Personal Narrative Of Travels To The Equinoctial Regions Of America During The Years 1799-1804 - Volume 1 - By Alexander Von Humboldt And Aime Bonpland.
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We Might Say, That These Fragments Had Not Time
To Enter Into Complete Solution In The Liquified Mass.
They contain
vitreous feldspar, and augite, and are the same as the celebrated
columnar porphyries of the island of
Panaria, which, without having
been part of a current of lava, seem raised up in the form of
hillocks, like many of the porphyries in Auvergne, in the Euganean
mountains, and in the Cordilleras of the Andes.
The objections against the volcanic origin of obsidians, founded on
their speedy loss of colour, and their swelling by a slow fire,
have been shaken by the ingenious experiments of Sir James Hall.
These experiments prove, that a stone which is fusible only at
thirty-eight degrees of Wedgwood's pyrometer, yields a glass that
softens at fourteen degrees; and that this glass, melted again and
unvitrified (glastenized), is fusible again only at thirty-five
degrees of the same pyrometer. I applied the blowpipe to some black
pumice-stone from the volcano of the isle of Bourbon, which, on the
slightest contact with the flame, whitened and melted into an
enamel.
But whether obsidians be primitive rocks which have undergone the
action of volcanic fire, or lavas repeatedly melted within the
crater, the origin of the pumice-stones contained in the obsidian
of the Peak of Teneriffe is not less problematic. This subject is
the more worthy of being investigated, since it is generally
interesting to the geology of volcanoes; and since that excellent
mineralogist, M. Fleuriau de Bellevue, after having examined Italy
and the adjacent islands with great attention, affirms, that it is
highly improbable that pumice-stone owes its origin to the swelling
of obsidian.
The experiments of M. da Camara, and those I made in 1802, tend to
support the opinion, that the pumice-stones adherent to the
obsidians of the Peak of Teneriffe do not unite to them
accidentally, but are produced by the expansion of an elastic
fluid, which is disengaged from the compact vitreous matter. This
idea had for a long time occupied the mind of a person highly
distinguished for his talents and reputation at Quito, who,
unacquainted with the labours of the mineralogists of Europe, had
devoted himself to researches on the volcanoes of his country. Don
Juan de Larea, one of those men lately sacrificed to the fury of
faction, had been struck with the phenomena exhibited by obsidians
exposed to a white heat. He had thought, that, wherever volcanoes
act in the centre of a country covered with porphyry with base of
obsidian, the elastic fluids must cause a swelling of the liquified
mass, and perform an important part in the earthquakes preceding
eruptions. Without adopting an opinion, which seems somewhat bold,
I made, in concert with M. Larea, a series of experiments on the
tumefaction of the volcanic vitreous substances at Teneriffe, and
on those which are found at Quinche, in the kingdom of Quito. To
judge of the augmentation of their bulk, we measured pieces exposed
to a forge-fire of moderate heat, by the water they displaced from
a cylindric glass, enveloping the spongy mass with a thin coating
of wax.
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