I should clarify what I mean when I say crawl before we walk.
I was wondering if you could begin describing some processes and rules that match your observations of certain rock types. In your own words propose a theory on how some rock types formed, such as sediments. Ie. Breccia is created in high energy fluvial environments, it has large, sharp edged clasts surrounded by a matrix. Limestone is created from....Sandstones are created in...
It may get bogged down so if you wish you can describe how you think things are created when you describe IRH's data.
I would like your view on some principles. These principles seem important: The principle of superposition, original horizontality, original lateral continuity.
Other principles you can define would be nice as well.
This way, we can work from a common base of knowledge and create a rational environment. If I tell you Breccia is this and then tell you that a certain mudstone is formed in the same depostional environment, you can then question my position or sanity.
If I subsribe to the principle of superposition, but then say that the younger strata is on the bottom of the undisturbed sequence, you can call me on it.