Note 9 — XIX

Paranas.As the men, owing to the sultry heat, the complete calm, and almost cloudless sky, slept quite as much as they rowed, we did not reach Paranas before the afternoon. It is a clean village, situated on a declivity between twenty and a hundred and fifty feet above the sea. The sides, which stand perpendicularly in the sea, consist of grey banks of clay receding landwards, and overspread with a layer of fragments of mussels, the intervals between which are filled up with clay, and over the latter is a solid breccia, cemented with lime, composed of similar fragments. In the clay banks are well-preserved petrifactions, so similar in color, habitat, and aspect to many of those in the German tertiary formations that they might be taken for them. The breccia also is fossil, probably also tertiary; at all events, the identity of the few species which were recognisable in it—Cerithium, Pecten, and Venus—with living species could not be determined.9