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1859
1860
1861
1866
1869
1872

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1859
1860
1861
1869
1872

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

1 blocks not present in 1866 1869 1872; present in 1859 1860 1861
Now turn to our richest geological museums, and what a paltry display we behold!

numbers of our 1859 1860 1861 1866 1869
very many 1872

I believe we are continually taking a most 1859 1860 1861 1866
I believe we often take an 1869
We probably take a quite 1872

tacitly admit to ourselves 1859 1860 1861 1866 1869
assume 1872

of the lapse of
years.
time.
During each
of these
....
years,
year,
over the whole world, the land and the water
has
have
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 sufficient care, as the important discoveries made every year in Europe prove. No organism wholly soft can be preserved. Shells and bones
will
will
decay and disappear when left on the bottom of the sea, where sediment is not
accumulating.
accumulation.
I believe we are continually taking a most erroneous view, when we tacitly admit to ourselves that sediment is being deposited over nearly the whole bed of the sea, at a rate sufficiently quick to embed and preserve fossil remains. Throughout an enormously large proportion of the ocean, the bright blue tint of the water bespeaks its purity. The many cases on record of a formation conformably covered, after an
immense
enormous
interval of time, by another and later formation, without the underlying bed having suffered in the interval any wear and
tear
tear,
seem explicable only on the view of the bottom of the sea not rarely lying for ages in an unaltered condition. The remains which do become embedded, if