38 



INCOMPATIBILITY OF THE ASSOCIATED 



hills are 132 and 436 feet high, at Antibes, 250 feet, 

 and at Cette the hill, which resembles on a small 

 scale the Rock of Gibraltar, rises 355 feet above the 

 sea level. Still more formidable are the hills inland. 

 Mont Pdd^mar (Gard) rises to a height of 1,128 feet, 

 whilst Santenay is not less than 1,640 feet high. The 

 relation of these hills to the surrounding plains, and 

 of the Fissure to certain bone caves is shown in Fig. 

 No. 4. 



FIG. 4. Diagram Section showing the position of some of the Ossiferous 

 Fissures on high isolated hills. 



Various Calcareous Rocks 



Amongst the animal remains found in the several 

 Ossiferous Fissures are those of : 



5 Carnivores - 



Cave lion. 

 Lynx. 



Wolf. 



4 Ungulates 



^Mammoth. 

 I Rhinoceros. 



2 Rodents 



Spotted Hyaena. 

 .Bear. 

 rLagomys. 

 \Hare. 



CHorse. 



px. 



3 Ruminants/ Deer. 



^Antelopes. 



Together with land shells of various living species. 

 The breccia, which is composed of sharp angular 

 fragments of the local rocks, imbedded in a matrix of 

 red clay or loam, is generally cemented by calcite. 

 The bones are mostly broken and splintered into 

 innumerable sharp fragments, and according to M. 



