Page:The evolution of worlds - Lowell.djvu/206

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THE EVOLUTION OF WORLDS

or Saturnian clouds, we do not know; but that it was once hot enough to vaporize water we are perfectly certain. And this from proof both of what did exist

Juke Butte, a denuded laccolith, as seen from the northwest—Gilbert.

and of what did not. That the surface temperature was at one time in the thousands of degrees Fahrenheit, the Plutonic magma underlying all the sedimentary rocks of the Earth amply shows. Reversely, the absence of any effect of water until we reach these sedimentary deposits, testifies that during all the earlier stages of the Earth's career water as such was absent, and as water subsequently appeared, it is clear that the Ideal section of a laccolith—Gilbert. conditions did not at first allow it to form. We are sure, therefore, that there was a time when water existed only as steam, and very possibly a period still anterior to that when it did not exist at all, its constituent hydrogen and oxygen not having yet combined. There was certainly an era, then, in the morning of the