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In our publications Bonpland and I have considered every phenomenon under different aspects, and classed our observations according to the relations they each have with one another. To convey an idea of the method followed, I will outline what we used in order to describe the volcanoes of Antisana and Pichincha, as well as Jorullo, which on the night of the 20th of September 1759 rose 1, feet up from the plains of Mexico. We fixed the position of these remarkable mountains in longitude and latitude by astronomical observations. We took the heights of different parts with a barometer, and determined the dip of the needle and magnetic forces. We collected plants that grew on the slopes of these volcanoes, and specimens of different rocks. We found out the exact height above sea-level at which we made each collection. We noted down the humidity, the temperature, the electricity and the transparency of the air on the brinks of Pichincha and Jorullo; we drew the topographical plans and geological profiles of these volcanoes by measuring vertical bases and altitude angles. In order to judge the correctness of our calculations we have preserved all the details of our field notes.

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