" ("New Amer. Cyclop.," art. Coal.)
DESTRUCTION OF POMPEII
The history of the growth of the European Continent, as recounted by
Professor Geikie, gives an instructive illustration of the relations of
geology to geography. The earliest European land, he says, appears to
have existed in the north and north-west, comprising Scandinavia,
Finland, and the northwest of the British area, and to have extended
thence through boreal and arctic latitudes into North America. Of the
height and mass of this primeval land some idea may be formed by
considering the enormous bulk of the material derived from its
disintegration. In the Silurian formations of the British Islands alone
there is a mass of rock, worn from the land, which would form a
mountain-chain extending from Marseilles to the North Cape (1800 miles),
with a mean breadth of over thirty-three miles, and an average height of
16,000 feet.
As the great continent which stood where the Atlantic Ocean now is wore
away, the continents of America and Europe were formed; and there seems
to have been from remote times a continuous rising, still going on, of
the new lands, and a sinking of the old ones.
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