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<br />~ <br />...& <br />...... <br /> <br /> 100 <br /> 90 <br /> 80 <br />1: 70 <br />0> <br />~ 60 <br />~ <br />as 50 <br />c <br />u: <br />i 40 <br />a. 30 <br /> 20 <br /> 10 <br /> <br />::a <br />~ <br />c: <br />a <br />CD <br />n <br />o <br />::J <br />CII <br />c: <br />6f <br />~ <br />Qo <br />rn <br />~ <br />S' <br />CD <br />CD <br />.. <br />,!It <br />5' <br />fl <br /> <br />~~ I IIII I I I <br /> r <br />q <br /> \ -+-- MiII3 <br />~ <br /> --*""" M-W4 <br /> ~ -.- M-lI#6 <br /> \ ---- M-l#7 <br /> , -+- M-lII8 <br /> \ -.6.- Average 3,4,6 <br /> \ --+- Average 7,8 <br /> \ <br /> It <br /> ~ <br /> i~ <br /> L <br /> \ t\ <br /> ~~ ~ I\. --.- --.0-_"'- -..------ - <br /> ~~ <br /> ~~ <br /> <br />10 3 1 3 <br />Grain Size in Millimeters <br /> <br />I BCllDERS I CCE8lES ~ c 1~va.1 F I \IF I \Ie I c I ~ I F I \IF I <br /> <br />o <br />1000 <br /> <br />3 <br /> <br />100 <br /> <br />3 <br /> <br />0.1 <br /> <br />3 <br /> <br />0.01 <br /> <br />SILTora..AY <br /> <br />Figure 3.7. Grain size distribution plots for various bar surface and subsurface sediments In the Mathers Hole study reach, RM 17.5. <br />