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A line is a set of points of constant direction, up to sign. More precisely, a line is a set of points such that there exists a nonzero vector vv such that for any two distinct points P,QP,Q on the line, PQ→=Q−P\overrightarrow{PQ} = Q-P is a vector either in the direction of vv or −v-v. Algebraically, a line is just a set of the form {(a+tx,b+ty):t∈R}\{(a+tx,b+ty):t\in\mathbb{R}\}, where (a,b)(a,b) is any point on the line and vv is in the direction of ±(x,y)\pm(x,y).

The ray starting from (a,b)(a,b) (in the direction (x,y)(x,y)) is the set of points {(a+tx,b+ty):t≥0}\{(a+tx,b+ty) : t \ge 0\}.

The dilation/scaling/homothety centered at (a,b)(a,b) with nonzero ratio/factor r≠0r\ne0 is the transformation (mapping) sending a point (x,y)(x,y) to (a+r(x−a),b+r(y−b))(a+r(x-a),b+r(y-b)). Note that it fixes the point (a,b)(a,b) (sends it to itself). (Why should r≠0r\ne0?)

To define the half-planes to the left (above) or right (below) a nonzero vector (a,b)(a,b), we'll need to rely on orientation from the previous section. But with orientation it's easy: the half-plane to the left (or above) (a,b)(a,b) is the set of points left of (a,b)(a,b). The half-plane to the right (or below) (a,b)(a,b) is the set of points right of (a,b)(a,b).

Type a concept, like “slope” or “photosynthesis”.

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