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After three hours' walking we reached a small plain called La Rambleta at the far end of the malpaís; from its center rises the Piton or Sugar Loaf. From the Orotava side this mountain resembles those pyramids with steps found in Féjoun or Mexico. Here we found the air holes that locals call the Nostrils of the Peak (Narices del Pico). Hot watery vapors seep out at regular intervals from cracks in the rock, and the thermometer marked 43.2°C. I cannot, however, accept the daring hypothesis which states that the Nostrils of the Peak are vents of an immense apparatus of distillation whose lower part is situated below sea-level. Since we have been studying volcanoes with more care, and since innate love for all that is marvelous is less common in geological books, doubts have been expressed about these constant and direct links between sea water and volcanic fire. There is a far simpler explanation of this phenomenon. The peak is covered with snow part of the year; we found snow still around on the Rambleta plain. This led us to conclude that the Tenerife peak, like the Andes and Manila islands' volcanoes, are filled with filtered water. The watery vapors emitted by the Nostrils and cracks of the crater are those same waters heated. |