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References 
Giant fluvial fans like the Ruo Shui, western China (150km apex to toe) leave a sedimentary record indistinguishable from the river style (here braided) shaping their surface
Better ways to select modern analogues, using climate and geomorphological relationships ...
New website of interest: SEPM Sequence Stratigraphy (STRATA) site by Chris Kendall ...
Debris-flows in action, if you want a thrill ...…
Phase-1 PhD studies incorporated …
Be more precise with your climate zones …
Pictorial lithofacies atlas beginning to be populated - try desiccation cracks to see full potential
Welcome to the AUDRI website
This is the completely rewritten version of the website: new layout, all sections rewritten to improve clarity, many more images, greatly improved navigation, new content. A primary aim is to make more obvious what is inside - so each major section has a much more detailed index page, and it is easier to jump into sub-sections.
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Rivers will be braided in plan form if the banks are not made resistant in some way.
Dryland anastomosing rivers may be impossible to detect in the rock record because both channel and floodplain are uniformly fine-grained and structureless.
Models for meandering river reservoirs usually over-estimate sand-body connectivity because it is assumed such rivers produce shoe-string ribbons of sand that are well-connected along the valley - this is rarely true.
