* DEFINITIONS Earth's surface The earth is not a true sphere and is slightly flattened at the poles. Its polar axis is somewhat smaller in length (about 43.45 km) than that of its equatorial axis. Any section of the earth parallel to the equator is a circle and any of its section parallel through the poles is an ellipse. Such a figure may be generated by revolving about its minor axis and is called an oblate spheroid. Precisely, the equatorial section is also slightly elliptical and therefore such a figure should be called an ellipsoid. Precise observations indicate that the southern hemisphere is a trifle larger than the northern. Therefore, all the polar sections are oval and can be called ovaloid. ...

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