, that my heart failed me, and a trembling almost disabled me. The rock moved under me, as the frightful sounds encreased, and as quick as it was possible for me, I came into day again. It was well I did; for I had not been many minutes out, before the water overflowed its channel, and filled the whole opening in rushing to the lake. The increase of the water, and the violence of the discharge, were an astonishing sight. I had a great escape. As the rocky mountain I have mentioned, is higher than either Snowden in North-Wales, or Kedar-Idris in Merionethshire, (which have been thought the highest mountains in this island), that is, it is full a mile and an half high from the basis, as I found by ascending it with great toil on the side that was from the water, and the top was a flat dry rock, that had not the least spring, or piece of water on it, how shall we account for the rapid flood that proceeded from its inside? Where did this great water come from?—I answer, might it not flow from the great abyss — and the great encrease of it, and the fearful noise, and the motion of the rock, be owing to some violent commotion in the abyss, occasioned by some natural or supernatural cause? That there is such an abyss, no one can doubt that believes revelation, and from reason and history it is credible, that there are violent concussions on this vast collection of water, by the divine appointment: and therefore, I imagine it is from thence the water of this mountain proceeds, and the great overflowing and terrifying sound at certain times. To this motion of the abyss, by the divine power exerted on it, I ascribe the earthquakes; and not to vapor, or electricity. As to electricity, which Dr. Stukeley makes the cause of the deplorable downfall of Lisbon*, in his book lately published, (called, The Philosophy of Earthquakes), there are many things to be objected against its being the origin of such calamities:—one objection is, and it is an insuperable one, that electrical shocks are ever momentary, by every experiment, but earthquakes are felt for several minutes. Another is, that many towns have been swallowed up in earthquakes, tho' Lisbon was only overthrown. Such was the case of the city of Callao, within two leagues of Lima. Tho' Lima was only tumbled into ruins, October 28, 1746; yet Callao sunk downright, with all its inhabitants,