Fig. 10.33. Example of a simulated cross section of alluvial stratigraphy constructed using the numerical model of Bridge and Leeder (1979).
The cross section is 10 km wide. Channel�belt aggradation rate is 20 m/ka. Channel width is 600 m and depth is 3m
0
&
"
s·
�· �
[
*.
0
�
2:
[ e!..
>
&
�·
a
@
�
�
�