Among the three formations of cirrus, cumulus and stratus, the cumulus has a special place as representing in the most actual sense what is meant by the term ‘cloud’. The reason is that both cirrus and stratus have characteristics which in one or the other direction tend away from the pure realm of atmospheric cloud-formation. In the stratus, the atmospheric vapour is gathered into a horizontal, relatively arched layer around the earth, and so anticipates the actual water covering below which extends spherically around the earth’s centre. Thus the stratus arranges itself in a direction which is already conditioned by the earth’s field of gravity. In the language of physics, the stratus forms an equipotential surface in the gravitational field permeating the earth’s atmosphere.