Before you can read a single line-equation, you need to be fluent in the little symbols hiding inside it. This page builds each one from absolute zero, in the order they depend on each other. Nothing here assumes you've met it before.
Everything in this topic lives on a flat sheet with two number-lines crossing at right angles.
Why we need it: a line is an infinite collection of points. To talk about those points with numbers, we first need an address system. The plane is that address system.
Look at figure s01: the green dot sits at (3,2) — walk 3 right, then 2 up.
Why the topic needs it: an equation of a line is a test. You feed it a point (x,y) and it answers "yes, you're on the line" or "no." Points are the things being tested.
Why the topic needs it: steepness is a comparison between two points — "for THIS much sideways, how much up?" That comparison is exactly Δy against Δx.
Why a ratio and not just the rise? Because rising 2 over a run of 1 is twice as steep as rising 2 over a run of 4. Only the ratio — up-per-step — measures true steepness independent of how big a step you took. That is the whole reason we divide.
Why does an angle turn up in a chapter about lines? Because "steepness" and "angle of tilt" are two words for the same thing — and the bridge between them is tan.
Why tan and not sin or cos?sin and cos each involve the slanted length (the hypotenuse), which changes when you pick a bigger triangle. But rise-over-run cancels that length out — exactly what slope needs. tanθ is defined as opposite-over-adjacent, so it lands precisely on our rise/run ratio. That's why slope =tanθ and not any other trig function.
Why the topic needs it: the slope–intercept form y=mx+c literally names the y-intercept c, and the Intercept form of a line is built entirely from both intercepts.
Why it matters here: in ax+by+c=0 (the standard form, and the starting point of Distance of a point from a line), the letters a,b,c are frozen numbers picking out one line, while x,y roam over all its points. Telling constants from variables is what lets you "read off" the slope −a/b without confusion.
Read top to bottom: the plane hosts points, points let us measure change, change gives rise/run, rise/run is slope, slope istanθ — and slope plus a point plus the membership idea produce every form of the line equation.