The rounded Turimiquiri summit and the sharp peaks, or cucuruchos, stand out, covered with jungle where many tigers live and are hunted for the beauty of their skin. We found that this grassy summit stood at 707 toises above sea-level. A steep rocky ridge going west is broken after a mile by an enormous crevice that descends to the Gulf of Cariaco. In the place where the mountain ridge should have continued two mamelons or calcereous peaks rise, with the more northern one the highest. It is the Cucurucho de Turimiquiri proper, considered to be higher than the Brigantín, well known to sailors approaching the Cumanà coast.

On my arrival at Terra Firma I was struck by the correlation between two natural phenomena: the destruction of Cumanà on the 14th of December 1797 and volcanic eruptions in the smaller West Indian Islands. Something similar happened at Caracas on the 26th of March 1812. In 1797 the volcano on Guadeloupe Island, on the Cumanà coast, seemed to have reacted; fifteen years later another volcano on San Vincente also reacted, and its effects were felt as far as Caracas and the banks of the Apure. Probably both times the center of the eruption was at an enormous depth in the earth, equidistant from the points on the earth's surface that felt the movement. The shock felt at Caracas in December 1811 was the only one that preceded the terrible catastrophe of the 26th of March 1812. In Caracas, and for 90 leagues around, not one drop of rain had fallen for five months up to the destruction of the capital. The 26th of March was a very hot day; there was no wind and no cloud. It was Ascension Day and most people had congregated in the churches. Nothing suggested the horrors to come. At seven minutes past four the first shock was felt. 'It was so violent that the church bells rang, and lasted five to six seconds. It was followed immediately by another lasting ten to twelve seconds when the ground seemed to ripple like boiling water. People thought the quake was over when an infernal din came from under the ground. It was like thunder but louder and longer than any tropical storm. Following this there was a vertical movement lasting three seconds followed by undulations. The shocks coming from these contrary movements tore the city apart. Thousands of people were trapped in the churches and houses. (78)