| completely denuded of all overlying strata?  That such extensive areas do exist cannot be 
 doubted: the granitic region of Parime is described by Humboldt as being at least nineteen times as large as Switzerland.  South of the 
 Amazon,| doubted: 1861 1866 1869 |  | doubted; 1872 | 
Boué colours an area composed of 
 ..| Amazon, 1866 1869 1872 |  | Amazon 1861 | 
rocks 
 of this nature as| ..... 1866 1869 1872 |  | such 1861 | 
equal to that of Spain, France, Italy, part of Germany, and the British Islands, all conjoined.  This region has not been carefully explored, but from the concurrent testimony of travellers, the granitic area 
 must be| of this nature as 1866 1869 1872 |  | as 1861 | 
very 
 large:| must be 1861 1866 |  | is 1869 1872 | 
thus, Von Eschwege gives a detailed section of these rocks, stretching from Rio de Janeiro for 260 geographical miles inland in a straight line; and I travelled for 150 miles in another 
 direction| large: 1861 1866 1869 |  | large; 1872 | 
and saw nothing but granitic rocks.  Numerous specimens, collected along the whole coast from near Rio Janeiro to the mouth of the Plata, a distance of 1100 geographical miles, were 
 examined by| direction 1861 1866 |  | direction, 1869 1872 | 
me, and they all belonged to this class.  Inland, along the whole northern bank of the Plata I saw, besides modern tertiary beds, only one small patch of slightly metamorphosed rock, which alone could have formed a part of the original capping of the granitic series.  Turning to a well-known region, namely, to the United States and Canada, as shown in Professor H. D. Rogers's beautiful map, I have estimated the areas by cutting out and weighing the paper, and I find that the metamorphic (excluding 
 "the| examined by 1866 1869 1872 |  | shown 1861 | 
semi-metamorphic")| "the 1866 1869 1872 |  | "the 1861 | 
and granitic rocks exceed, in the proportion of 19 to 
 12.5,| semi-metamorphic") 1866 1869 1872 |  | semi-metamorphic") 1861 | 
the whole 
 of the newer| 12.5, 1866 1869 |  | 12.5, not only the true coal measures, well known to be here developed in extraordinary force, but likewise the Umbral series, which together compose 1861 |  | 12.5, 1872 | 
Palæozoic 
 formations.| of the newer 1866 1869 1872 |  | newer 1861 | 
In many regions the metamorphic and granitic 
 rocks| formations. 1866 1869 1872 |  | formation. 1861 | 
would be 
 seen to be much more widely extended, if| rocks 1866 1869 1872 |  | areas 1861 | 
all the sedimentary beds 
 were removed which| seen to be much more widely extended, if 1866 1869 |  | greatly increased in size, if we could remove 1861 |  | found much more widely extended than they appear to be, if 1872 | 
rest unconformably on them, and which 
 ...| were removed which 1866 1869 1872 |  | which 1861 | 
could not have formed part of the original mantle under which 
 they| OMIT 1866 1869 1872 |  | at the line of junction have not been metamorphosed, showing that they 1861 | 
..| they 1866 1869 1872 |  | the 1861 | 
were crystallized.  Hence it is probable that in some parts of the world whole 
 formations,| ..... 1866 1869 1872 |  | granitic rocks 1861 | 
marking at least sub-stages in the several successive geological epochs,| formations, 1861 1866 |  | formations 1869 1872 | 
| marking at least sub-stages in the several successive geological epochs, 1861 1866 |  | OMIT 1869 1872 | 
 |