CAVE VISIT


SALLE ROBERT DE JOLY  

Through a man-made tunnel with 220 steps, we come to the 1st chamber, situated at a depth of 55 metres. A faint light from the natural entrance greets us. This is a pothole or aven in French. The pile of debris, immediately visible, was formed by the collapse of the natural entrance as well as stones and soil that has fallen in due to the natural attrition of wind and rain. Remains of animals that have either fallen in or been thrown there in more recent times have also been found.
To dig through this pile is to dig into time itself, with domestic animals on top and remains of long vanished species further down. Reindeer and bison lived in this region during the last ice age that ended more than 12,000 years ago. You can find out more about them and the men who hunted them at the Regional Museum of Prehistory.

It is through this hole that the first explorers entered. They were led by Robert de Joly and descended on 19th August 1935. The pothole was of course well known to local people but, due to its great depth, it had never been explored.

The first great chamber is 125 metres long and 90 metres wide, a little more than one hectare in area (2.5 acres). The numerous crystallisations of stalagmites and stalactites display a vast range of shapes, some of which are extremely delicate.
About 6 million years ago, the lowest level of the caves was formed by an underground river, now long gone. During the last step of the visit, you will be able to admire this remarkable gallery.
Limestone is slightly soluble in water and little by little, rainwater, in combination with carbon dioxide that naturally occurs in the soil, filters through to become slightly acidic and corrosive. This corrosive water then eats away at the small fissures it passes through, enlarging and distorting them.
The shape of the stalagmites often gives rise to their name: "piles of plates" for example. These particular shapes are found only in caves with high roofs. Drops fall from the roof and spread out in micro-droplets when contact is made with the floor. Drops falling from a lower height have less speed on impact and form different shapes: fine "candles" result.


In this part of the cave beside the "piles of plates", the "palm trees" have grown. They can be as tall as 15 metres. There is the 11-metre "pine cone", the symbol of Orgnac. Similar to the "piles of plates", the "palm trees" only exist where cave roofs are high but where water drops regularly and more abundantly. The many splash-outs of micro droplets from numerous drops cause a build up of "petals" on the sides of these extraordinary stalagmites.

To the left, several metres in front of the cave wall, a curtain of stalactites has joined the stalagmites below to form the "organ pipes". In the centre is the funeral urn of the discoverer of these caves, Robert de Joly, whose last wish, a short time before his death in 1968, was that his remains should be placed in the caves.

SALLE DU CHAOS  

After the retreat of water to lower levels, the roof began to collapse. Huge blocks of stone fell to the bottom of the gallery to form what is now the floor of the first chambers. The roof of the cave became closer to the surface of the earth. These blocks crashed down through a funnel-shaped passage into the deepest parts of the caves - see below.

Despite its troubled history, the caves are, today a true example of stability. Stalagmites growing on fallen blocks are about 15,000 years old. No man-made structure of this age exists.

If calcite-laden, water droplets remain in contact with the cave roof for long enough, a deposit is formed and gradually builds up into stalactites. If the droplets flow down an inclined wall, lines of calcite are deposited and build up to form curtains. Some are thin and translucent. The range of brown and ochre tints is due to iron oxides and organic materials carried by the water as it filters through the limestone bedrock.

SALLE ROUGE  

The last step of the visit is 120 metres underground where you can see the original gallery that was cut out 6 million years ago by the flow of water. The corrosive effects of the water are clearly visible on the walls and amply illustrate the antiquity of the caves. The huge pillars were formed after the flow of water retreated to a lower level.

A sound and light show ends your underground trip and lifts will bring you to the surface again.

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