Caves of Nerja
Encyclopedia
The Caves of Nerja are a series of caverns close to the town of Nerja
Nerja
Nerja is a municipality on the Costa del Sol in the province of Málaga, Andalusia, southern Spain. It is on the country's southern Mediterranean coast, about 50 km east of Málaga.-History:...

 in Andalusia
Andalusia
Andalusia is the most populous and the second largest in area of the autonomous communities of Spain. The Andalusian autonomous community is officially recognised as a nationality of Spain. The territory is divided into eight provinces: Huelva, Seville, Cádiz, Córdoba, Málaga, Jaén, Granada and...

. Stretching for almost 5 km the caverns are one of Spain's major tourist attractions. Concerts are regularly held in one of the chambers which forms a natural amphitheatre
Amphitheatre
An amphitheatre is an open-air venue used for entertainment and performances.There are two similar, but distinct, types of structure for which the word "amphitheatre" is used: Ancient Roman amphitheatres were large central performance spaces surrounded by ascending seating, and were commonly used...

.

The caves were re-discovered in modern times on 12 January 1959 by five friends, who entered through a narrow sink hole, known as "La Mina". This forms one of the two natural entrances to the cave system. A third entrance was created in 1960 to allow easy access for tourists. The cave is divided into two main parts known as Nerja I and Nerja II. Nerja I includes the Show Galleries which are open to the public, with relatively easy access via a flight of stairs and concreted pathways to allow tourists to move about in the cavern without difficulty. Nerja II, which is not open to the public comprises the Upper Gallery discovered in 1960 and the New Gallery discovered in 1969.

History

Approximately 5 million years ago, during the Upper Miocene
Miocene
The Miocene is a geological epoch of the Neogene Period and extends from about . The Miocene was named by Sir Charles Lyell. Its name comes from the Greek words and and means "less recent" because it has 18% fewer modern sea invertebrates than the Pliocene. The Miocene follows the Oligocene...

, water penetrated the fissures of the marble rock and dissolved it, forming a huge subterranean cavern. Seismic movement and landslides during the Holocene
Holocene
The Holocene is a geological epoch which began at the end of the Pleistocene and continues to the present. The Holocene is part of the Quaternary period. Its name comes from the Greek words and , meaning "entirely recent"...

 forced the water to find new pathways through the cave system and began the formation of the giant stalactite
Stalactite
A stalactite , "to drip", and meaning "that which drips") is a type of speleothem that hangs from the ceiling of limestone caves. It is a type of dripstone...

s and stalagmite
Stalagmite
A stalagmite is a type of speleothem that rises from the floor of a limestone cave due to the dripping of mineralized solutions and the deposition of calcium carbonate. This stalagmite formation occurs only under certain pH conditions within the underground cavern. The corresponding formation on...

s that can be seen in the cave.

Skeletal remains found in the caverns indicate that they were inhabited from about 25,000 BC up until the Bronze Age
Bronze Age
The Bronze Age is a period characterized by the use of copper and its alloy bronze as the chief hard materials in the manufacture of some implements and weapons. Chronologically, it stands between the Stone Age and Iron Age...

. Cave paintings from the Paleolithic
Paleolithic
The Paleolithic Age, Era or Period, is a prehistoric period of human history distinguished by the development of the most primitive stone tools discovered , and covers roughly 99% of human technological prehistory...

 and post-Paleolithic eras have been discovered on the walls of the cave. For about 4,000 years from 25,000 BC the caves were used seasonally by a small group of humans, and were occupied by cave hyena
Cave Hyena
The Cave Hyena is an extinct subspecies of spotted hyena native to Eurasia, ranging from Northern China to Spain and into the British Isles...

 during the periods that the humans were absent. By 21,000 BC the human population had taken up year round residence in the caves and had increased in number. A culture based on hunting in the local area had evolved, illustrated by first cave paintings found in the cave which date to around the time. Pine nuts and snails were also important elements of the diet. Up until around 10,800 BC the hunting culture continued to develop with more prey species being taken, including goats, rabbits, fish and marine mammals. A wide variety of animal bones, shells and fish bones from this time have been found in the cave, including the remains of a number of offshore species, along with stone and bone tools. By 4500 BC domesticated animals were being kept and the area around the cave was being used for farming and the production of pottery. By 3800 BC textiles and more advanced styles of pottery were being produced and parts of the cave were being used as a burial chamber.


Galleries

Show Gallery

Each of the galleries has a number of halls, areas where the walls, floors or ceilings close in to subdivide the main caverns. The Show Gallery is accessed by a 8 m flight of stairs leading to the Entrance Hall () where archaeological excavations took place and where some of the finds are now displayed. Off to one side a passage leads the Mine Hall (), and Hall of the Sink () where further archaeological excavations take place. This area is not normally open to the public. Back through the Entrance Hall is the Hall of the Nativity () which is filled with columns of calcite. A skeleton recovered from the cave is on display in a glass case in this subsection. From the Entrance Hall a passage called the Hall of the Tusk () leads down to the Hall of the Waterfall or Ballet (). It is here that concerts and festivals of dance are staged and there are about 100 seats set permanently in the cave. This large cavern has little to separate it from the Hall of the Phantoms () apart from some columns. The Hall of the Phantoms is named after an unusual speleothem
Speleothem
A speleothem , commonly known as a cave formation, is a secondary mineral deposit formed in a cave. Speleothems are typically formed in limestone or dolostone solutional caves.-Origin and composition:...

. At the end of this cavern is a large rockfall which separates it from the Hall of the Cataclysm () which is over 100 m long and dominated by the huge central column which is the biggest in the world, measuring 13 m by 7 m at the base and standing 32 m high. Further down into the hall is the Organ Corner () where fluted columns can be struck to produce different notes. Some of the columns seem to have been intentionally altered to produce different notes by the prehistoric inhabitants of the cave. High up in the far corner of this cave is the opening which allows access to the Upper and New Galleries.

Upper and New Galleries

The Upper and New Galleries are each divided into two halls. In the Upper Hall are the Columns of Hercules () and the Hall of Immensity (), while in the New Gallery there are the Hall of the Lance () and the Hall of the Mountain (). These two areas contain many of the cave paintings, but tourist access is restricted to specialised caving "speleothem tourism".
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