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Show form . The exhibits ( represent reprosent ) 60 ( minimum ininfintini ) or ( fair fidix ) ( Con- Con ) ditions and do not apply to any section where ( rap- rap ) ids , riffles , or contraction in the channel occur . It was pointed ( out otit ) in oral testimony by Hoyt ( Vol . 23 , ( page -page page ) 4154 ) that the velocities as shown for the ( Green GTecii ) River station near Green River ( Utah Utali ) ( might illiglit ) , , be fairly indicative of velocities in the reasonably straight stretches of Green River located between the mouth of the San Rafael River and the mouth ; that the velocities as shown for the ( Colorado ColoradD ) River near Cisco , Utah , might be fairly indicative of the Colorado River between Moab and the mouth of the Green , with the exception of the section at The Slide ; that the velocities as ( shown s1lown ) at the Lees Ferry gaging station might be ( fairly faiTly ) indicative of ( veloci veloci- veloci ) ties through the Glen Canyon section except at those stretches which , on account of excessive slopes or contraction resulting from bedrock or gravel and boulder obstructions at the mouths of streams or . washes have been characterized as rapids or rapid water stretches ; and that the velocity records at the Bluff station might be fairly indicative of stretches ( on oii ) the San ( Juan Juaia ) other than those on which rapids occur . Green River near ( Green Greem ) River , Utah . ( -As As ) shown on plate 2 , Exhibit ( 82-A 82A ) , the velocity in the thread of ( the t1le ) ( current curreiit ) ranges from less than 2 miles an hour |