Due to the thickness of the vegetation, made up of a plant of the Musaceae family, it was hard to find a path. We had to make one through that jungle of musaceous plants; the negroes led us, cutting a path with machetes. We saw the peak at intervals through breaks in the cloud, but soon we were covered in a thick mist and could only proceed using the compass; with each step we risked finding ourselves at the edge of a precipice, which fell 6, feet down to the sea. We had to stop, surrounded by cloud down to the ground, and we began to doubt if we would reach the eastern peak before sunset. Luckily the negroes carrying the water and the food had arrived, so we decided to eat something. But the meal did not last long because either the Capuchin father had not calculated our numbers properly or the slaves had already eaten everything. We found only olives and some bread. We had been walking for nine hours without stopping or finding water. Our guides seemed to lose heart, and wanted to go back. Bonpland and I had difficulty in persuading them to stay with us.

Despite the heat the traveler feels under his feet on the brink of the crater, the cone of ashes remains covered with snow for several months. The cold, angry wind, which had been blowing since dawn, forced us to seek shelter at the foot of the Piton. Our hands and feet were frozen, while our boots were burned by the ground we walked on. In a few minutes we reached the foot of the Sugar Loaf, which we had so laboriously climbed; our speed of descent was in part involuntary as we slipped down on the ashes. We reluctantly abandoned that solitary place where nature had magnificently displayed herself before us. We deluded ourselves that we might again visit the Islands, but this, like many other plans, has never been carried out.

The fevers reigning in Cariaco forced us, to our regret, to shorten our stay there. As we were still not completely acclimatized, the inhabitants to whom we had been recommended warned us not to delay. In the town we met many people who, through a certain ease of behaviour, or through being more broad-minded and preferring a United States type government, revealed that they were in contact with foreigners. For the first time we heard the names of Franklin and Washington enthusiastically pronounced. With these shows of enthusiasm we heard complaints about the present state of New Andalusia, exaggerated enumerations of their natural wealth, and passionate and impatient hopes for a better future. This state of mind struck a traveler who had been witness to the great political upheavals in Europe.

May 13th. We left Mandavaca at half past two in the morning. After six hours of travelling we passed the mouth of the Idapa or Siapa on the east. It rises on the Uturan mountain. It has white waters. Its upper course has been strangely misrepresented on La Cruz's and Surville's maps, which all later maps have imitated. We stopped near the Cunuri raudal. The noise of the little cataract got much louder during the night. Our Indians said that meant certain rain. It fell before sunrise. However, the araguato monkeys' continuous wails had warned us that rain was approaching.

We were forced to cut our own track across the malpaís. The slope is very steep, and the volcanic blocks slipped under our feet. The rubble on the peak's summit has sharp edges and leaves gaps into which explorers risk falling up to their waists. Unfortunately the laziness and bad temper of our guides made this ascent more difficult. They were despairingly phlegmatic. The night before they had tried to convince us not to pass beyond the limit of the rocks. Every ten minutes they would sit down to rest; they threw away pieces of obsidian and pumice-stone that we had carefully collected. Finally we realized that none of them had ever visited the volcano's summit before.

While on the spot I sketched a view (17) of the crater's interior edge as it is seen on the descent through the eastern wall's breach. Nothing is more striking than the superimposition of these lava strata, which reveals similar sinuosities to the calcareous rock of the Alps. These enormous ledges, sometimes horizontal and sometimes sloping or undulating, reminded us that long ago the entire mass had flowed, and that a combination of disruptive causes determined a particular flow. The Crest of the wall exhibits the same strange ramifications we find in coke. The northern edge is the highest. Towards the south-west the wall has considerably subsided and an enormous amount of scoria seems glued to the outer edge. On the west the rock is perforated, and through a wide opening you can see the sea and horizon. Perhaps the force of the steam broke through here just when the lava overflowed from the crater.