Laws of relative dating geology updating of new row is not allowed in after trigger

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[SE] The principle of cross-cutting relationships states that any geological feature that cuts across, or disrupts another feature must be younger than the feature that is disrupted.

But the faults do not appear to continue into the coal seam, and they certainly do not continue into the upper sandstone.

The simplest and most intuitive way of dating geological features is to look at the relationships between them.

There are a few simple rules for doing this, some of which we’ve already looked at in Chapter 6.

The boundary between the two represents a time gap of nearly 300 million years.

[SE ]Figure 8.9 The four types of unconformities: (a) a nonconformity between non-sedimentary rock and sedimentary rock, (b) an angular unconformity, (c) a disconformity between layers of sedimentary rock, where the older rock has been eroded but not tilted, and (d) a paraconformity where there is a long period (millions of years) of non-deposition between two parallel layers.

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