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The only time such obscuring might not occur is during the very recent period when dating uncertainty is likely to be low and sample spacing may be very tight.
This non-uniformity is attributed to the anisotropic sample spacing.
The period of flame growth is prolonged with decreasing sample spacing and finally, at a small enough sample spacing, the flame distance keeps increasing until the flame disappears.
The flame distance decreases monotonically and approaches the single flame radius with increasing sample spacing also.
We believe these sample spacing can be used in other places with the same landscape forms and geology (geomorphological compartments).
This flame movement is attributed to the fuel vapor accumulation effect, which becomes more dominant with decreasing sample spacing.
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The set of all possible outcomes of an experiment is called a "sample space".
An "event" is a well-defined subset of the sample space.
In infinite sample spaces it implies, but is not implied by, equation (1).
With enough sample space, it all evens out, or in some cases, you can get even.
To describe this situation symbolically, let S denote the sample space.
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