Personal Narrative Of Travels To The Equinoctial Regions Of America During The Years 1799-1804 - Volume 3 - By Alexander Von Humboldt And Aime Bonpland.
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Within The
Tropics Great Serenity Of The Sky And A Perfect Dissolution Of The
Vapours Diminish The Extinction Of The Light Sent Back To Us By The
Lunar Disc.
I was singularly struck during the eclipse by the want of
uniformity in the distribution of the refracted light by the
terrestrial atmosphere.
In the central region of the disc there was a
shadow like a round cloud, the movement of which was from east to
west. The part where the immersion was to take place was consequently
a few minutes prior to the immersion much more brightly illumined than
the western edges. Is this phenomenon to be attributed to an
inequality of our atmosphere; to a partial accumulation of vapour
which, by absorbing a considerable part of the solar light, inflects
less on one side the cone of the shadow of the earth? If a similar
cause, in the perigee of central eclipses, sometimes renders the disc
invisible, may it not happen also that only a small portion of the
moon is seen; a disc, irregularly formed, and of which different parts
were successively enlightened?
On the morning of the 30th of March we doubled Punta Gigantes, and
made for the Boca Chica, the present entrance of the port of
Carthagena. From thence the distance is seven or eight miles to the
anchorage near the town; and although we took a practico to pilot us,
we repeatedly touched on the sandbanks. On landing I learned, with
great satisfaction, that the expedition appointed to take the survey
of the coast under the direction of M. Fidalgo, had not yet put to
sea.
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