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Why spend so long trying to model channels as ribbons when the channel is mud-filled and the sand is elsewhere?
Version 4 is now offline - permanently !! 
All material is now in Version 6 ...
Better ways to select modern analogues, using climate and geomorphological relationships ...
Smart new Executive Summary now live ...
New website of interest: SEPM Sequence Stratigraphy (STRATA) site by Chris Kendall ...
Debris-flows in action, if you want a thrill ...…
River to Rock Record conference, Aberdeen
Sedimentary Processes section removed, material placed elsewhere (version 6c)
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.
Look out for the new Topic Thread navigation (top left and top right) to guide you through longer sections.
Look in Reservoirs and Analogues section for a guide to conceptual and numerical reservoir modelling.
Tell us what you think, share ideas or ask questions, through the Feedback section.
Rivers will be braided in plan form if the banks are not made resistant in some way.
Q: When might an incised valley not be an incised valley even though it cuts down 60m into the underlying succession?
A: When it is a confluence scour !!
Antidune sedimentary structures can be mistaken for hummocky cross-stratification (HCS) - doing this would lead to interpreting fluvial deposits as marine !!
