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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This
Consideration Explains To A Certain Point, Why, Under A Perfectly
Serene Sky, The State Of The Thermometer And The Hygrometer Being
Precisely The Same In The Air Nearest The Earth, The Peak Is
Sometimes Visible, And At Other Times Invisible, To Navigators At
Equal Distances.
It is even probable, that the chance of perceiving
this volcano would not be greater, if the ashy cone, at the summit
of which is the mouth of the crater, were equal, as in Vesuvius, to
a quarter of the total height.
These ashes, being pumice-stone
crumbled into dust, do not reflect as much light as the snow of the
Andes; and they cause the mountain, seen from afar, to detach
itself not in a bright, but in a dark hue. The ashes also
contribute, if we may use the expression, to equalize the portions
of aerial light, the variable difference of which renders the
object more or less distinctly visible. Calcareous mountains,
devoid of vegetable earth, summits covered with granitic sand, the
high savannahs of the Cordilleras,* (* Los Pajonales, from paja,
straw. This is the name given to the region of the gramina, which
encircles the zone of the perpetual snows.) which are of a golden
yellow, are undoubtedly distinguished at small distances better
than objects which are seen in a negative manner; but the theory
indicates a certain limit, beyond which these last detach
themselves more distinctly from the azure vault of the sky.
The colossal summits of Quito and Peru, towering above the limit of
the perpetual snows, concentre all the peculiarities which must
render them visible at very small angles.
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