Oregon and Eldorado; or, Romance of the RiversBulfinch, Thomas
History
Oregon and Eldorado; or, Romance of the Rivers
Bulfinch, Thomas
Amazon River; Columbia River; El Dorado; Lewis and Clark Expedition (1804-1806); Oregon -- Discovery and exploration
The degrees of least curvature will be longest,
and those of greatest curvature shortest; that is, one would have to
travel farther on the flattened part of the earth to see any difference
in the position of the north-star than in those parts where the
curvature is greater. So a degree of latitude near the pole, if
determined by the position of the north-star, would be found, by actual
measurement, to be longer than one similarly determined at the equator.
It was to ascertain whether the fact was so that the two scientific
expeditions were sent out.
The party which was sent to the northern regions travelled over snow and
ice, swamps and morasses, to the arctic circle, and fixed their station
at Tornea, in Lapland. The frozen surface of the river afforded them a
convenient level for fixing what is called by surveyors the base line.
The cold was so intense, that the glass froze to the mouth when they
drank, and the metallic measuring rod to the hand. In spite, however, of
perils and discomforts, they persevered in their task, and brought back
careful measurements of a degree in latitude 66° north, to be compared
with those made by the other party at the equator, whose movements we
propose more particularly to follow.
Before we take leave of the northern commissioners, however, we will
mention another method they took of demonstrating the same fact. If the
earth be depressed at the poles, it must follow that bodies will weigh
heavier there, because they are nearer the centre of the earth. But how
could they test this fact, when all weights would be increased
alike,--the pound of feathers and the pound of lead? The question was
settled by observing the oscillation of a pendulum. The observers near
the pole found that the pendulum vibrated faster than usual, because,
being nearer the centre of the earth, the attracting power was
increased. To balance this, they had to lengthen the pendulum; and the
extent to which they had to do this measured the difference between the
earth's diameter at the poles, and that in the latitude from which they
came.
Public-domain text, read in full here on John Shaqi.
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