The Gran Caverna de Santo Tomàs is considered the longest cavern
systems in Cuba, measuring about 46.25 kilometres in length.
Karst is a topography formed from the dissolution of soluble
carbonate rocks such as limestone and dolomite. The lowest part
of this cave system is still active and the stream, called
Arroyo Santo Tomàs, flows through it. Gran Caverna de Santo
Tomás takes its name from the Santo Tomás river, which forms
most of the huge gorges.
Due to the great variety of karst formations, both on the
surface and in the cave, and due to important archaeological
discoveries, the Gran Caverna de Santo Tomàs has been visited by
a significant number of tourists and scientists in the last 20
years, despite the problems due to its distance from the main
tourist routes around the island.
The entrance of the cave is about 150 meters high from the
ground. The cavern system is formed on 7 levels. You will visit
the cave in the sixth level, in other words the level above the
lowest level. While the lowest level whic is 113 m high from the
sea level, is filled completely by water of the Arroyo Santo
Tomàs, the sixth level is normally dry. Only during events of
floods, the water rises and partly floods the sixth level. It is
also the second-youngest level. The upper levels are older and
show more signs of destruction, like collapsed ceilings. The
uppermost level is at 202 m high from the sea level, so that the
cave has a vertical range of about 89 m (the height difference
between the highest and lowest points in the cave).
The cavern system was originally named Caverna del Moncada when
it was discovered, wheras the cave at the entrance named Cueva
de las Avispar (Wasp Cave). It was later named Cueva de Santa
Tomàs. The reason why the name Gran Caverna de Santo Tomás has
remained is because a joke of a caver, referring to the size of
the cave system, was written in brochures by those promoting the
territory.