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Show 3.184 ( Gv'oss-Jihianwiatioii GvossJihianwiatioii ) ( B R ) ( 'Vol Vol Nrol ) 26 ( '4687- '468,7- ) . , . , pp . 4694 ) : The stage of water was probably a little higher when ( he lie ) went down ( in iii ) 1908 , as it would ( undoubtl- undoubtl ) edly be higher in the first part of May than it would be in the middle of July of any ( year' year ) , ( ordi- ordi ) ( narily iiarily ) speaking . He ( can't cant ) say anything in regard to his recollection ; and in making that answer he is frank in ( stating statiug ) that he is going on what he knows in regard to the discharge of the stream . It would be simply a guess , but he ( would -Niould Niould ) say it was probably about six thousand ( second-feet secondfeet ) when he started from Greenriver on his first trip . ( R . 4687-4688 . ) He has been raised on water , and has traveled a great deal on boats all his life ; his main practice in civil engineering has been hydraulic engineering . He has just formed some ideas of stream flow . His estimate on stream flow would be based on his ( gen- gen ) eral knowledge of the flow of the Green River , from ( studying studyilig ) the records of the river . He could only make an estimate of the flow in ( second-feet secondfeet ) of the river when he started on his second trip , but he is willing to make the estimate right out loud , so everyone can hear it . The river averages about six hundred feet in width . The quieter part of the river is quite ( shal- shal ) low ; maybe only a foot or ( so s3 ) deep . The rest of the river would be two or three , four , five or six feet deep . This would be where the main flow of the |