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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The Zone Of Perpetual Snows Also
Forms A Fourth Of The Height Of The Mountain; And The Base Of This
Zone, Seen On The Coast Of The Pacific, Fills An Extent Of 3437
Toises (6700 Metres).
But though Chimborazo is two-thirds higher
than the peak, we do not see it, on account of the curve of the
globe, at more than 38 miles and a third farther distant.
The
radiant brilliancy of its snows, when, at the port of Guayaquil, at
the close of the rainy season, Chimborazo is discerned on the
horizon, may lead us to suppose, that it must be seen at a very
great distance in the South Sea. Pilots highly worthy of credit
have assured me, that they have seen it from the rock of Muerto, to
the south west of the isle of Puna, at a distance of 47 leagues.
Whenever it has been seen at a greater distance, the observers,
uncertain of their longitude, have not been in a situation to
furnish precise data.
Aerial light, projected on mountains, increases the visibility of
those which are seen positively; its power diminishes, on the
contrary, the visibility of objects which, like the peak of
Teneriffe and that of the Azores, detach themselves in a brown
tint. Bouguer, relying on theoretical considerations, was of
opinion that, according to the constitution of our atmosphere,
mountains seen negatively cannot be perceived at distances
exceeding 35 leagues. It is important here to observe, that these
calculations are contrary to experience. The peak of Teneriffe has
been often seen at the distance of 36, 38, and even at 40 leagues.
Moreover, in the vicinity of the Sandwich Islands, the summit of
Mowna-Roa, at a season when it was without snows, has been seen on
the skirt of the horizon, at the distance of 53 leagues. This is
the most striking example we have hitherto known of the visibility
of a mountain; and it is the more remarkable, that an object seen
negatively furnishes this example.
The volcanoes of Teneriffe, and of the Azores, the Sierra Nevada of
Santa Martha, the peak of Orizaba, the Silla of Caracas, Mowna-Roa,
and Mount St. Elias, insulated in the vast extent of the seas, or
placed on the coasts of continents, serve as sea-marks to direct
the pilot, when he has no means of determining the position of the
vessel by the observation of the stars; everything which has a
relation to the visibility of these natural seamarks, is
interesting to the safety of navigation.
CHAPTER 1.2.
STAY AT TENERIFE.
JOURNEY FROM SANTA CRUZ TO OROTAVA.
EXCURSION TO THE SUMMIT OF THE PEAK OF TEYDE.
From the time of our departure from Graciosa, the horizon continued
so hazy, that, notwithstanding the considerable height of the
mountains of Canary,* (* Isla de la Gran Canaria.) we did not
discover that island till the evening of the 18th of June. It is
the granary of the archipelago of the Fortunate Islands; and, what
is very remarkable in a region situated beyond the limits of the
tropics, we were assured, that in some districts, there are two
wheat harvests in the year; one in February, and the other in June.
Canary has never been visited by a learned mineralogist; yet this
island is so much the more worthy of observation, as the
physiognomy of its mountains, disposed in parallel chains, appeared
to me to differ entirely from that of the summits of Lancerota and
Teneriffe.
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