All electrical action also ceased, which fully confirms the theory, of Professor Faraday, that "electricity is a force generated by the rapid axial revolution of the earth, and that magnetic attraction in all cases points or operates at right angles to its current." Hence electricity, from the nature of its cause, must be superficial.

Every appearance of water disappeared at the depth of only 9000 feet. From this depth downward the rock was of a basaltic character, having not the slightest appearance of granite formation—confirming, in a most remarkable manner, the discovery made only last year, that all granites are of aqueous, instead of igneous deposition. As a corollary from the law of atmospheric pressure, it was found utterly impossible to vaporize water at a greater depth than 24,000 feet, which point was reached in 1869. No amount of heat affected it in the least perceptible manner, and on weighing the liquid at the greatest depth attained, by means of a nicely adjusted scale, it was found to be of a density expressed thus: 198,073, being two degrees or integers of atomic weight heavier than gold, at the surface.

The report then proceeds to discuss the question of the true figure of the earth, whether an oblate spheroid, as generally supposed, or only truncated at the poles; the length of a degree of longitude at the latitude of Dudzeele, 51 deg. 20 min. N., and one or two other problems. The concluding portion of the report is reproduced in full.

For the past twelve months it was found impossible to endure the heat, even sheltered as the miners were by the atmospheric cover and cage, for more than fifteen minutes at a time, so that the expense of sinking had increased geometrically for the past two years. However, important results had been obtained, and a perpendicular depth reached many thousands of feet below the deepest sea soundings of Lieutenant Brooks. In fact, the enormous excavation, on the 1st of November, 1872, measured perpendicularly, no less than 37,810 feet and 6 inches from the floor of the shaft building! The highest peak of the Himalayas is only little over 28,000 feet, so that it can at once be seen that no time had been thrown away by the Commissioners since the inception of the undertaking, in April, 1849.

The first symptoms of alarm were felt on the evening of November 1. The men complained of a vast increase of heat, and the cages had to be dropped every five minutes for the greater part of the night; and of those who attempted to work, at least one half were extricated in a condition of fainting, but one degree from cyncope. Toward morning, hoarse, profound and frequent subterranean explosions were heard, which had increased at noon to one dull, threatening and continuous roar. But the miners went down bravely to their tasks, and resolved to work as long as human endurance could bear it. But this was not to be much longer; for late at night, on the 4th, after hearing a terrible explosion, which shook the whole neighborhood, a hot sirocco issued from the bottom, which drove them all out in a state of asphyxia. The heat at the surface became absolutely unendurable, and on sending down a cage with only a dog in it, the materials of which it was composed took fire, and the animal perished in the flames. At 3 o'clock a. m. the iron fastenings to another cage were found fused, and the wire ropes were melted for more than 1000 feet at the other end. The detonations became more frequent, the trembling of the earth at the surface more violent, and the heat more oppressive around the mouth of the orifice. A few minutes before 4 o'clock a subterranean crash was heard, louder than Alpine thunder, and immediately afterward a furious cloud of ashes, smoke and gaseous exhalation shot high up into the still darkened atmosphere of night. At this time at least one thousand of the terrified and half-naked inhabitants of the neighboring village of Dudzeele had collected on the spot, and with wringing hands and fearful outcries bewailed their fate, and threatened instant death to the officers of the commission, and even to the now terrified miners. Finally, just before dawn, on the 5th of November, or, to be more precise, at exactly twenty minutes past 6 a. m., molten lava made its appearance at the surface!

The fright now became general, and as the burning buildings shed their ominous glare around, and the languid stream of liquid fire slowly bubbled up and rolled toward the canal, the scene assumed an aspect of awful sublimity and grandeur. The plains around were lit up for many leagues, and the foggy skies intensified and reduplicated the effects of the illumination. Toward sunrise the flow of lava was suspended for nearly an hour, but shortly after ten o'clock it suddenly increased its volume, and, as it cooled, formed a sort of saucer-shaped funnel, over the edges of which it boiled up, broke, and ran off in every direction. It was at this period that the accomplished Dusoloy, so long the Superintendent, lost his life. As the lava slowly meandered along, he attempted to cross the stream by stepping from one mass of surface cinders to another. Making a false step, the floating rock upon which he sprang suddenly turned over, and before relief could be afforded his body was consumed to a crisp. I regret to add that his fate kindled no sympathy among the assembled multitude; but they rudely seized his mutilated remains, and amid jeers, execrations, and shouts of triumph, attached a large stone to the half-consumed corpse and precipitated it into the canal. Thus are the heroes of science frequently sacrificed to the fury of a plebeian mob.

It would afford me a pleasure to inform the department that the unforeseen evils of our scientific convention terminated here. But I regret to add that such is very far from being the case. Indeed, from the appearance of affairs this morning at the volcanic crater—for such it has now become—the possible evils are almost incalculable. The Belgian Government was duly notified by telegraph of the death of the Superintendent and the mutinous disposition of the common people about Bruges, and early on the morning of the 6th of November a squad of flying horse was dispatched to the spot to maintain order. But this interference only made matters worse. The discontent, augmented by the wildest panic, became universal, and the mob reigned supreme. Nor could the poor wretches be greatly condemned; for toward evening the lava current reached the confines of the old village of Dudzeele, and about midnight set the town on fire. The lurid glare of the conflagration awakened the old burghers of Bruges from their slumbers and spread consternation in the city, though distant several miles from the spot. A meeting was called at the Guildhall at dawn, and the wildest excitement prevailed. But after hearing explanations from the members of the commission, the populace quietly but doggedly dispersed. The government from this time forward did all that power and prudence combined could effect to quell the reign of terror around Bruges. In this country the telegraph, being a government monopoly, has been rigorously watched and a cordon of military posts established around the threatened district, so that it has been almost impossible to convey intelligence of this disaster beyond the limits of the danger. In the mean time, a congress of the most experienced scientists was invited to the scene for the purpose of suggesting some remedy against the prospective spread of the devastation. The first meeting took place at the old Guildhall in Bruges and was strictly private, none being admitted except the diplomatic representatives of foreign governments, and the members elect of the college. As in duty bound, I felt called on to attend, and shall in this place attempt a short synopsis of the proceedings.

Professor Palmieri, of Naples, presided, and Dr. Kirchoff officiated as secretary.

Gassiot, of Paris, was the first speaker, and contended that the theory of nucleatic fusion, now being fully established it only remained to prescribe the laws governing its superficial action. "There is but one law applicable, that I am aware of," said he, "and that is the law which drives from the center of a revolving body all fluid matter toward the circumference, and forcibly ejects it into space, if possible, in the same manner that a common grindstone in rapid motion will drive off from its rim drops of water or other foreign unattached matter. Thus, whenever we find a vent or open orifice, as in the craters of active volcanoes, the incandescent lava boils up and frequently overflows the top of the highest peak of the Andes."

Palmieri then asked the speaker "if he wished to be understood as expressing the unqualified opinion that an orifice once being opened would continue to flow forever, and that there was no law governing the quantity or regulating the level to which it could rise?"