This is a bump for lunkhead.
I will try a quick summary.
In any one place in the world there may be a series of strata. These have particular kinds of rocks one a top the other.
Sometimes the layers are obviously "screwed up" as when a mountain range has risen and the layers are twisted and bent. However, even then the relationships may be intact. That is which layer is next to what layer.
When comparing layers from different places sometimes you find that a few of the layers from one place match up with layers from another. The nature of the rocks, the relationship between them, the kind of fossils in them and perhaps even some degree of thickness are the same. However, this new place may add (above or below) additional layers not found somewhere else.
If site after site (many 1,000's) are examined it becomes possible to find a clear pattern. Even without one place with all the layers it is clear what the sum of all strata would look like. (though there are places with all or a lot of it in one place).
All of this was done around two centuries ago.
Much, much later the technology became available to give absolute, rather than relative, dates to the layers.
Lo and behold, now pay attention, this part is important:
The dates corresponded to the already determined order from deep down in the geologic column being old to high up being newer.
If anyone can doubt the validity of the overall result after that they have some serious information processing deficits.
Now the geolgists can please correct any big booboos I have made.
[This message has been edited by NosyNed, 02-13-2004]