Below, each foundation is: plain words → the picture → why the topic needs it. They are ordered so every new symbol only uses ideas already built above it. Nothing is assumed — no symbol is used before the section that defines it.
Look at figure s01. The black dot is the heavy central body. The red arrow is r: it points at the planet, and its length is the distance r (no arrow — plain r means just the length, forgetting direction; we make this precise in the next section).
Why the topic needs it: the orbit is the set of all positions r the planet visits. Every later idea on this page — the velocity arrow, the spin-making cross product, the orbit's shape — is built on top of this one arrow.
Picture: take the red arrow, keep it pointing the same way, but squash it until it's exactly one unit long. That stub is r^. So any position splits as r=rr^ = (how far) × (which way).
Why the topic needs it: the whole page distinguishes "how far" (r) from "which way" (r^). Gravity pulls with a strength set by r and a direction set by r^; separating them now lets every later statement about "outward" versus "inward" be exact.
In figure s02, the red arrow v is drawn tangent to the orbit path — it always points along the direction of travel. It is generally not aligned with r: r points outward from the centre, while v points along the curve.
Why the topic needs it: the spin amount is built from both where you are (r) and where you're going (v). One without the other tells you nothing about the orbit's rotation.
Look again at figure s02: the small wedge marks ϕ. Here is what each size of ϕlooks like physically (we describe motion in words now; the exact rate symbols come in §8):
Why the topic needs it: the angle between r and v is exactly what the cross product in §5 measures, and it is what makes the simple picture "distance × speed" work only at special points. Note that sinϕ takes the same value at ϕ and 180∘−ϕ, so a point on the outbound half and its mirror on the inbound half share the same value of the sideways ingredient — a first hint of a conserved quantity. See Flight-path angle.
This is the heart of the whole topic, so we build it slowly.
Figure s03 shows why the length is that parallelogram area. Two arrows sweep out a slanted box; its area is base × height =∣a∣×(∣b∣sinθ). When the arrows point the same way (θ=0) the box is flat — zero area — so a×a=0.
Why the topic needs it:h=r×vis the definition of specific angular momentum. Its length is (twice) the rate at which the position arrow sweeps out area — the link to Kepler's Second Law. Its direction is fixed, which is why the orbit stays in one plane. Because h=rvsinϕ, the simple h=rv holds only at the apsides where ϕ=90∘ (this is the parent's "h=rv everywhere" mistake).
Now we can finally read the gravity arrow the parent note uses: the acceleration of the planet is a=−r2GMr^. Every piece is now defined — GM (strength), r2 (weaker with distance, length from §2), and −r^ (direction: inward, from §2).
Why the topic needs it: because the small mass cancels out of orbital motion (see the parent's "why divide by m"), the only mass that matters is the central M, and it always appears glued to G. So GM=μ is the natural single knob. It sits inside h=GMp and inside gravity a=−r2GMr^.
The four shape symbols, each a picture (figure s04):
Why the topic needs it:h=GMp links the conserved spin h to the shape symbol p. Without p (and its cousins e,a,θ) the formula would have nothing geometric to say. These come out of the Two-body problem.
Plain picture: if r is your distance from the centre, r˙ is your outward/inward speed (r˙>0 outward, r˙<0 inward), and r¨ is whether that speed is speeding up. Zero r˙ means momentarily neither approaching nor receding — exactly the apsides, the same ϕ=90∘ points from §4 (now stated as a rate: r˙=0).
Why the topic needs it: the conservation proof uses dtdh=0, and the orbit derivation uses r˙,r¨,θ˙ in polar form. Every step in the parent note that has a dot or a dtd is standing on this idea.