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1 blocks not present in 1859 1861 1866 1869 1872; present in 1860
But perhaps it would be safer to allow two or three inches per century, and this would reduce the number of years to one hundred and fifty or one hundred million years.

in all probability a far 1859
it is not improbable that a 1860

years! 1859 1860 1861
years! Now turn to our richest geological museums, and what a paltry display we behold! 1866

numbers of our 1859 1860 1861 1866 1869
very many 1872

of one inch per century for the whole length would be
a sufficient
an ample
allowance. At this rate, on the above data, the denudation of the Weald must have required 306,662,400 years; or say three hundred million years.
The action of fresh water on the gently inclined Wealden district, when upraised, could hardly have been great, but it would somewhat reduce the above estimate. On the other hand, during oscillations of level, which we know this area has undergone, the surface may have existed for millions of years as land, and thus have escaped the action of the sea: when deeply submerged for perhaps equally long periods, it would, likewise, have escaped the action of the coast-waves. So that in all probability a far longer period than 300 million years has elapsed since the latter part of the Secondary period.
I have made these few remarks because it is highly important for us to gain some notion, however
imper- fect,
imperfect,
of the lapse of
time.
years.
During each
of these
of these
year,
years,
over the whole world, the land and the water
have
has
been peopled by hosts of living forms. What an infinite number of generations, which the mind cannot grasp, must have succeeded each other in the long roll of years! Now turn to our richest geological museums, and what a paltry display we behold!
On
On
the
the
Poorness
poorness
of
of
our
our
Palæontological
Palæontological
Collections .
Collections .
collections .—
That our
palæontological
palæontological
collections are
very
very
imperfect
imperfect,
is admitted by every one. The remark of that admirable palæontologist,
the late
the late
Edward Forbes, should
never
not
be forgotten, namely, that numbers of our fossil species are known and named from single and often broken specimens, or from a few specimens collected on some one spot. Only a small portion of the surface of the earth has been geologically explored, and no part with