The Book of Stars: Being a Simple Explanation of the Stars and Their Uses to Boy LifeCollins, A. Frederick (Archie Frederick)
Science
The Book of Stars: Being a Simple Explanation of the Stars and Their Uses to Boy Life
Collins, A. Frederick (Archie Frederick)
Astronomy -- Juvenile literature; Stars -- Juvenile literature
The railroad companies were just as much put to for it was next to
impossible to make a timetable to fit the local time of each town and
still keep up a running schedule; and the result was that the railroads
finally got up a system of their own which they called _railroad time_.
This was all well enough for everybody but the poor traveler, who, not
knowing the difference in time between local time and railroad time,
nearly always found he was either an hour too early or—as it usually
happened—a minute or two too late to catch his train.
As new towns sprung up and railroads multiplied, things had come to
such a pretty pass in 1883 that nobody but the astronomers knew what
the real time was, and they wouldn’t tell; then a new time scheme was
tried out, and as it is still used we must conclude it is a fairly
good one. It is called the _zone_, or _belt system of standard time_;
the time used is called standard time because the towns and cities and
railroads all use it and there is no confusion.
To understand what _standard time_ means we have to know first what a
_standard meridian_ is. A meridian, as we have said, is an imaginary
line running due north and south anywhere we want it, but while a
standard meridian is also a line running due north and south it has a
fixed position.
The first fixed or _prime meridian_, as it is called, passes through
_Greenwich_ (pronounced Gren´-ij), which is a part of London, England.
The reason this meridian was chosen by geographers to reckon distance
east and west from is because the Royal Observatory at Greenwich is one
of the oldest in the world and it was the first from which exact time
was sent out.
If a circle is divided into 360 degrees, as shown in Fig. 163, and
it is also divided into 24 parts, each part will be a space equal to
15 degrees or 1 hour. Now geographers have divided the Earth into 24
equal parts by meridians separated by 15 degrees, and each space, or
belt, between them represents 1 hour, as shown in Fig. 164. These fixed
meridians start at the first, or prime meridian, at Greenwich and all
the other meridians are measured in degrees east or west of Greenwich
as the case may be.
[Illustration: FIG. 163.—CIRCLE DIVIDED INTO 360 DEGREES AND 24 HOURS.]
Starting west from the first, or prime meridian, which passes through
Greenwich the time at the second standard meridian, which is called the
15th meridian because it is 15 degrees from the first meridian, will be
one hour behind Greenwich time.
At every standard meridian the mean solar time is used as the standard
time and every place on it and halfway to the meridian on both sides
uses it, and so local time and standard.
Public-domain text, read in full here on John Shaqi.
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