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completely denuded of all overlying strata? That such extensive areas do exist cannot be
the granitic region of Parime is described by Humboldt as being at least nineteen times as large as Switzerland. South of the
Boué colours an area composed of
rocks
→of this nature as
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
very
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
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
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
and granitic rocks exceed, in the proportion of 19 to
→12.5,
the whole
→of the newer
Palæozoic
In many regions the metamorphic and granitic
would be
→seen to be much more widely extended, if
all the sedimentary beds
→were removed which
rest unconformably on them, and which
→OMIT
could not have formed part of the original mantle under which
were crystallized. Hence it is probable that in some parts of the world whole
→marking at least sub-stages in the several successive geological epochs,
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