| Comparison with 1861 | 
  | 
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 it 
has 
 always suffered the extremity of | always suffered the extremity of 1860 1861 1866 |  
| suffered the extremity of 1859 |  
| invariably suffered extreme 1869 |  
| 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 existing 
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 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 was not deposited, or 
 ..| ..... 1860 1861 1866 1869 1872 |  | again 1859 |  
  
as the bed of an open and unfathomable sea.  | 
 | 
|  Looking to the existing oceans, which are thrice as extensive as the land, we see them studded with many islands; but not 
one oceanic 
island 
is as yet known to afford even a remnant of any palæozoic or secondary formation.  Hence we may perhaps infer, that during the palæozoic and secondary periods, neither continents nor continental islands existed where our oceans now extend; for had they existed 
there, 
palæozoic and secondary formations would in all probability have been accumulated from sediment derived from their wear and 
 | 
 
  
  
a 
 metamorphosed | metamorphosed 1859 1860 1861 1866 |  | partially metamorphosed 1869 1872 |  
  
condition.  But the descriptions which we 
 now | now 1859 1860 1861 1866 |  now 1869 1872 |  
  
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 
 suffered the extremity of | suffered the extremity of 1859 |  
| always suffered the extremity of 1860 1861 1866 |  
| invariably suffered extreme 1869 |  
| 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, 1859 |  | remains 1860 1861 1866 1869 1872 |  
  
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 | existing 1859 1860 1861 1866 |  | now existing 1869 1872 |  
  
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 
 successive | successive 1859 1860 1861 |  | several successive 1866 1869 1872 |  
  
formations; whether Europe and the United States during these intervals existed as dry land, or as a submarine surface near land, on which sediment was not deposited, or 
 again | again 1859 |  again 1860 1861 1866 1869 1872 |  
  
as the bed of an open and unfathomable sea.  | 
 | 
 Looking to the existing oceans, which are thrice as extensive as the land, we see them studded with many islands; but 
 not | not 1859 1860 1861 1866 1869 |  | hardly 1872 |  
  
one 
 oceanic | oceanic 1859 1860 1861 |  
| truly oceanic island (with the exception of New Zealand, if this can be called a truly oceanic 1866 1869 1872 |  
  
 island | island 1859 1860 1861 |  | island) 1866 1869 1872 |  
  
is as yet known to afford even a remnant of any palæozoic or secondary formation.  Hence we may perhaps infer, that during the palæozoic and secondary periods, neither continents nor continental islands existed where our oceans now extend; for had they 
 existed | existed 1859 1860 1861 1866 |  | existed, 1869 1872 |  
  
 there, | there, 1859 1860 1861 1866 |  there, 1869 1872 |  
  
palæozoic and secondary formations would in all probability have been accumulated from sediment derived from their wear and 
 |