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
Science
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
TUTOR. It is foreign to my present purpose to speak of the inhabitants
of the earth, as that more properly belongs to Geography. Thus much
however I shall tell you, that, although it must be very cold and
dreary, they are not so long deprived of light as you may imagine; for,
even under the poles, when the sun is hidden from them, they are but a
short time in total darkness, for, you must recollect, that the twilight
continues till the sun is eighteen degrees below the horizon; and the
sun’s greatest depression, you know, can be but twenty three degrees and
a half, equal to the inclination of the earth’s axis. Besides this, the
moon is above the horizon of the poles a fortnight together; being half
her period north, and the other half south, of the equator; and, as the
moon at full is in the sign opposite to the sun, the tropical full moons
must be twenty-four hours above the horizon at the polar circles.
PUPIL. This description is very pleasing, as I had no idea of their
being favoured with so much light in the absence of the sun: and, I
find, as the sun is longer above the horizon in summer than in winter,
the moon, on the contrary, continues longer with us in winter, when we
most need her assistance, than she does in summer.
TUTOR. As you seem to understand what I have been explaining, I shall
shew you, that the reason why it is hottest when we are farthest from
the sun is, that in winter when we are nearest to him the days are
shorter, his rays sail very obliquely on us, and are more dispersed than
they are in summer, when he not only remains longer above the horizon,
but being higher, his rays fall more direct on us, by which means the
earth becomes so much heated that it has not time in the short nights to
get cold again.—When the earth is nearest the sun it is summer in the
southern hemisphere, therefore it is reasonable to suppose that the heat
there must far exceed ours in the same latitude; but to counteract this
their summer is shorter by eight days than ours: and it is well known
that it is much colder near the poles in the southern than in the
northern hemisphere: but this is accounted for from there being more
land to retain the heat in the latter than in the former.
PUPIL. My doubts on this head being now removed, I must beg you to give
me such other information as you may think proper.
TUTOR. As there are different degrees of heat and cold, the earth has
been divided into five zones, namely, one torrid, two temperate, and two
frigid zones.
PUPIL. How are they distinguished?
TUTOR. The torrid zone is all that space surrounding the globe contained
between the tropics, having the equator running through the middle of
it. It is so called on account of its excessive heat, for, twice every
year the sun is vertical to the inhabitants, that is, he shines directly
on their heads, and casts no shadow, but under their feet, at noon.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account