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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I
Am Rather Inclined To Think, That The Chayma Indians Of Cumana Did
Not See The Same Bolides As The
Portuguese in Brazil and the
missionaries in Labrador; but at the same time it cannot be doubted
(and this fact
Appears to me very remarkable) that in the New
World, between the meridians of 46 and 82 degrees, between the
equator and 64 degrees north, at the same hour, an immense number
of bolides and falling-stars were perceived; and that those meteors
had everywhere the same brilliancy, throughout a space of 921,000
square leagues.
Astronomers who have lately been directing minute attention to
falling-stars and their parallaxes, consider them as meteors
belonging to the farthest limits of our atmosphere, between the
region of the Aurora Borealis and that of the lightest clouds.* (*
According to the observations which I made on the ridge of the
Andes, at an elevation of 2700 toises, on the moutons, or little
white fleecy clouds, it appeared to me, that their elevation is
sometimes not less than 6000 toises above the level of the coast.)
Some have been seen, which had not more than 14,000 toises, or
about five leagues of elevation. The highest do not appear to
exceed thirty leagues. They are often more than a hundred feet in
diameter: and their swiftness is such, that they dart in a few
seconds through a space of two leagues. Of some which have been
measured, the direction was almost perpendicularly upward, or
forming an angle of 50 degrees with the vertical line. This
extremely remarkable circumstance has led to the conclusion, that
falling-stars are not aerolites which, after having hovered a long
time in space, unite on accidentally entering into our atmosphere,
and fall towards the earth.* (* M. Chladni, who at first considered
falling-stars to be aerolites, subsequently abandoned that idea.)
Whatever may be the origin of these luminous meteors, it is
difficult to conceive an instantaneous inflammation taking place in
a region where there is less air than in the vacuum of our
air-pumps; and where (at the height of 25,000 toises) the mercury
in the barometer would not rise to 0.012 of a line. We have
ascertained the uniform mixture of atmospheric air to be about 0.
003, only to an elevation of 3000 toises; consequently not beyond
the last stratum of fleecy clouds. It may be admitted that, in the
first revolutions of the globe, gaseous substances, which yet
remain unknown to us, have risen towards that region through which
the falling-stars pass; but accurate experiments, made upon
mixtures of gases which have not the same specific gravity, show
that there is no reason for supposing a superior stratum of the
atmosphere entirely different from the inferior strata. Gaseous
substances mingle and penetrate each other on the least movement;
and a uniformity of their mixture may have taken place in the lapse
of ages, unless we believe them to possess a repulsive action of
which there is no example in those substances we can subject to our
observations. Farther, if we admit the existence of particular
aerial fluids in the inaccessible regions of luminous meteors, of
falling-stars, bolides, and the Aurora Borealis; how can we
conceive why the whole stratum of those fluids does not at once
ignite, but that the gaseous emanations, like the clouds, occupy
only limited spaces? How can we suppose an electrical explosion
without some vapours collected together, capable of containing
unequal charges of electricity, in air, the mean temperature of
which is perhaps 25 degrees below the freezing point of the
centigrade thermometer, and the rarefaction of which is so
considerable, that the compression of the electrical shock could
scarcely disengage any heat? These difficulties would in great part
be removed, if the direction of the movement of falling-stars
allowed us to consider them as bodies with a solid nucleus, as
cosmic phenomena (belonging to space beyond the limits of our
atmosphere), and not as telluric phenomena (belonging to our planet
only).
Supposing the meteors of Cumana to have been only at the usual
height at which falling-stars in general move, the same meteors
were seen above the horizon in places more than 310 leagues distant
from each other.* (* It was this circumstance that induced Lambert
to propose the observation of falling-stars for the determination
of terrestrial longitudes. He considered them to be celestial
signals seen at great distances.) How great a disposition to
incandescence must have prevailed on the 12th November, in the
higher regions of the atmosphere, to have rendered during four
hours myriads of bolides and falling stars visible at the equator,
in Greenland, and in Germany!
M. Benzenberg observes, that the same cause which renders the
phenomenon more frequent, has also an influence on the large size
of the meteors, and the intensity of their light. In Europe, the
greatest number of falling stars are seen on those nights on which
very bright ones are mingled with very small ones. The periodical
nature of the phenomenon augments the interest it excites. There
are months in which M. Brandes has reckoned in our temperate zone
only sixty or eighty falling-stars in one night; and in other
months their number has risen to two thousand. Whenever one is
observed, which has the diameter of Sirius or of Jupiter, we are
sure of seeing the brilliant meteor succeeded by a great number of
smaller ones. If the falling stars be very numerous during one
night, it is probable that they will continue equally so during
several weeks. It would seem, that in the higher regions of the
atmosphere, near that extreme limit where the centrifugal force is
balanced by gravity, there exists at regular periods a particular
disposition for the production of bolides, falling-stars, and the
Aurora Borealis.* (* Ritter, like several others, makes a
distinction between bolides mingled with falling-stars and those
luminous meteors which, enveloped in vapour and smoke, explode with
great noise, and let fall (chiefly in the day-time) aerolites.
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