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 



hillsides, similarly contoured to those of the north, which lie south 

 of and immediately adjoining Trench Gulch. 



Through virtually the entire Klondike tract and far beyond it 

 on all sides there are evidences of high water flows. No more per- 



