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Show record , as follows : Hoyt 100 ( Vol . 1 , page 159to 173 , Vol . 2 , pages ( 184-200 184-20-0 ) ) ; Lumnsden ( Vol . 4 , page 672 ) ; Kolb ( ( Yol Vol ) . 5 , page 827 ) ; Blake ( Vol . 5 , page 954 ) ; Galloway ( Vol . 6 , page 1058 ) ; Edwards ( Vol . 11 , page 1953 ) ; Sawyer ( Vol . 11 , page 2119 ) ; ( I'VIc- IVIc ) Donald ( Vol . 12 , page 2195 ) ; Loper ( Vol . 13 , page 2408 ) ; Newby ( Vol . 17 , page 3259 ) ; Yokey ( Vol . ( 18 is ) , page 3425 ) ; Richardson ( Vol . 20 , page 3692 ) ; Hoyt ( Vol . 23 , page 4124 ) ; Ross ( Vol . 24 , page 4233 ) . ( Colorado Co7orado ) ( River Biver ) ( from froin ) the mouth of the Green to ( Modb Ifoab ) . Except at The Slide and perhaps one or two isolated localities , the Colorado River ( "between between between ) Moab and the mouth of the Green River flows in a canyon fill of unconsolidated shifting sand and silt . ( Exhibit 75 . ) ( The -The The ) limits of horizontal shift are fixed , by the adjacent rock walls and talus slopes , but betweenthese ( limits Ihnits ) the river meanders ( simi- simi ) larly to the Green . ( Any Iny ) one of the bars shown on Plates 30 ( to -to to ) 33 ( Exhibit 76 ) could , with a few changes in general dimensions , be used to illustrate bars along the Colorado . Roughly , there are about 2.7 acres of low exposed sand ( bars baTS ) to the mile along the Colorado compared to about 1.4 acres to the mile ( along aloncr ) the Green below the San Rafael . This ratio ( would ivould ) probably hold true for the submerged ( crossing crosshig ) bars . All side and crossing bars are noted with appropriate ( symbols syi-nbols syinbols ) on the ( river-survey riversurvey ) maps , Plates 44 , 45 , and 46 . ( Exhibit 78 . ) ( Outstanding Outstand'1119 Outstand1119 ) bars ( with ivith ) ( shallow sliallow ) depths ( were -were were ) observed at Mile 3.5 ( 4 ZI ) 4.9 7.8 10 11.8 14 16.5 19.5 21 21.5 22 28 , , , , , , , , , , , , , |