This article needs additional citations for verification .(October 2014) |
Location | foothills of the Swartberg, near Oudtshoorn |
---|---|
Region | South Africa |
Coordinates | 33°23′34″S22°12′53″E / 33.39278°S 22.21472°E |
History | |
Material | Precambrian limestone |
Site notes | |
Excavation dates | 1930 |
Archaeologists | A.J.H. Goodwin |
The Cango Caves are located in Precambrian limestones at the foothills of the Swartberg range near the town of Oudtshoorn, in the Western Cape Province of South Africa. The principal cave is one of the country's finest, best known, and most popular tourist caves and attracts many visitors from overseas. Although the extensive system of tunnels and chambers go on for over 4 km (2+1⁄2 mi), only about a quarter of this is open to visitors, who may proceed into the cave only in groups supervised by a guide.
Cave paintings and artifacts indicate that the caves were in use throughout prehistory over a long period during the Middle and Later Stone Ages. [1] [2]
The caves were rediscovered in modern times in 1780 by a local farmer named Jacobus Van Zyl. [3] The chamber he first was lowered down into was found to be as long as a football field, and is named Van Zyl Hall in his honor. Further exploration was done and a second chamber discovered in 1792. The caves soon became a popular place to visit. [4]
In 1829 Dr Andrew Smith visited the Cango Caves, which contained much to tempt his scientific curiosity. [5]
A.J.H. Goodwin, an archaeologist at the University of Cape Town, carried out a test excavation in the Cango Caves in 1930 which found stone artefacts and other cultural material. [2]
The Cango Caves Ordinance of 1971 gave certain legal powers over the caves to what was then the Administrator of the Cape; legally, these same powers now devolve to the local government members of the executive. However, day-to-day management of the caves is the responsibility of the municipality of Oudtshoorn. [6]
Mr. Johnny van Wassenaer, the cave’s first official guide [7] is purported to have walked 29 hours to find the end of the caves in 1898. When there, he is said to have calculated that he was 25 km (15+1⁄2 mi) from the entrance, and 275 m (902 ft) underground; his route apparently followed an underground river. So far, explorers are finding more and more caves to support this story. [8]
The first rough survey was done in 1897, mapping out the first 26 chambers. [7] In 1956 the South African Spelaeological Association was tasked to draw up an accurate mapping of the Cango Caves, and look for alternative entrances.
Their results indicated that the caves were 775 m (2,543 ft) long in a single line, and that they never rise nor fell more than 16 m (52 ft). These were called Cango I. The nearest point to the surface in the caves is at the top of the shaft in the Devil's Kitchen, 52.6 m (173 ft) from the floor.
In 1972 James Craig-Smith, Luther Terblanche and Dart Ruiters widened an obstructed passage to discover Cango II. It stretches 270 m (890 ft) beyond the end of the Devil’s Kitchen. At the end of Cango II there is a shaft that descends 20 m (66 ft) to a chamber filled with water. This water flowed in the direction of Cango I.
In August 1975, during a symposium on cave biology, an exploration team led by Hans Oosthuizen, Luther Terblanche, Michale Schultz, Digby Ellis, Jean Paul Matisse, Bob Mann, Florus Koper and Peter Breedt drained the chamber of most of its water and crawled through what was previously an underwater passage. This led to the discovery of more caves, called Cango III. Altogether these caves are about 1,000 m (3,300 ft) long. The biggest of the chambers, stretches about 300 m (980 ft).
Digby Ellis and Dave Land added 290 m (950 ft) to Cango III when they discovered a crawlway in December 1977. A further 90 m (300 ft) was added in June 1978. All these extensions were surveyed in August 1978 by Dave Land, Charles Maxwell, Brian Russell and Dave Crombie. [8]
Tours are conducted at regular intervals on most days—there is a "Standard Tour" which takes an hour and an "Adventure Tour" which takes an hour and a half. The "Adventure Tour" consists of crawling through narrow passages and climbing up steep rock formations guided by small lights. The caves contain halls and limestone formations (on both tours) as well as small passages on the Adventure Tour. The smallest passage that tourists will have to pass through on the Adventure Tour is just under 15 cm to exit. Visiting the caves are considered to be part of exploring the scenic Route 62.
The Cinema Museum in London holds film of a visit to the caves in the 1930s. [9]
Oudtshoorn is a town in the Western Cape province of South Africa, located between the Swartberg mountains to the north and the Outeniqua Mountains to the south. Dubbed the "ostrich capital of the world", Oudtshoorn is known for its ostrich-feather booms, during 1865–1870 and 1900–1914. With approximately 60,000 inhabitants, it is the largest town in the Klein Karoo region. The town's economy is primarily reliant on the ostrich farming and tourism industries. Oudtshoorn is home to the world's largest ostrich population, with a number of specialised ostrich breeding farms, such as the Safari Show Farm and the Highgate Ostrich Show Farm, as stated by Pierre D. Toit.
The Swartberg mountains are a mountain range in the Western Cape province of South Africa. It is composed of two main mountain chains running roughly east–west along the northern edge of the semi-arid Little Karoo. To the north of the range lies the other large semi-arid area in South Africa, the Great Karoo. Most of the Swartberg Mountains are above 2000 m high, making them the tallest mountains in the Western Cape. It is also one of the longest, spanning some 230 km from south of Laingsburg in the west to between Willowmore and Uniondale in the east. Geologically, these mountains are part of the Cape Fold Belt.
The R328 is a Regional Route in Western Cape, South Africa that connects Mossel Bay in the south to Prince Albert in the north via Oudtshoorn.
Sof Omar Caves is the longest cave in Ethiopia at 15.1 kilometres (9.4 mi) long. When surveyed in 1972, it was the longest cave in Africa. Since then explorations in Madagascar and Algeria have overtaken it. It is situated to the east of Ginnir, in the East Bale Zone of the Oromia Region in southeastern Ethiopia, through which the Weyib River flows. It sinks at the Ayiew Maco entrance and reappears at the Holuca resurgence 1 kilometre (0.62 mi) away. According to tradition Sof Omar was the name of a Muslim holy man who lived in the area and Ayiew the name of his daughter. Maco and Holuca are local names for 'name' and "cave", respectively. Long a religious centre, it is sacred both to Islam and the local Oromo traditional religion. The caves are known for their many pillars, particularly in the "Chamber of Columns". As of 2011, the site was added on UNESCO tentative list, still to be considered for a possible inscription.
Lamb Leer is a 14.59 hectare geological Site of Special Scientific Interest between East Harptree and Priddy in the Mendip Hills, Somerset, notified in 1983. The cavern is a fragment of a very ancient major cave system which now contains one of the largest chambers in the Mendip Hills.
The Bothongo WonderCave in Kromdraai, Gauteng, South Africa is situated within the Bothongo Rhino & Lion Nature Reserve in the Cradle of Humankind, a UNESCO World Heritage Site. The cave is the third-largest cave chamber in the country. It is 5-10 million years old. The single chamber has an area of 46,000 square metres (500,000 sq ft), and is 125 by 154 metres.
Koněprusy Caves, also Zlatý kůň, is a cave system in the heart of the limestone region known as Bohemian Karst in the Central Bohemian Region of the Czech Republic. It is located in the municipality of Koněprusy, about 25 kilometres (16 mi) southwest of Prague, 6 km (3.7 mi) south of Beroun. With the length of 2 km (1.2 mi) and vertical range of 70 m (230 ft), it is the largest cave system in Bohemia.
Rumbling Hole is a cave on Leck Fell, in Lancashire, England. Its entrance is a 50-metre (160 ft) deep fenced shaft, and it rapidly descends a series of pitches to a low aqueous passage that has been connected to Lost Johns' Cave. It is part of the Three Counties System, an 87-kilometre (54 mi) cave system that spans the borders of Cumbria, Lancashire, and North Yorkshire.
Langcliffe Pot is a cave system on the slopes of Great Whernside in Upper Wharfedale, about 3 kilometres (1.9 mi) SSE of Kettlewell in North Yorkshire. It is part of the Black Keld Site of Special Scientific Interest where the "underground drainage system which feeds the stream resurgence at Black Keld is one of the largest and deepest in Britain, although only a small proportion of its cave passages are accessible at present." Mossdale Caverns is also part of the Black Keld SSSI. Although a considerable length of passage has been explored in Langcliffe Pot, the current end is over 170 metres (560 ft) above the resurgence, and over 4 kilometres (2.5 mi) in distance. A trip to the far end has been described as "one of the most serious undertakings in British caving".
The Caves of the Tullybrack and Belmore hills are a collection of caves in southwest County Fermanagh, Northern Ireland. The region is also described as the West Fermanagh Scarplands by environmental agencies and shares many similar karst features with the nearby Marble Arch Caves Global Geopark.
Short Drop Cave and Gavel Pot are different entrances into the same cave system on Leck Fell, in Lancashire, England. The main top entrance, Short Drop Cave, is a small hole in a fenced off shakehole near the main stream sink. Gavel Pot, a window into the system, is a large fenced shakehole some 40-metre (130 ft) deep requiring tackle to descend. There are two other smaller entrances into Short Drop Cave. At its base the system links via a sump with Lost Johns' Cave, and is part of the Three Counties System, an 87 kilometres (54 mi) cave system which spans the borders of Cumbria, Lancashire, and North Yorkshire.
Grotte de Lombrives or Lombrives Cave is a large natural cavern located in Ornolac-Ussat-les-Bains, at the eastern edge of the Pyrénées Ariégeoises Natural Regional Park, in the Ariège department of Occitanie, in southwestern France.
Death's Head Hole is a cave on Leck Fell, in Lancashire, England. Its entrance is a 64-metre (210 ft) deep shaft. It leads into Lost Johns' Cave and is part of the Three Counties System, an 87-kilometre (54 mi) cave system which spans the borders of Cumbria, Lancashire, and North Yorkshire.
Long Drop Cave is a cave on Leck Fell, in Lancashire, England. It leads into Death's Head Hole, and is part of the Three Counties System, an 87-kilometre (54 mi) cave system which spans the borders of Cumbria, Lancashire, and North Yorkshire.
Boomplaas Cave is located in the Cango Valley in the foothills of the Swartberg mountain range, north of Oudtshoorn, Eden District Municipality in the Western Cape Province, South Africa. It has a 5 m (16 ft) deep stratified archaeological sequence of human presence, occupation and hunter-gatherer/herder acculturation that might date back as far as 80,000 years. The site's documentation contributed to the reconstruction of palaeo-environments in the context of changes in climate within periods of the Late Pleistocene and the Holocene. The cave has served multiple functions during its occupation, such as a kraal (enclosure) for animals, a place for the storage of oil rich fruits and as a hunting camp. Circular stone hearths and calcified dung remains of domesticated sheep as well as stone adzes and pottery art were excavated indicating that humans lived at the site and kept animals.
The Kogelbeen Cave forms part of eight caves on the dolomitic Ghaap Plateau of the Northern Cape, South Africa. It is commonly known as Kogelbeengrotte in Afrikaans. The cave is located on Kogelbeen Farm in Pixley ka Seme District Municipality. It is the longest known cave in the Northern Cape with a length of 788 meters. The Kogelbeen Cave has a diverse fauna with over 39 species living in five life zones within the cave.
Swinsto Cave is a limestone cave in West Kingsdale, North Yorkshire, England. It leads into Kingsdale Master Cave and it is popular with cavers as it is possible to descend by abseiling down the pitches, retrieving the rope each time, and exiting through Valley Entrance of Kingsdale Master Cave at the base of the hill. It is part of a 27-kilometre (17 mi) long cave system that drains both flanks of Kingsdale.
Ockert Stefanus "Okkie" Terblanche is a South African retired politician and retired police general who served as the Shadow Deputy Minister of Police and as a Member of the National Assembly from 2019 until retiring from politics in 2024. He represented the Western Cape in the National Council of Provinces (NCOP) from October 2015 to May 2019. Terblanche is a member of the Democratic Alliance (DA).
Jingling Pot is a limestone cave in West Kingsdale, North Yorkshire, England. Located adjacent to Jingling Beck, it is a lenticular-shaped 45-metre (148 ft) deep shaft that descends straight from the surface. At the bottom the rift extends to the north and descends steeply into a further chamber, at the end of which the initials of the original explorers may be seen scratched into the rock. A narrow shaft in this second chamber drops into a complex of small crawls and rifts, which approach close to a passage in the One-armed Bandit Series of Aquamole Pot. A second set of shafts descend parallel to the surface shaft. These can be entered through a rock window a little way below the entrance.
The Long Kin East Cave - Rift Pot system is a limestone cave system on the southern flanks of Ingleborough, North Yorkshire in England lying within the designated Ingleborough Site of Special Scientific Interest. Long Kin East Cave starts as a long meandering stream passage but then plummets down a 58-metre (190 ft) deep shaft when it meets a shattered fault into which Rift Pot also descends. At the bottom, the stream flows through some low canals and sumps, to eventually emerge at Austwick Beck Head in Crummackdale.
{{cite web}}
: CS1 maint: numeric names: authors list (link)