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The Aragua...
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The Aragua valleys form a basin, closed between granitic and calcareous mountain ranges of unequal height. Due to the land's peculiar configuration, the small rivers of the Aragua valleys form an enclosed system and flow into a basin blocked off on all sides; these rivers do not flow to the ocean but end in an inland lake, and thanks to constant evaporation lose themselves, so to speak, in the air. These rivers and lakes determine the fertility of the soil and agricultural produce in the valleys. The aspect of the place and the experience of some fifty years show that the water-level is not constant; that the balance between evaporation and inflow is broken. As the lake lies 1, feet above the neighboring Calabozo steppes, and 1, feet above sea-level, it was thought that the water filtered out through a subterranean channel. As islands emerge, and the water-level progressively decreases, it is feared the lake might completely dry out.

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