We knew that the whole of the beds of the present seas must be receiving the washings of the rivers and the bodies of many fishes and animals, and that the rocks of the future must be forming down there by these accumulations. Long lines were let down from the ship with a dredge at the end, and thus parts of the bottom of the sea were brought up and carefully examined. It was found that the washings, stones, clay, and mud of the land were carried hundreds of miles out to sea, and laid upon the bottom. But in the deeper parts, where the Alps would be almost covered—there was a fine grey mud composed almost entirely of the shells of the little foraminifera, and this, no doubt, is the chalk of future times, or perhaps limestone of a harder kind. Deeper, too, than where this grey mud is found, there is a reddish mud, exceedingly fine and soft. We cannot exactly say yet whether this is formed from the remains of shell-fish; but it is, at all events, very like the clay of the land, and in some future time will most likely become like that stiff mud we know so well. So that even the materials for bricks are being made now, and perhaps when all those hundreds of islands scattered about the Pacific Ocean are joined into one great Continent, this red mud will be raised and made use of for building the houses of new peoples and nations. When we see this going on now, of course it is very easy to conclude that the chalk, a great deal of which is above the sea now, must have been formed in the same way at the bottom of an ancient ocean, and afterwards raised by the same kind of upward force which made the granite break through other earths. If we did not know that the same cause was at work now, and that the same kinds of shell-fish were living and laying down new beds of chalk under the sea, we should not know how to account for the quantities of chalk in the world. For innumerable ages these little creatures have thus been paving the floor of the ocean with their dead bodies, and you may suppose that countless millions of them must have lived and died! In some of the chalks the shells of the foraminifera can be quite distinctly seen with a microscope, and when these are compared with the shells of living ones, they are seen to be almost exactly alike. Next time you pass through one of the railway cuttings through the chalk in going to Brighton, or Ramsgate, or Dover, remember that those high cliffs were built up by these Liliputian giants under the sea, and you may think of the chalk as “foraminifera earth”. COAL.