The _Salto de Tequendama_, a remarkable cascade, of which we had heard much, and which has been described in most glowing language, is distant to the southwest of Bogotá about fifteen miles. We had made arrangements to visit it a fortnight ago, but the illness of one of our party caused us to defer it. We now determined to see the fall, and return to the city on the same day. To accomplish our design, we set out before day (about 5 o'clock) this morning. A rapid ride of an hour and a half brought us to the small village of Suácha, situated upon the plain of Bogotá, near its southern border. The last earthquake, from which Bogotá suffered so severely, was felt with the utmost violence at Suácha, and prostrated entirely the church, which is again rising from its ruins. Our route continued a league further over the plain, and we crossed the river Funza, whose course has been very circuitous through the plain, but is particularly devious where we passed over it, upon an uncouth and not very safe bridge, to the Hacienda de Canoas. The river winds sluggishly to our left towards the fall. Our path led over the high hills which appear to have been once the banks of the great lake which must have covered the plain which the view from these heights embraces. To eminences which are wholly devoid of trees succeed others which are well wooded, where we enter a more picturesque region, worthy of the fine scene which we were now eager to witness. We were convinced that we were near it, and listened for the deafening roar which we expected would betray the rush of the waters into the tremendous gulf that receives them. The path was steep, and shortly before we arrived at the spot where it was necessary to alight from our horses, the sounds of the fall reached us; but we were distant from it a few hundred yards only. My first sensation was disappointment, when I stood upon the brink of the chasm into which a stream whose greatest width is estimated at forty feet, is precipitated to a depth which did not seem to exceed three hundred feet, but which is estimated to be more than six hundred. The river being now uncommonly low, a sheet of water about fourteen or fifteen feet in width, is tossed about thirty feet upon a ledge of rocks, from which it dashes in foam to the bottom of the deep abyss, a large proportion of it dissipating in spray. The foot of man has never trodden the bottom of this chasm. Its sides are perpendicular to a considerable distance below, and the strata of rock are exactly horizontal, so that no means of descending have yet been discovered within the curvilinear aperture, where the mountain seems to have parted and given passage to the Funza.