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<br /> <br />FLOODING PROCESSESAND ENVIRONMENTS ON ALLUVIAL FANS <br /> <br />31 <br /> <br /> <br />-"''''~- <br />'-"""'1 <br /> <br />f' <br />r. <br /> <br />)//8/ <br /> <br />" <br /> <br />" <br /> <br />" <br />',' <br />, <br />" <br />" <br />,. <br />. <br />" <br />IJ zcPJ <br />J!?haffey <br /> <br />~; <br />I <br />~ <br />~ <br />~ <br />~ <br />~ <br />~ <br /> <br />"- <br />~..'" <br />-:;' <br /> <br />" <br />" <br />" <br /> <br />'" <br /> <br />25 <br /> <br />~ <br />\ /" <br /> <br />.. <br /> <br />- <br /> <br />FIGURE 2-2 Where fans converge from multiple source valleys, the fan shape may nol be obvious. The coalescing <br />Day and Dccr Canyon fans on a bajada along the southem slopes of the San Gabriel Mountains near Cucamonga, <br />California, flooded in January 1969. SOURCE: Singer and Price (1971). <br />