The Life of Sir Humphry Davy, Bart. LL.D., Volume 2 (of 2)Paris, John Ayrton
History
The Life of Sir Humphry Davy, Bart. LL.D., Volume 2 (of 2)
Paris, John Ayrton
Chemists -- England -- Biography; Davy, Humphry, Sir, 1778-1829
"When these revolutions became less frequent, and the globe
became still more cooled, and the inequalities of its temperature
preserved by the mountain chains, more perfect animals became
its inhabitants, many of which, such as the mammoth, megalonix,
megatherium, and gigantic hyena, are now extinct. At this period,
the temperature of the ocean seems to have been not much higher
than it is at present, and the changes produced by occasional
eruptions of it have left no consolidated rocks. Yet one of
these eruptions appears to have been of great extent and of some
duration, and seems to have been the cause of those immense
quantities of water-worn stones, gravel, and sand, which are
usually called _diluvian_ remains;--and it is probable that this
effect was connected with the elevation of a new continent in the
southern hemisphere by volcanic fire. When the system of things
became so permanent, that the tremendous revolutions depending
upon the destruction of the equilibrium between the heating and
cooling agencies were no longer to be dreaded, the creation of man
took place; and since that period there has been little alteration
in the physical circumstances of our globe. Volcanoes sometimes
occasion the rise of new islands, portions of the old continents
are constantly washed by rivers into the sea, but these changes are
too insignificant to affect the destinies of man, or the nature of
the physical circumstances of things. On the hypothesis that I have
adopted, however, it must be remembered, that the present surface
of the globe is merely a thin crust surrounding a nucleus of fluid
ignited matter; and consequently, we can hardly be considered as
actually safe from the danger of a catastrophe by fire.
* * * * *
"I beg you to consider the views I have been developing as
merely hypothetical, one of the many resting-places that may be
taken by the imagination in considering this subject. There are,
however, distinct facts in favour of the idea, that the interior
of the globe has a higher temperature than the surface; the heat
increasing in mines the deeper we penetrate, and the number of warm
sources which rise from great depths, in almost all countries,
are certainly favourable to the idea. The opinion, that volcanoes
are owing to this general and simple cause, is, I think, likewise
more agreeable to the analogies of things, than to suppose them
dependent upon partial chemical changes, such as the action of air
and water upon the combustible bases of the earths and alkalies,
though it is extremely probable that these substances may exist
beneath the surface, and may occasion some results of volcanic
fire;--and on this subject my notion may perhaps be the more
trusted, as for a long while I thought volcanic eruptions were
owing to chemical agencies of the newly discovered metals of the
earths and alkalies, and I made many and some dangerous experiments
in the hope of confirming this notion, but in vain.
Public-domain text, read in full here on John Shaqi.
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