Natural history -- Nicaragua; Nicaragua -- Description and travel
I have quoted this graphic account of the great volcanic eruption
of St. Vincent in 1812 from Canon Kingsley's delightful work to
impress on my readers, in more eloquent language than I can
command, the fact of great explosions having taken place in recent
times similar in character, though much inferior in extent and
force, to that by which I believe the great basin of the Lake of
Masaya and similar basins in the same and adjoining Pacific
provinces have been blasted out. I do not shut my eyes to the fact
that great as was the force in operation in 1812 at St. Vincent,
that necessary to excavate the great chasm at Masaya was
incomparably greater. No one is more disinclined than I am to
invoke the aid of greater natural forces in former times than are
now in existence. But I believe there is good reason to infer that
at the close of the glacial period volcanic energy was much more
intense than now. So strained is the earth's crust at some parts
that it is surmised that even a great difference in the pressure of
the atmosphere such as occurs during a cyclone, may be sufficient
to bring on an earthquake or a volcanic eruption already imminent.
Whether this be so or not, there can be no doubt that at the
melting away of the ice of the glacial period there was an enormous
change in the strains on the earth's crust. Ice that had been piled
up mountains high at the poles and along the chain of the Andes all
through tropical America melted away and ran down to the ocean
beds. This great transference of weight could not have been
accomplished without many rendings of the earth's crust and many
outpourings of lava and volcanic outbursts. Let us reflect, too,
that not only was an enormous mass of matter, before lying over the
poles, removed nearer to the equator, and many mountain-chains
relieved of the ice of thousands and tens of thousands of years,
but that there must have been an actual change in the earth's
centre of gravity. All our experience shows that the ice was more
developed on some meridians than others; probably nowhere in the
whole world did it lie so thick as along the American continents;
and everywhere it must have been greater over the land than over
the sea. When it assumed its liquid form, and arranged itself
freely according to its specific gravity, the centre of gravity of
the earth must have been effectively changed. All who have studied
the present statical condition of the earth's crust will readily
admit that such a change might produce greater volcanic outbursts
than any known to history.
Public-domain text, read in full here on John Shaqi.
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