OK, I've heard some creationists here are quite unfamiliar with a standard Geology concept called stratigraphic correlation.
So this is an attempt to explain it.
Stratigraphic correlation is how we build a complete picture of rocks based on a sample of the various portions of the rocks.
We want to find out how far a rock layer extends in an area. We also may want to know how the environment of deposition changed across an area. If you are standing on a beach you are looking out at the ocean which is depositing sediments in one say, while the dunes you are standing on represent a completely different environment of deposition and some erosion.
When we look at rock cores or exposed "cuts" where rock layers are exposed in a layer we describe the rock and the particle size, and any fossils in them and their general appearance (color, features, etc.)
Then we may travel for miles in some other direction and find another exposed "cut" or look at some different rock core and describe the rock layers in it.
When we set these two descriptions side by side we can find commonalities and some cases where things are missing.
Look at this cartoon. It represents the descriptions from two exposures of several layers of rocks separated by 10 miles:
What you see are some layers, like C and F which look almost exactly alike. They have the same type of fossils and the same type of particle sizes (the little dashes indicate "clay", very fine particles). We assume C and F are correlated which means that they are likely different areas of a very large extent of the SAME environment of deposition and since this is a unique fossil we don't find earlier or much later, they represent the same time-frame as well.
Note how B and D are the same but they aren't at the same level! What this indicates is that LAYER E is MISSING in the first column and was probably eroded away at some places but not in all places. OR it was never deposited over in the area where the first set of layers was exposed. Perhaps the colum that contains E was in DEEPER WATER and the water didn't cover the land in the area of the first column so it didn't deposit any rocks.
Later we see B and D can be CORRELATED and that indicates the water covered all that area.
This is a simplistic gloss of how correlation works, but it underlies how geologists build big, detailed histories of very large areas of land.
Here's a picture of correlations that run down the entire WEST SIDE of the state of Kansas (note the little picture in the upper right corner that shows where the columns are from)
I know this is really hard to see (HERE's a larger version), but what it represents is the real power of being able to CORRELATE across big distances. It requires some advanced knowledge of geology, mineralogy, stratigraphy, and environmental depositional systems.
Ultimately you can generate some really nice pictures in 3 dimensions. Here's something called a FENCE DIAGRAM that represents correlation in 2 dimensions (X and Y) and in the 3rd dimension (the rock layers). The little "poles" in the fence diagram are the rock cores that were described and correlated. Attempts were made to interpolate the data between these datapoints.
For more information on STRATIGRAPHY and CORRELATION, check HERE or HERE.
(Resource 1)
(Resource 2)
So this is an attempt to explain it.
Stratigraphic correlation is how we build a complete picture of rocks based on a sample of the various portions of the rocks.
We want to find out how far a rock layer extends in an area. We also may want to know how the environment of deposition changed across an area. If you are standing on a beach you are looking out at the ocean which is depositing sediments in one say, while the dunes you are standing on represent a completely different environment of deposition and some erosion.
When we look at rock cores or exposed "cuts" where rock layers are exposed in a layer we describe the rock and the particle size, and any fossils in them and their general appearance (color, features, etc.)
Then we may travel for miles in some other direction and find another exposed "cut" or look at some different rock core and describe the rock layers in it.
When we set these two descriptions side by side we can find commonalities and some cases where things are missing.
Look at this cartoon. It represents the descriptions from two exposures of several layers of rocks separated by 10 miles:

What you see are some layers, like C and F which look almost exactly alike. They have the same type of fossils and the same type of particle sizes (the little dashes indicate "clay", very fine particles). We assume C and F are correlated which means that they are likely different areas of a very large extent of the SAME environment of deposition and since this is a unique fossil we don't find earlier or much later, they represent the same time-frame as well.
Note how B and D are the same but they aren't at the same level! What this indicates is that LAYER E is MISSING in the first column and was probably eroded away at some places but not in all places. OR it was never deposited over in the area where the first set of layers was exposed. Perhaps the colum that contains E was in DEEPER WATER and the water didn't cover the land in the area of the first column so it didn't deposit any rocks.
Later we see B and D can be CORRELATED and that indicates the water covered all that area.
This is a simplistic gloss of how correlation works, but it underlies how geologists build big, detailed histories of very large areas of land.
Here's a picture of correlations that run down the entire WEST SIDE of the state of Kansas (note the little picture in the upper right corner that shows where the columns are from)

I know this is really hard to see (HERE's a larger version), but what it represents is the real power of being able to CORRELATE across big distances. It requires some advanced knowledge of geology, mineralogy, stratigraphy, and environmental depositional systems.
Ultimately you can generate some really nice pictures in 3 dimensions. Here's something called a FENCE DIAGRAM that represents correlation in 2 dimensions (X and Y) and in the 3rd dimension (the rock layers). The little "poles" in the fence diagram are the rock cores that were described and correlated. Attempts were made to interpolate the data between these datapoints.

For more information on STRATIGRAPHY and CORRELATION, check HERE or HERE.
(Resource 1)
(Resource 2)