OCR Text |
Show His deduction ( from froin ) ( that 'that that ) 369 is ( that Oat ) ( the die ) ( lessor lesser ) ve locity in that particular case , also ( something soiiietlihig ) of a change in sediment , causes the river to build a different type of river . ( R . 1304 . ) As a hypothetical ( case ca-se case ) : Supposing you had ( the tbe ) same volume of water , less velocity , the bars would form more slowly with the same fall , the same ( vol- vol ) ( ume unie ) of water but less velocity , but it would ( inher inber- inber ) ently require that the river have more width and . less depth . The assumption of ( volume voluine ) of ( water water- water ) and less velocity includes that assumption . If the river has the same volume of water ( same sa-me same ) , slope , and less velocity , then it is an inexorable law it have less depth and more ( width wiath ) . A swiftly moving stream moves the sediment more readily , of course , than a slow moving ( stream streain ) . . It moves it in places and then automatically drops it in eddies and points where , for some reason , it is possible for it to do so . ( R . 1305 . ) He ( would -would would ) say that the swift river puts ( every every- every ) thing in a turmoil , the condition that you find at any time is a condition of maximum stability . In other words , the river stirs things up , and it falls ( into ilito ) some accidental form . If that accidental form is a stable form , , capable of resisting the forces ( of of' of ) the river more than some other form does , then it lasts for a longer time , and they are , more likely to ( find filid ) it when they are investigating . The permanent ( form-every formevery ) sedimentary river has a form that is so ( wide ivide ) and so shallow that ( re- re ) ( 33307-31--VOL 3330731VOL ) . 1-2-1 |