Letters on Astronomy: in which the Elements of the Science are Familiarly Explained in Connection with Biographical Sketches of the Most Eminent AstronomersOlmsted, Denison
Science
Letters on Astronomy: in which the Elements of the Science are Familiarly Explained in Connection with Biographical Sketches of the Most Eminent Astronomers
Olmsted, Denison
Astronomy
The poles of the horizon are the zenith and nadir. The _zenith_ is the
point directly over our heads; and the _nadir_, that directly under our
feet. The plumb-line (such as is formed by suspending a bullet by a
string) is in the axis of the horizon, and consequently directed towards
its poles. Every place on the surface of the earth has its own horizon;
and the traveller has a new horizon at every step, always extending
ninety degrees from him, in all directions.
_Vertical circles_ are those which pass through the poles of the
horizon, (the zenith and nadir,) perpendicular to it.
The _meridian_ is that vertical circle which passes through the north
and south points.
The _prime vertical_ is that vertical circle which passes through the
east and west points.
The _altitude_ of a body is its elevation above the horizon, measured on
a vertical circle.
The _azimuth_ of a body is its distance, measured on the horizon, from
the meridian to a vertical circle passing through that body.
The _amplitude_ of a body is its distance, on the horizon, from the
prime vertical to a vertical circle passing through the body.
Azimuth is reckoned ninety degrees from either the north or south point;
and amplitude ninety degrees from either the east or west point. Azimuth
and amplitude are mutually complements of each other, for one makes up
what the other wants of ninety degrees. When a point is _on_ the
horizon, it is only necessary to count the number of degrees of the
horizon between that point and the meridian, in order to find its
azimuth; but if the point is _above_ the horizon, then its azimuth is
estimated by passing a vertical circle through it, and reckoning the
azimuth from the point where this circle cuts the horizon.
The _zenith distance_ of a body is measured on a vertical circle passing
through that body. It is the complement of the altitude.
The _axis of the earth_ is the diameter on which the earth is conceived
to turn in its diurnal revolution. The same line, continued until it
meets the starry concave, constitutes the _axis of the celestial
sphere_.
The _poles of the earth_ are the extremities of the earth's axis: the
_poles of the heavens_, the extremities of the celestial axis.
The _equator_ is a great circle cutting the axis of the earth at right
angles. Hence, the axis of the earth is the axis of the equator, and its
poles are the poles of the equator. The intersection of the plane of the
equator with the surface of the earth constitutes the _terrestrial_, and
its intersection with the concave sphere of the heavens, the
_celestial_, equator. The latter, by way of distinction, is sometimes
denominated the _equinoctial_.
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