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Haitón del Guarataro

solutional cave·Venezuela·limestone

The Haitón del Guarataro is a significant solutional cave system located in Venezuela's Falcón State, notable for being the deepest limestone cave in the country. Discovered and first surveyed in 1973, it serves as a tourist attraction within the Juan Crisóstomo Falcón National Park and is formed in Oligocene reefal limestone.

Key Facts

  • It is the deepest limestone cave in Venezuela.
  • The entrance is a tourist attraction within Juan Crisóstomo Falcón National Park.
  • The cave has a total depth of 305 meters.
  • Its total passage length is 640 meters.
  • It was first explored and surveyed in April 1973 by the Venezuela '73 British Karst Research Expedition.
  • It is formed in Oligocene reefal limestone.
Haitón del Guarataro
Location Detail
Sierra de San Luis, Falcón State, 2.5 kilometers south-east of Curimagua, within Juan Crisóstomo Falcón National Park
Depth Meters
305
Width Meters
12
Known For Features

Deepest Limestone Cave In Venezuela, Large Entrance Shaft

Formation Period
Explored in 1973
Geological Age
Oligocene
Associated Wildlife

Cave Crickets, Phalangodid Harvestmen, Hyalella Meinerti, Troglobitic Trichopolydesmid Millipede

Access Difficulty
moderate
Year Of Discovery
1973

About Haitón del Guarataro

The Haitón del Guarataro is a significant solutional cave system located in the Sierra de San Luis, within Venezuela's Falcón State. It holds the distinction of being the deepest limestone cave in Venezuela, a geological feature that draws interest from both speleologists and tourists.

Geological Significance and Formation

This extensive cave system was formed through dissolution processes in Oligocene reefal limestone. The cave's entrance is a large shaft, approximately 12 meters in diameter, which descends through a series of drops totaling over 200 meters. The main passages extend for considerable distances, with a total surveyed length of 640 meters and a depth of 305 meters.

Exploration and Tourism

The Haitón del Guarataro was first thoroughly explored and surveyed in April 1973 by members of the Venezuela '73 British Karst Research Expedition. Today, its entrance serves as a tourist attraction within the Juan Crisóstomo Falcón National Park, offering visitors a glimpse into the subterranean world of Venezuela.

Flora and Fauna

Faunal surveys conducted during the cave's exploration revealed a limited number of cave-dwelling organisms. These included common cave inhabitants such as cave crickets and harvestmen, alongside more specialized species like a depigmented troglophile shrimp (Hyalella meinerti) found in a large pool, and a troglobitic millipede discovered on the roof of the cave's terminal chamber.

Source: Wikipedia ↗

Frequently Asked Questions

What is the Haitón del Guarataro?

The Haitón del Guarataro is a solutional cave system located in the Sierra de San Luis, Falcón State, Venezuela. It is recognized as the deepest limestone cave in Venezuela and is a popular tourist attraction.

Where is the Haitón del Guarataro located?

The Haitón del Guarataro is situated in the Sierra de San Luis in Falcón State, Venezuela, approximately 2.5 kilometers south-east of Curimagua. It is part of the Juan Crisóstomo Falcón National Park.

How deep is the Haitón del Guarataro?

The Haitón del Guarataro has a measured depth of 305 meters. The entrance shaft alone is 12 meters in diameter, leading to further drops within the cave system.

When was the Haitón del Guarataro discovered or first explored?

The cave was first explored and surveyed in April 1973 by members of the Venezuela '73 British Karst Research Expedition.

What kind of rock is the Haitón del Guarataro formed in?

The Haitón del Guarataro is formed in Oligocene reefal limestone. This type of geological formation is characteristic of solutional caves.

What wildlife has been found in the Haitón del Guarataro?

A faunal survey recorded a few cave-dwelling species, including cave crickets, harvestmen, a depigmented troglophile shrimp (Hyalella meinerti) found in a pool, and a troglobitic millipede discovered on the ceiling of the terminal chamber.