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Show The maps contained in 1036 ( Complainant's Complainants ) Exhibit No . . 10 were printed in 1926 and would indicate that the , checking was done before they were printed . ( All AU ) of these gages would be taken in consideration in making corrections , and they were taken into ( con- con ) sideration in making adjustments on these maps . The information you would have on it then would be the ( topographers' topographers ) notes , or , at least , their gage . - and the general knowledge that a flood on the San Juan would make a very great difference on the . water level of the Green and Colorado . ( R . 4073 . ) The adjustment would not change the general picture of the profile at all , because the slope ( or or- or ) gradient in general is such that a minor fluctuation makes very little difference in it . At some ( par- par ) ticular point it might make a difference of a few feet , and would change the slope a few per cent at that particular place . That brings him to the point of the change in the slope of a rapid between low stage and high stage . ( R . 4074-4075 . ) The general type of the slope would , of course , vary from low stage to high stage . The rapid will appear on any profile , however , as a rapid . It would not ( appear appear- appear ) as more of a rapid the higher the profile went . The rapid would appear shorter and sharper at a low stage , and longer and flatter at a high stage . There would be a difference in appearance ; yes , sir . ( R , 4073-4075 . ) |