Equator

an imaginary great cirele of the celestial vault or on the surface of the earth. In Astronomy.— A great circle of the celestial vault at right angles to its axis, and dividing it into a northern and a southern hemisphere. It is constituted by the plane of the earth’s equator, produced in every direction till it reaches the concave of the celestial sphere. In his progre north and south, and vice vers a, the sun is twice a year in the celestial equator — viz., at the Equinoxes. The point in the equator which touches the meridian is raised above the true horizon by an are which is the complement of the latitude. The sun and planets all have equators,.They rotate around their several axes, and the plane at right angles in each case is the equator of the heavenly body. In Geography.— A great circle on the surface of the earth equidistant from its poles, and dividing it into two hemispheres. Its latitude is zero; it is therefore marked on maps as 0. Other parallels of latitude are counted from it, augmenting in their numerical designation as their distance from it north or south increases, the poles being 90°. The plane of the equator is » plane perpendicular to the earth’s axis and pa ing through its center. In Magnetism.— A somewhat irregular line, nearly but not quite a great circle of the earth, in which there is no dip of the magnetic needle. It is hence called also the aclinie line. It is inclined to the horizon at an angle of 12°, and cuts it at two points almost exactly opposite to each other, the one in the Atlantic and the other in the Pacific. It is not far from the geographical] equator, but its situation slowly alters year by year, there being a slow oscillation of the magnetic poles, while the geographical equator and poles are fixed. The two points in which the magnetic equator cuts the horizon seem traveling at present from i to We Equatorial, an astronomical instrument designed to note the course a the stars as they move through the sky.