At The Distance Of Six Miles From The Island Of Piedra Raton We Passed, First, On The East, The Mouth

Of the Rio Sipapo, called Tipapu by the Indians; and then, on the west, the mouth of the Rio Vichada.

Near the latter are some rocks covered by the water, that form a small cascade or raudalito. The Rio Sipapo, which Father Gili went up in 1757, and which he says is twice as broad as the Tiber, comes from a considerable chain of mountains, which in its southern part bears the name of the river, and joins the group of Calitamini and of Cunavami. Next to the Peak of Duida, which rises above the mission of Esmeralda, the Cerros of Sipapo appeared to me the most lofty of the whole Cordillera of Parima. They form an immense wall of rocks, shooting up abruptly from the plain, its craggy ridge of running from south-south-east to north-north-west. I believe these crags, these indentations, which equally occur in the sandstone of Montserrat in Catalonia,* (* From them the name of Montserrat is derived, Monte Serrato signifying a mountain ridged or jagged like a saw.) are owing to blocks of granite heaped together. The Cerros de Sipapo wear a different aspect every hour of the day. At sunrise the thick vegetation with which these mountains are clothed is tinged with that dark green inclining to brown, which is peculiar to a region where trees with coriaceous leaves prevail. Broad and strong shadows are projected on the neighbouring plain, and form a contrast with the vivid light diffused over the ground, in the air, and on the surface of the waters.

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