Chiquibul Cave System

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The Chiquibul Cave System is one of the largest and best-known cave systems in Central America. It consists of four distinct caves along the course of the Chiquibul River; Actun Kabal, Actun Tun Kul (Tunkul) and Cebada Cave in Belize, and Xibalba in Guatemala, as well as several other smaller associated caves. Included within the cave system are two of the largest caverns in the world.

Cave Natural underground space large enough for a human to enter

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 also refer to much smaller openings such as sea caves, rock shelters, and grottos, though strictly speaking a cave is exogene, meaning it is deeper than its opening is wide, and a rock shelter is endogene.

Central America central geographic region of the Americas

Central America is a region found in the southern tip of North America and is sometimes defined as a subcontinent of the Americas. This region is bordered by Mexico to the north, Colombia to the southeast, the Caribbean Sea to the east and the Pacific Ocean to the west and south. Central America consists of seven countries: Belize, Costa Rica, El Salvador, Guatemala, Honduras, Nicaragua and Panama. The combined population of Central America is estimated to be between 41,739,000 and 42,688,190.

Belize country in Central America

Belize, formerly British Honduras, is a politically independent constitutional monarchy located on the north eastern coast of Central America. Belize is bordered on the northwest by Mexico, on the east by the Caribbean Sea, and on the south and west by Guatemala. It has an area of 22,970 square kilometres (8,867 sq mi) and a population of 408,487 (2019). Its mainland is about 180 mi (290 km) long and 68 mi (110 km) wide. It has the lowest population and population density in Central America. The country's population growth rate of 1.87% per year is the second highest in the region and one of the highest in the Western Hemisphere.

Contents

Entrance to Actun Kabal, part of the Chiquibul Cave System, in Belize Actun Kabal entrance.jpg
Entrance to Actun Kabal, part of the Chiquibul Cave System, in Belize

Actun Kabal (Kabal Group)

This upper section of the Chiquibul Cave System has over 12 km of mapped passages with a depth of -95 m. Included is Chiquibul Chamber, at 250 m by 150 m one of the world's largest caverns.

Actun Tun Kul

Tun Kul ("stone drum") includes Belize Chamber - with dimensions of 300 m by 150 m by 65 m, it is one of the largest natural caverns in the world. Tun Kul was connected with Cebada Cave in 1999 resulting in a 39km long cave.

Huge cave passage in Actun Kabal, part of the Chiquibul Cave System, in Belize Kabal-kotob trunk.jpg
Huge cave passage in Actun Kabal, part of the Chiquibul Cave System, in Belize

Cebada Cave

Cebada Cave and Tun Kul were linked in 1999; at 39 km it is the longest cave in Belize.

Xibalba

This downstream section of the Chiquibul Cave System is entirely within Guatemala, and at -187 m was briefly that country's deepest cave (currently Jul Mas Nim, at -294 m). Over seven kilometres of passages have been mapped, including some that are over 100 m wide. The cave entrance is 200 m across.

Exploration

Cavers Mike Boon and Tom Miller visited the area in 1971 and 1982 respectively, with Miller initiating the first cave explorations as part of his PhD work. Miller followed up with major international, interdisciplinary expeditions in 1984, 1986 and 1988, partially funded by National Geographic and the National Speleological Society. The first expedition surveyed 23 km of dry cave passages in Kabal and Tun Kul at the upstream part of the system, ending at a sump at the end of Tun Kul. The second expedition surveyed 27 km of dry and river passages in Cebada and Xibalba. The third expedition attempted but failed to connect Cebada with Tun Kul. In 1990 a comprehensive cave survey was prepared by Steve Grundy and Olivia Whitwell.

National Geographic Society American non-profit scientific and educational institution

The National Geographic Society (NGS), headquartered in Washington, D.C., United States, is one of the largest non-profit scientific and educational organizations in the world. Founded in 1888, its interests include geography, archaeology, and natural science, the promotion of environmental and historical conservation, and the study of world culture and history. The National Geographic Society's logo is a yellow portrait frame—rectangular in shape—which appears on the margins surrounding the front covers of its magazines and as its television channel logo. Through National Geographic Partners, the Society operates the magazine, TV channels, a website, worldwide events, and other media operations.

National Speleological Society Organization for exploration, conservation, and study of caves in the United States

The National Speleological Society (NSS) is an organization formed in 1941 to advance the exploration, conservation, study, and understanding of caves in the United States. Originally headquartered in Washington D.C., its current offices are in Huntsville, Alabama. The organization engages in the research and scientific study, restoration, exploration, and protection of caves. It has more than 10,000 members in more than 250 grottos.

Cave survey the three-dimensional mapping of underground caverns

A cave survey is a map of all or part of a cave system, which may be produced to meet differing standards of accuracy depending on the cave conditions and equipment available underground. Cave surveying and cartography, i.e. the creation of an accurate, detailed map, is one of the most common technical activities undertaken within a cave and is a fundamental part of speleology. Surveys can be used to compare caves to each other by length, depth and volume, may reveal clues on speleogenesis, provide a spatial reference for other areas of scientific study and assist visitors with route-finding.

Biology

Biological collections and observations were conducted in 1986 in Cebada Cave, and other collections were made in 1984 and 1988. Seventy invertebrate species are known from the system.

Protection

Despite its remoteness, the area is threatened by agricultural activities, fires, illegal logging, wildlife hunting, looting of cultural artifacts, and vandalism of both cultural and geological assets. The Chiquibul Cave System is within Chiquibul National Park, a 264,000-acre reserve in the Maya Mountains massif. In 2007 it was determined that the cave system needed special consideration, and in 2010 The Nature Conservancy presented a five-year management plan which includes provisions for controlled tourism on a very limited basis.

Illegal logging harvest, transportation, purchase, or sale of timber in violation of laws

Illegal logging is the harvest, transportation, purchase or sale of timber in violation of laws. The harvesting procedure itself may be illegal, including using corrupt means to gain access to forests; extraction without permission, or from a protected area; the cutting down of protected species; or the extraction of timber in excess of agreed limits.

Chiquibul National Park National Park in Belize

Chiquibul National Park is Belize's largest national park. It is 1,073 km2 (414 sq mi) in size. The park is located in Belize's Cayo District. The national park surrounds Caracol, a Mayan city. Caracol has been designated as an archaeological reserve and is not included within the park's total area. Chiquibul Forest Reserve is adjacent to the park.

Maya Mountains mountain range

The Maya Mountains are a mountain range located in Belize and eastern Guatemala, in Central America.

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References

Tom Miller, Chiquibul Expedition 1984 The Canadian Caver vol 16 no 2 1984

<i>The Canadian Caver</i>

The Canadian Caver is a semiannual publication that documents the activities of Canadian cavers exploring caves within Canada and overseas.

Tom Miller, Chiquibul 1986 The Canadian Caver vol 18 no 2 1986

Nick Williams et al., Journal of Cave And Karst Studies No 58(2) August 1996