The Atlantic Monthly, Volume 09, No. 55, May, 1862 by Various
page 103 of 277 (37%)
page 103 of 277 (37%)
![]() | ![]() |
|
|
the latter, at a depth of sixty-four feet, is under a weight equal to
that of three such atmospheres, which is reduced to one when it reaches the sea-level. The change is even much greater for those fishes that come from a depth of several hundred feet. These laws of limitation in space explain many facts in the growth of Coral Reefs that would be otherwise inexplicable, and which I will endeavor to make clear to my readers. For a long time it was supposed that the Coral animals inhabited very deep waters, for they were sometimes brought up on sounding-lines from a depth of many hundreds or even thousands of feet, and it was taken for granted that they must have had their home where they were found; but the facts recently ascertained respecting the subsidence of ocean-bottoms have shown that the foundation of a Coral wall may have sunk far below the place where it was laid, and it is now proved beyond a doubt that no Reef-Building Coral can thrive at a depth of more than fifteen fathoms, though Corals of other kinds occur far lower, and that the dead Reef-Corals sometimes brought to the surface from much greater depths are only broken fragments of some Reef that has subsided with the bottom on which it was growing. But though fifteen fathoms is the maximum depth at which any Reef-Builder can prosper, there are many which will not sustain even that degree of pressure, and this fact has, as we shall see, an important influence on the structure of the Reef. Imagine now a sloping shore on some tropical coast descending gradually below the surface of the sea. Upon that slope, at a depth of from ten to twelve or fifteen fathoms, and two or three or more miles from the main-land, according to the shelving of the shore, we will suppose that one of those little Coral animals to whom a home in such deep waters is genial has established itself. How it happens that such a being, which |
|


