"There was fighting and fighting between the old and new school, and all on a question that would make a crab laugh,--questions that were hypercritical and infinite, and about which everybody knew nothing at all, and they thought they knew as well as God. Questions were talked of with positiveness, and argued; and, when I look back upon them, I cannot help thinking they were no better than the contentions of children around the cradle. But all this gave me great repulsion for dogmatic theology, and it is a repulsion which I have not got over, and the present prospects are that I never shall."--_Henry Ward Beecher_. EARTHQUAKES AND PREDICTIONS.--Professor Rudolf Falb, of Vienna, it is reported, predicted to an hour the earthquakes which have occurred in France and Italy. "Writing in the Austrian papers some days ago, he pointed out that the annular eclipse of the sun, which commenced on Tuesday morning at 6.41 Greenwich time, was central at 9.13 P. M., and ended on the earth generally at twenty-five minutes past midnight on Wednesday morning, was likely to be accompanied with strong atmospheric and seismic disturbances. The learned physicist has gained great reputation by previous similar forecasts. His first and great success was the foretelling the destructive shock at Belluno, on June 29, 1873. Nearly the whole of Northern Italy was affected, and upwards of fifty lives were lost. Very shortly afterwards he gave warning of the probability of an eruption of Etna, which followed at the time anticipated in 1874."--_London Echo_. "John S. Newberry, professor of geology and paleontology at Columbia College, being the American authority upon all matters pertaining to the crust of the earth, was naturally interested in the earthquake that visited Long Island on Wednesday. He derides the idea that the local seismic disturbance has any connection with the recent occurrences at Mentone, as the shocks were too far apart, and, if connected, should have been felt within eight hours of each other, whereas there was several days' difference. His theory, which is amply sustained by observation, is that an earthquake is a movement caused by a shrinking, from loss of heat, of the interior of the earth and the crushing together and displacement of the rigid exterior as it accommodates itself to this contraction. It has been noticed that the earth is shaken along the Alleghany chain nearly every year. It is impossible to predict a recurrence of the shocks, but it is quite probable they will recur. There is a record of 231 earthquakes in the New England States between the years 1638 and 1869."--_Brooklyn Eagle_. CHAPTER II--STRUCTURE OF THE BRAIN.