Home / Tower, Fayette B. Illustrations of the Croton Aqueduct. New York: Wiley and Putnam, 1843. / Passage

Illustrations of the Croton Aqueduct

Tower, Fayette B. Illustrations of the Croton Aqueduct. New York: Wiley and Putnam, 1843. 254 words

But though water expands by heat and contracts by cold, there is even a limit to this law, for had there not been, the lower parts of water would have frozen first, and thus entire lakes, rivers and oceans, perhaps, become solid, and had they become thus frozen, they would have remained so ; for, as the heat at the surface would not have descended far through the colder parts, the

main body of the ice must forever have remained solid, as in the arctic circle. To obviate this great disadvantage, water contracts by the increase of cold till we come

near the freezing temperature, (40° F.) when it begins to expand and continues so to do till it freezes ; at 32° F. Hence, water at 40° is at its greatest density and

will lie at the bottom, with cooler water or ice floating above it. However much the surface be cooled, water colder than 40° cannot descend to displace water warmer

than itself. Hence we never can have ice formed at the bottom of deep water, though it is not uncommon to find it thus situated, in shallow streams or rivers of rapid flow. Here the temperature of the whole body of water is brought down to the freezing point, and in freezing the ice adheres to the sides and bottom of the

stream. What a beautiful provision is this, that the coldest water should rise to the surface, and there freeze and remain, exposed to the warmth of the sun-beams and