The water has now reached its highest point, and will soon begin to recede and continue to do so till the old confines are reached. Residents of the locality say that the weather conditions have no effect upon the lake, for its rise in the seventh year takes place regardless of the fact of rain or drouth. Amos Jordan, a veteran of the civil war, who lives on a bluff overlooking the lake, says the only apparent difference between wet and dry seasons when the rise occurs is that the water appears to be colder in time of drouth. What is true of the rise of the waters is also true of their recession, for they gradually disappear regardless of the amount of rainfall in the county. The phenomenon is explained on the theory that there is a subterranean outlet, which becomes closed in some way and is opened by the pressure of the water when the highest point is reached every seventh year; but this is mere guesswork and nothing has ever been discovered to justify such a theory. The Pennsylvania Railroad Company, which owns a number of ice-houses on the edge of the lake, made soundings at different places before the rise began, and found the greatest depth to be ninety feet. * * * * * Hundreds more of such clippings have been preserved in a scrap book describing similar phenomena all over the Earth, all of which seem solvable through claims herein set forth, in the combined influences of frictional and volcanic heat, and the occasional contact with outpouring streams from the _internal_ ocean of fresh water. THE END. TRANSCRIBER’S NOTES: Italicized text is surrounded by underscores: _italics_. Obvious typographical errors have been corrected. Inconsistencies in hyphenation have been standardized. Archaic or variant spelling has been retained.