Principles of Geology: or, The Modern Changes of the Earth and its Inhabitants Considered as Illustrative of GeologyLyell, Charles, Sir
Science
Principles of Geology: or, The Modern Changes of the Earth and its Inhabitants Considered as Illustrative of Geology
Lyell, Charles, Sir
Geology
To make still more clear the supposed working of this machinery, I shall
compare it to a somewhat analogous case that might be imagined to occur
in the history of human affairs. Let the mortality of the population of
a large country represent the successive extinction of species, and the
births of new individuals the introduction of new species. While these
fluctuations are gradually taking place everywhere, suppose
commissioners to be appointed to visit each province of the country in
succession, taking an exact account of the number, names, and individual
peculiarities of all the inhabitants, and leaving in each district a
register containing a record of this information. If, after the
completion of one census, another is immediately made on the same plan,
and then another, there will, at last, be a series of statistical
documents in each province. When those belonging to any one province
are arranged in chronological order, the contents of such as stand next
to each other will differ according to the length of the intervals of
time between the taking of each census. If, for example, there are sixty
provinces, and all the registers are made in a single year, and renewed
annually, the number of births and deaths will be so small, in
proportion to the whole of the inhabitants, during the interval between
the compiling of the two consecutive documents, that the individuals
described in such documents will be nearly identical; whereas, if the
survey of each of the sixty provinces occupies all the commissioners for
a whole year, so that they are unable to revisit the same place until
the expiration of sixty years, there will then be an almost entire
discordance between the persons enumerated in two consecutive registers
in the same province. There are, undoubtedly, other causes besides the
mere quantity of time, which may augment or diminish the amount of
discrepancy. Thus, at some periods a pestilential disease may have
lessened the average duration of human life, or a variety of
circumstances may have caused the births to be unusually numerous, and
the population to multiply; or, a province may be suddenly colonized by
persons migrating from surrounding districts.
These exceptions may be compared to the accelerated rate of fluctuation
in the fauna and flora of a particular region, in which the climate and
physical geography may be undergoing an extraordinary degree of
alteration.
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