New lands within the Arctic circle: Narrative of the discoveries of the Austrian ship "Tegetthoff" in the years 1872-1874Payer, Julius
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New lands within the Arctic circle: Narrative of the discoveries of the Austrian ship "Tegetthoff" in the years 1872-1874
Payer, Julius
Admiral Tegetthoff (Ship); Arctic regions; Franz Josef Land (Russia) -- Discovery and exploration
Kepes, be advantageously applied to reduce the inflammation which
generally results.
10. It is remarkable that great heat as well as great cold should
generate the great evil—thirst. It is also remarkable how rapidly the
demoralisation produced by thirst extends when any one of the party
begins to show signs of suffering from it. Habit, however, enables men
to struggle against thirst more successfully than against hunger. Many
try to relieve it by using snow; which is especially pernicious when
its temperature falls considerably below the point of liquefaction.
Inflammation of the mouth and tongue, rheumatic pains in the teeth,
diarrhœa, and other mischiefs, are the consequences, whenever a party
incautiously yields to the temptation of such a momentary relief. It is
in fact a mere delusion, because it is impossible to eat as much snow—say
a cubic foot—as would be requisite to furnish an adequate amount of
water. Snow of a temperature of 37° to 50° (C.) below zero feels in the
mouth like hot iron, and does not quench, but increases thirst, by its
inflammatory action on the mucous membranes of the parts it affects.
The Eskimos prefer to endure any amount of thirst rather than eat snow,
and it is only the Tschuktschees who indulge in it as a relish with
their food, which is always eaten cold. Snow-eaters during the march
were regarded by us as weaklings, much in the same way as opium-eaters
are. Catarrhs of every kind are less frequent in Polar expeditions, and
the chills to which we are exposed by passing suddenly from the cold of
the land journey to the warmer temperature of the ship, have no evil
consequences. It deserves to be investigated whether this arises from the
difference of the amount of ozone in the atmosphere of the respective
latitudes.—Now let us return to our journey.
Public-domain text, read in full here on John Shaqi.
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