Top 
References 
Meandering rivers leave behind amalgamated point bar deposits, such as this 100km reach of the Mississippi River, USA
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.
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.
It is a big mistake to think that rain falls rarely in drylands - sometimes rain is so intense it causes immense damage. The key point is that evaporation rates far exceed rainfall, so the flow in rivers DECREASES downstream.
River planform as seen from satellite or plane can be deceptive and unreliable - human interference goes back many centuries and may create features not present in the rock record
Antidune sedimentary structures can be mistaken for hummocky cross-stratification (HCS) - doing this would lead to interpreting fluvial deposits as marine !!
