The Study of Astronomy, adapted to the capacities of youth: In twelve familiar dialogues, between a tutor and his pupil: explaining the general phænomena of the heavenly bodies, the theory of the tides, &c.Stedman, John, teacher of astronomy
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The Study of Astronomy, adapted to the capacities of youth: In twelve familiar dialogues, between a tutor and his pupil: explaining the general phænomena of the heavenly bodies, the theory of the tides, &c.
Stedman, John, teacher of astronomy
Astronomy -- Juvenile literature -- Early works to 1800
PUPIL. We find it sometimes extremely hot here in our summer; surely, in
the torrid zone it must be almost insupportable?
TUTOR. They are inured to it from their infancy.—But we are departing
from our subject.—The temperate zones are comprehended between the
tropics and polar circles, that between the tropic of Cancer and the
arctic circle is called the north temperate zone, and that between the
tropic of Capricorn and the antarctic circle the south temperate zone.
PUPIL. I suppose they are called temperate because the heat is not so
intense as in the torrid zone?
TUTOR. True. Neither is the cold so severe as in the frigid zones, which
are those regions comprized within the polar circles, and are
denominated north and south, as they are contiguous to the north or
south poles.
PUPIL. Why are they called frigid?
TUTOR. They are called frigid or frozen zones, because near the poles
there are perpetual fields of ice, the heat of the sun, even in summer,
being insufficient to dissolve it.—Now try if you can tell me the
breadth of each zone in degrees.
PUPIL. The torrid zone being twenty-three degrees and a half on each
side the equator must be forty-seven degrees, which must also be the
breadth of the frigid zones, as the polar circles are distant
twenty-three degrees and a half from the poles, which are their centers.
And, as from the equator to either pole is ninety degrees, from the
equator to the tropics twenty-three and a half, and from the polar
circle to the pole twenty-three and a half, if the sum of these, that
is, forty-seven, be taken from ninety, the remainder, forty-three, will
be the breadth of each of the temperate zones.
TUTOR. Very well.
PUPIL. From what you have told me I have no doubt but that the earth is
globular, but I have no proof of it: I must therefore beg your
assistance.
TUTOR. That it cannot be an extended plane, as some have imagined, is
very evident; for, if it were, the angle made with that plane and the
north pole star would be always equal, for reasons I have before given
you: neither can it be cylindrical, that is like a garden roller, as
others have supposed.—If a person travel northward the pole star becomes
more elevated, and if he could penetrate to the north pole of the earth
the star would be in the zenith, or directly over his head: on the
contrary, if he travel southward, it is more and more depressed till he
arrives at the equator, where the star is in the horizon; as he proceeds
it disappears, and other stars rise to his view, invisible to us. Here
then you see it must be circular northward and southward.
PUPIL. I am convinced it must be so.
Public-domain text, read in full here on John Shaqi.
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