from the Earth: The surface of the Earth becoming saturated, and in some places penetrating into the seams and crevices of rock and soil, at once forms a medium of attraction for the waters below to follow. Another valid reason is the general condition of the atmosphere from the time of drouth to a condition of moisture when it becomes really a mammoth sponge after being dampened. Against the claim that rainfall has little or no influence in raising or producing springs or lakes, or living wells, this question naturally arises regarding springs, which has in a measure been answered. It is, however, a pertinent question, and a pleasant one to answer fully. In the summer season, most commonly of any, the air becomes hot and dry. The surface of the Earth loses the moisture of the air’s influence, together with the Sun’s heat evaporating the dampness, becomes generally arid, and fails thereby to be a conductor of the moisture from below. As a season of very dry atmosphere occurs for months at times, the soil becomes correspondingly dry and dusty to quite a depth. From this cause the springs and water in wells recede and sink away. It is an easy matter to find people who have witnessed the following seeming phenomena in times of drouth: After a period of weeks or months of drouth before any rainfall has occurred at all, the fountains, long dry, often commence to run, and wells begin to fill with water, and this without a drop of rain. Just here comes the pleasant task of answering the question fully: How can this occur without a soaking rain? At such times, when the Earth and all nature is thirsting for water, and every fountain seems to have dried up forever, the day will come which will bring these evidences. The aged will complain of their rheumatism; men’s bones will ache; geese will wash in the dust; the peacock will scream; birds, beasts and vegetation will feel a humidity in the air and intuitions that rain is near. As the atmosphere has felt the approach and preparation for rain some time in advance, so all Nature feels its effects. To illustrate the burned or dry condition of the air, you may consider this test: Take a pail of water, and a dry sponge, big as your head, and lay the sponge on the surface, and it will take a long time for the sponge to absorb the water and become fully saturated. Wet the sponge before the test and squeeze it dry as you can, and lay it on, and it will fill rapidly and quickly. Pour a pail of water on the floor and try the same experiment. Your sponge will not fill at all if dry, only a little as it comes in contact with the water; but moisten it as before, and press it nearly dry, and throw on the puddle of water, and it will drink itself full at once, drawing up the water like a pump. You cannot wipe up a floor with a dry sponge.