6.6 ft) in diameter and has columnar jointing due to the large cooling surface. Other tubes have concentric and radial jointing features. The tubes are infilled due to the low slope angle of emplacement.

    Extraterrestrial lava tubes

    Lunar lava tubes have been discovered[6] and have been studied as possible human habitats, providing natural shielding from radiation.[7]

    Martian lava tubes are associated with innumerable lava flows and lava channels on the flanks of Olympus Mons. Partially collapsed lava tubes are visible as chains of pit craters, and broad lava fans formed by lava emerging from intact, subsurface tubes are also common.[8]

    Caves, including lava tubes, are considered candidate biotopes of interest for extraterrestrial life.[9]

    Notable examples

    See also

    • Caving – Recreational pastime of exploring cave systems
    • Geology of the Moon – Structure and composition of the Moon
    • Lava cave – Cave formed in volcanic rock, especially one formed via volcanic processes
    • Mars habitat – Facility where humans could live on Mars
    • Speleology – Science of cave and karst systems
    • Speleothem – Structure formed in a cave by the deposition of minerals from water

    Notes


  • "Hawaiʻi Volcanoes National Park – Lava Tubes". National Park Service. 28 April 2020. Retrieved 21 July 2020.

  • "Lava Tube". United States Geological Survey Photo glossary of volcano terms. 2000. Archived from the original on 2007-07-14. Retrieved 2007-08-07.

  • The Virtual Lava Tube Archived 2004-07-26 at the Wayback Machine goodearthgraphics.com, Large educational site on lava tube features and how they form, with many photos, Retrieved 2018-06-19

  • Bunnell, D. (2008). Caves of Fire:Inside America's Lava Tubes. National Speleological Society, Huntsville, AL. ISBN 978-1-879961-31-9.

  • Polyak, Victor J.; Provencio, Paula P. (2020). "The 'hornito-style' lava stalagmites and lava column in Lava Column Cave, El Malpais National Monument" (PDF). New Mexico Geological Society Special Publication. 14: 37–40. Retrieved 24 October 2020.

  • Handwerk, Brian (October 26, 2009), First Moon 'Skylight' Found -- Could House Lunar Base?, National Geographic, archived from the original on 2011-10-10, retrieved 2011-01-27

  • "Lunar Lava Tubes Radiation Safety Analysis". Division for Planetary Sciences 2001 meeting. American Astronomical Society. November 2001. Archived from the original on 2002-09-23. Retrieved 2007-08-07.

  • Richardson, J.W. et al. (2009). The Relationship Between Lava Fans and Tubes on Olympus Mons in the Tharsis Region, Mars. Archived 2012-10-28 at the Wayback Machine 40th Lunar and Planetary Science Conference, Abstract #1527, Retrieved 2018-06-19

  • Idota, Tetsuya; Biagioni, Edoardo; Binsted, Kim (December 2018). "Swarm Exploration of Extraterrestrial Lava Tubes with Ad-Hoc Communications". 2018 6th IEEE International Conference on Wireless for Space and Extreme Environments (WiSEE): 163–168. doi:10.1109/WiSEE.2018.8637325. ISBN 9781538642443. S2CID 61811871.

  • "Surtshellir-Stefánshellir System". Caves of Iceland. Showcaves. Archived from the original on 2012-04-24. Retrieved 2007-08-07.

  • Forti; Galli; Rossi (July 2004). "Minerogenesis of Volcanic Caves of Kenya". International Journal of Speleology. 32 (1/4): 3–18. doi:10.5038/1827-806X.32.1.1. Archived from the original on 2017-04-09. Retrieved 7 Apr 2017.

  • Barclay, Jennifer (2012-04-27). "10 Reasons Travelers Can't Keep Away from Jeju Island". CNN Travel. Archived from the original on 2015-12-24. Retrieved 2015-12-23.

  • Gulden, Bob (2011-06-21), World's Longest Lava Tubes, retrieved 2011-06-26

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