Comparison with 1872 |
|
which I wrote in 1859,
about the existence of living beings long before the Cambrian period, and which about the existence of living beings long before the Cambrian period, and which 1872 |
and which 1866 |
about the vast periods which had probably elapsed before the Cambrian system, 1869 |
are almost the same with those used
by Sir W.
Logan, Logan, 1866 1872 | Logan. 1869 |
have
proved proved 1872 | come 1866 | proved 1869 |
true. true. 1866 1872 | true. 1869 |
Nevertheless, Nevertheless, 1872 |
Notwithstanding these several facts, 1866 |
Nevertheless 1869 |
the difficulty of assigning any good cause
for the absence
...OMIT 1872 |
beneath the Silurian formations 1866 |
beneath the Upper Cambrian formations 1869 |
of vast piles of strata rich in fossils
beneath the Cambrian system is beneath the Cambrian system is 1872 |
is 1866 1869 |
very great. If these
most ancient beds had
been wholly
worn away by denudation, or obliterated
by metamorphic action, we ought to find
only small remnants of the formations next succeeding them in age, and these ought to be very generally
in a metamorphosed
condition. But the descriptions which we now
possess of the Silurian deposits over immense territories in Russia and in North America, do not support the view, that the older a formation is, the more
invariably it invariably it 1872 | it 1859 1860 1861 1866 1869 |
has
suffered extreme suffered extreme 1872 |
suffered the extremity of 1859 |
always suffered the extremity of 1860 1861 1866 |
invariably suffered extreme 1869 |
denudation and metamorphism. |
|
The case at present must remain inexplicable; and may be truly urged as a valid argument against the views here entertained. To show that it may hereafter receive some explanation, I will give the following hypothesis. From the nature of the organic remains,
which do not appear to have inhabited profound depths, in the several formations of Europe and of the United States; and from the amount of sediment, miles in thickness, of which the formations are composed, we may infer that from first to last large islands or tracts of land, whence the sediment was derived, occurred in the neighbourhood of the existing
continents of Europe and North America. This same view has since been maintained by Agassiz and others. But we do not know what was the state of things in the intervals between the successive
formations; whether Europe and the United States during these intervals existed as dry land, or as a submarine surface near land, on which sediment
|
which I wrote in 1859,
about the vast periods which had probably elapsed before the Cambrian system, about the vast periods which had probably elapsed before the Cambrian system, 1869 |
and which 1866 |
about the existence of living beings long before the Cambrian period, and which 1872 |
are almost the same with those
since used since used 1869 1872 | used 1866 |
by Sir W.
Logan. Logan. 1869 | Logan, 1866 1872 |
..
....... 1869 | come 1866 | proved 1872 |
....... 1869 | true. 1866 1872 |
Nevertheless Nevertheless 1869 |
Notwithstanding these several facts, 1866 |
Nevertheless, 1872 |
the difficulty of assigning any good
reason reason 1869 1872 | cause 1866 |
for the absence
beneath the Upper Cambrian formations beneath the Upper Cambrian formations 1869 |
beneath the Silurian formations 1866 |
OMIT 1872 |
of vast piles of strata rich in fossils
is is 1866 1869 |
beneath the Cambrian system is 1872 |
very great.
It does not seem probable that the It does not seem probable that the 1869 1872 |
If these 1859 1860 1861 |
If the 1866 |
most ancient beds
have have 1869 1872 | had 1859 1860 1861 1866 |
been
quite quite 1869 1872 | wholly 1859 1860 1861 | generally 1866 |
worn away by denudation, or
that their fossils have been wholly obliterated that their fossils have been wholly obliterated 1869 1872 |
obliterated 1859 1860 1861 |
if their fossils had been wholly obliterated 1866 |
by metamorphic action,
for if this had been the case we should have found for if this had been the case we should have found 1869 1872 |
we ought to find 1859 1860 1861 |
we ought to have found 1866 |
only small remnants of the formations next succeeding them in age, and these
would always have existed would always have existed 1869 1872 |
ought to be very generally 1859 1860 1861 |
ought to have existed almost always 1866 |
in a
partially metamorphosed partially metamorphosed 1869 1872 | metamorphosed 1859 1860 1861 1866 |
condition. But the descriptions which we
....... 1869 1872 | now 1859 1860 1861 1866 |
possess of the Silurian deposits over immense territories in Russia and in North America, do not support the view, that the older a formation is, the more
it it 1859 1860 1861 1866 1869 | invariably it 1872 |
has
invariably suffered extreme invariably suffered extreme 1869 |
suffered the extremity of 1859 |
always suffered the extremity of 1860 1861 1866 |
suffered extreme 1872 |
denudation and metamorphism. |
|
The case at present must remain inexplicable; and may be truly urged as a valid argument against the views here entertained. To show that it may hereafter receive some explanation, I will give the following hypothesis. From the nature of the organic
remains remains 1860 1861 1866 1869 1872 | remains, 1859 |
which do not appear to have inhabited profound depths, in the several formations of Europe and of the United States; and from the amount of sediment, miles in thickness, of which the formations are composed, we may infer that from first to last large islands or tracts of land, whence the sediment was derived, occurred in the neighbourhood of the
now existing now existing 1869 1872 | existing 1859 1860 1861 1866 |
continents of Europe and North America. ↑1 blocks not present in 1859 1860 1861 1866 1869; present in 1872 | This same view has since been maintained by Agassiz and others.
|
But we do not know what was the state of things in the intervals between the
several successive several successive 1866 1869 1872 | successive 1859 1860 1861 |
formations; whether Europe and the United States during these intervals existed as dry land, or as a submarine surface near land, on which sediment
|