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GEOLOGY OF THE KLONDIKE GOLD FIELDS.
307
on the less favored bank of the streams, and surely in the case of the Eldorado former evidence of this deposition ought to be had on the
Grand Forks Village—Valley of the Bonanza
hillsides, similarly contoured to those of the north, which lie south of and immediately adjoining French Gulch.
Through virtually the entire Klondike tract and far beyond it on all sides there are evidences of high water flows. No more per-
