We are normally only interested in orthogonal coordinate systems, where the surfaces of constant coordinate values (isosurfaces) intersect each other along . There are a large number of these, linked to certain 2D mappings of the (complex) plane. We shall mainly restrict ourselves to three.
There are a substantial set of other orthogonal coordinates that have use in certain cases; most of these are the three dimensional analogue of 2D coordinates obtained by a conformal map, extended as either cylindrical or polar coordinates. The simplest of these are discussed in many books (parabolic, spheroidal, ellipsoidal, toroidal, bispherical, bipolar, conical, ....). In engineering this choice of coordinate system is sometimes referred to as “field theory”.