The Cave of the hundred mammoths, also known as Miremont cave, Cro des Cluzeau or Cro de Granville, is about south of Rouffignac on a hill slope along the right-hand side of the La Binche river, a left tributary of the Manaurie. Perched only about one kilometer farther east on the opposite side of the valley is the little village of Fleurac. The rocks of the cave are flat-lying limestones belonging to the uppermost Coniacian; they are very rich in flint nodules. These rocks together with overlying Santonian rocks form the limestone plateau of Légal, the divide between the drainage basins of the rivers Lisle and Vézère. The Rouffignac cave and the Villars Cave possess the most extensive cave system of the Périgord, with more than of underground passageways. There are 10 natural shafts that lead to a deeper level. So far, a further of passageways have been explored in this deeper level. Below the deeper level exists a bottom level with a small underground rivulet. Visitors of the cave board an electric train that takes them about into the interior. The plan of the cave reveals a fractal-like dendritic pattern that is not random but organized along certain preferred directions. Presumably the cave was formed during the Pliocene about 3 to 2 million years ago. Water had infiltrated the bedrock along certain zones of weakness and dissolved the limestone. Today this process has come to an end, and the cave is mostly dry except for the rivulet along the base level.
The artistic representations in the cave were mainly executed as engravings or black contour drawings. In contrast with the caves in Lascaux and Font-de-Gaume the representations in the Rouffignac cave are not polychrome. So far 224 animal representations and 4 human figures have been registered. The animal representations can be subdivided as follows:
Additionally there is a single cave bear. Amongst the six animal groups cited the mammoths take on a prominent role. The woolly rhinoceros are also commoner than in other similar caves, where representations are rare. Signs are somewhat underrepresented with 17 tectiform and 6 serpentiform signs being known. Fairly common are finger flutings, macaroni- or meander-like traces that take up a surface of and decorate walls and ceilings. In September 2011 Jess Cooney, a Cambridge archeologist, and Dr Leslie Van Gelder of Walden University, USA announced that their research had identified the artists who had created a large proportion of the flutings to be children as young as three years old. 63 animal representations alone are found on the ceiling of the so-called Le Grand Plafond chamber. Here again the representations are associated with a shaft.
Cave bears
The presence of cave bears in the Rouffignac cave is attested by scratch marks on the walls and also by their resting places.
Age
Because of the general lack of artifacts and occupation traces, the Rouffignac cave has not been dated directly. According to André Leroi-Gourhan the style of the representations can be attributed to his style IV and belong therefore into the Middle Magdalenian, about 13,000 years BP. Reconnaissance excavations in front of the entry of the cave found traces of human occupations dating back to the Mesolithic and to the Neolithic. Some Iron Age remains capped the deposits. Therefore, mesolithic hunters must have had their encampment in front of the cave from about 9,200 to 7,800 years BP. In the Sauveterrian level, geometrically shaped microliths were found, the so-called Rouffignac heads. The neolithic and Iron Age levels yielded remnants of burials.
Visiting the cave
The Rouffignac cave is open to the public between April 1 and November 1. The number of visitors is restricted to 550 per day.
Literature
Leroi-Gourhan, A.. Rouffignac. In: Dictionnaire de la Préhistoire, sous la dir. d'A. Leroi-Gourhan, Presses universitaires de France, Paris, pp. 959–960
