DSC07981 (2)

7extural diuersity of Jha ial deposits

139

ydgrodzie and

■eactivation of d sandy dusts ication is less

characteristic with defined e peak flows n above Iow was covered

1    the upper e Iow JeveL !ain oniy at sst deposits

;and which >sits which be channel and less are much

ished: the

2    to —0.6 deposits;

0) being

—6.0 to are less

⁶¹

*1

2 i

PLI

V

*1    b

ible to am of ncient der to

great

riable

. The d by żates very arne

the

Fig- 14. Comparison of grain size properties of diflerent types of (luvial deposits — standard

deviation <7, versus mean diameter Mz

ą _ channe! deposits (abbreviations are as for Table I); B — overbank deposits; C — channel fili deposits: u — accumulated by running water. b — sedimentation from suspension; D — alluvial fan deposits: a — coarse deposits. fr, — medium-grained deposits. f, — fine deposits; E — modern deposits: a — lateral gravel bars deposits. b — sandy-gravdly bar deposits, c — high discharge-forroed deposits in the channel and on the floodplain