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Show ( Vol . 4 , pages 726 77 , 737 ) ; Kolb ( Vol . 4 page ° 790 ; Vol . 5 , page 821 ) ; Blake ( Vol . 5 , ( page pacre ) 912 ) ; Galloways ( ( Vol AT"ol ATol ) . 6 , pages 112 , 1126 , 1144 ) ; Baldwin ( VoL 6 , page 1189 ) ; Aurand ( Vol . 7 , page 1354 , bars mile 2 , 4 , 14 , 18,20 , 232 24 ( , ) ) 25 ( , ) ) 271 301 31 ) ; Lint ( Vol . 8 , page 1480 ) ; ( Dellenbaugh Dellenbaugli ) ( Vol . 9 , page 1528 ) ; Clark ( Vol . 9 , page 1710 ) ; ( Stone Stoiie ) ( Vol . 10 , page 1782 ) ; ( Eodin Rodin ) ( Vol . 10 , page 1802 ) ; ( Woodbuiy Woodbury ) ( Vol . 10 , page 1816 ) ; Edwards ( Vol . 10 , page 1907 ) ; Kane ( Vol . 11 , page 2003 ) ; Sawyer ( Vol . 11 , pages 2099 , 2113 ) ; 2YIeDonald ( Vol . 12 , page 2173 ) ; Loper ( ( Vol Yol ) . 13 , page 2347 ) ; Bennett ( Vol . 17 , page 3225 ) ; Newby ( Vol . 17 , page 3244 ) ; ( Tokey Yokey ) ( Vol . 18 , pages 3425 , 3440 ) ; ( Keeside Reeside ) ( ( Vol Yol ) . 21 , page 3925 ) ; Nye ( Vol . 24 , page 4183 ) ; Ross ( Vol . 24 , page ( 4198 1198 ) ) ; ( Photographs as follows : Ex . 77 , Nos . 22 , 231 26Y 312 322 111 ) . ( Colorado Coloi-ado Coloiado ) ( River Rive ) near Cisco , ( Utah Utak ) . ( -On On ) Plate 3 , Exhibit ( 82-A7 82A7 ) it is shown that the mean depth at the gaging ( station statioii ) varies from less than 3 feet when the discharge is about 2,000 ( second-feet secondfeet ) to mean depths of 20 feet with flood flows of 60,000 to 70,000 ( second-feet secondfeet ) . As shown ( on oil ) Plate 9 , Exhibit ( 82-A 82A ) , the mean ( depth d9pth ) for half ( the tlie ) time is less than ( 3,8 3.8 ) feet . ( Depth Deptli ) in channel Moab to ( mouth moutlb ) . ( Testimony -Testimony Testimony ) by W . ( Gr G ) . Hoyt ( Vols . 1 and 2 ) , based on observations described on pages 73 and 74 , Exhibit 75 , indicates that the ( deep deep- deep ) ¬ est part in cross section at the following locations ( was ivas ) , in general less than 2.5 feet during the period , |