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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For In All Volcanoes, Even When
There Are Lateral Eruptions, The Ashes And The Rapilli Issue
Conjointly With The Vapours Only From The Opening At The Summit Of
The Mountain.
Now, at Teneriffe, the black rapilli extend from the
foot of the Peak to the sea-shore; while the
White ashes, which are
only pumice ground to powder, and among which I have discovered,
with a lens, fragments of vitreous feldspar and pyroxene,
exclusively occupy the region next to the Peak. This peculiar
distribution seems to confirm the observations made long ago at
Vesuvius, that the white ashes are thrown out last, and indicate
the end of the eruption. In proportion as the elasticity of the
vapours diminishes, the matter is thrown to a less distance; and
the black rapilli, which issue first, when the lava has ceased
running, must necessarily reach farther than the white rapilli. The
latter appear to have been exposed to the action of a more intense
fire.
I have now examined the exterior structure of the Peak, and the
composition of its volcanic productions, from the region of the
coast to the top of the Piton: - I have endeavoured to render these
researches interesting, by comparing the phenomena of the volcano
of Teneriffe with those that are observed in other regions, the
soil of which is equally undermined by subterranean fires. This
mode of viewing Nature in the universality of her relations is no
doubt adverse to the rapidity desirable in an itinerary; but it
appears to me that, in a narrative, the principal end of which is
the progress of physical knowledge, every other consideration ought
to be subservient to those of instruction and utility.
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