| OCR Text |
Show Photographs as follows 102 show the nature of the exposed bed , bars , and banks between Moab and the mouth of the Green River : Exhibit 77 , Photographs ( Nbs Nos ) . 70 , 71 , 75 , 77 , 84 ) 862 1502 151 , 1532 155y 156Y 1582 1609 163 , 165Y 1679 168 , . A complete description of the temporary nature of the typical ( side sidle ) sand bar is described on page 71 , Exhibit 75 , and plate 36 of Exhibit 76 . Testimony of Virgil Baldwin , who ( lias has ) made more boat trips on Colorado River belo , v Moab than all the rest of the witnesses put together , proves ( con- con ) ( clusively clusi-vely clusively ) that ( conditions cond-itions 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 , ( uiiconsolidated unconsolidated ) mass of sand and silt so spread out that the channel , if any , is obscured . ' Dent ( Vol . 7 , page 1227 ) describes the Colorado River as very changeable between its rock walls . Richardson ( Vol . 20 , page 3692 ) describes ( 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 ) ing character of the bed of the Colorado ( River Rivei ) downstream from Moab is contained in the record as follows ; . ( Hoy Hoyt ) ( Vol . 2 , page 210 ) ; ( Pronimel Prommel ) ( Vol . 6 , page 1034 ) ; Baldwin ( Vol . 6 , pages 1166 . , 1180 , 1184 ) ; Galloway ( Vol . 6 , ( page pacre ) 1055 ) ; Cleary ( Vol . 16 , page 2926 ) ; Edwards ( Vol . 10 , page 1909 ) ; Dugan ( Vol . 16 , page 2992 ) - Ross ( Vol . 24 , page 4307 ) ; Baldwin ( Vol . 29 , p . 5074 ) . |
