OCR Text |
Show Compl . Exhibit 77 , Photographs 147 Nos . 70 , 71 , 75 , , 77 ) ( 84 S4 ) ( , ; ) ( 86 S6 ) ( , ) ) 150 ( , ) ) 151 , 153 , ( 155,156y 155156y ) 158 , 160 , 163 ) 165 ) 167 ) 16S . A complete description of the temporary nature of the typical side sand bar is described on page 71 , Compl . Exhibit 75 , and plate 36 of Compl . Exhibit 76 . Testimony of Virgil Baldwin ( Abs . R . vol . 1 , p . 307 ) , who has made more boat trips on Colorado River below Moab than all the rest of the witnesses put together , shows that conditions on the Colorado River are similar to that already described on the Green River and that the river throughout , except at The Slide , flows over unstable , shifting , unconsolidated mass of sand and silt so spread out that the channel , if any , is obscured . Dent ( Abs . R . vol . 1 , p . 328 ) describes the ( Colo- Colo ) rado River as very changeable between its rock walls . Richardson ( Abs . R . vol . 2 , p . 936 ) describes ( shift shift- shift ) ing character of the bed of Colorado River at its junction with the Green River . Additional testimony with reference to the ( shift shift- shift ) ing character of the bed of the Colorado River downstream from Moab is contained in the record . ( 10 " ) Colorado River Through Cataract Canyon . ( -No No ) evidence has been introduced to show that there is decided shifting of river bed in this stretch . Kolb , who has been through 10Hoyt ( Abs . ( E R ) . vol . 1 , p . 26 ) ; Prommel ( Abs . ( E R ) . vol . 1 , p . 268 ) ; Baldwin ( Abs . ( E R ) . vol . 1 , p . 307 ) ; Galloway Abs . R . vol . 1 , p . 284 ) ; Cleary ( Abs . R . vol . 2 , p . 749 ) ; Edwards ( Abs . ( E R ) . vol . 2 , p . 767 ) ; Dugan ( Abs . ( E R ) . vol . 2 , p . 775 ) ; ( Eoss Pcss ) ( Abs . ( E R ) . vol . 2 , p . 1055 ) ; Baldwin ( Abs . ( E R ) . vol . 1 , p . 307 ) . |