He has likewise observed a mass of rock, which forms the extremity of a pretty high mountain, the foot of which is washed by the sea. This rock is at a considerable height, intirely pierced by pholades, that species of marine shell-fish so well known, which digs cells into the stones. It appears from hence, that this rock was some time covered by the sea. According to Mons. Donati, the sea has insensibly retired from the parts, which were washed by it; and he thinks, that there must have been a very considerable space of time between that and the time, when this mountain, pierced by pholades, was covered by the waters of the sea. He deduces his opinion from the following fact. There is in this rock, pretty near the surface of the sea, a natural cavern fill’d with earth. In this earth have been found ancient Roman sarcophagi and lamps. It follows from hence, that even in the time of the Romans this part of the rock, in which this cavern is situated, was not under water. As there is but a small distance between the cavern and the surface of the water, it follows, that the water has sunk but very little since the time of the Romans. If it has sunk in the same proportion since the time, when it covered the top of the rock, there is no doubt, but that the time, when it was intirely covered by the sea, must have been very distant. If the same manner of reasoning be used, with respect to the bed of marine bodies, mentioned above, which crosses the mountains, that separate Provence from Piedmont, we shall be obliged to presume, that the time, when those mountains were under the waters of the sea, was at a very great distance from the present. Mons. Donati concludes from these facts, and the consequences deduced from them, that the Mediterranean sea is a very ancient, and not a modern one, as Mons. de Buffon imagines.