Visual walkthrough — Antiderivative — definition, family of solutions (+C)
Before we begin, three plain-word anchors so no symbol arrives unearned:
Step 1 — A slope-report is just an arrow at every point
WHAT. We take a slope-report and draw it not as a graph but as a field of little tilted arrows — one short line segment at each point of the plane, tilted to the slope demands there.
WHY. This is the honest picture of what an antiderivative is given. We are not told heights; we are told tilts. Drawing the tilts first stops us from secretly assuming a height we were never handed.
PICTURE. Look at the figure: at every grid point sits a short pastel dash. Its steepness is fixed by ; its vertical position is NOT fixed by anything yet — that freedom is the whole story.

- — the slope the arrow at horizontal position must have.
- Each dash — one instruction: "a curve passing here must be this steep."
Step 2 — Threading one curve through the arrows
WHAT. We now trace a single curve that stays tangent (flush) to every arrow it passes. Wherever it goes, its ruler-tilt equals the local arrow.
WHY. A curve tangent to the field everywhere is exactly a curve whose slope-report is — i.e. . That equation is the definition of an antiderivative, now drawn instead of written.
PICTURE. The bold lavender curve hugs the arrows. Notice we had to choose where to start it — we dropped it in at one height and let the arrows steer the rest.

- — the tilt of our bold curve at (its ruler).
- — the tilt the arrow field demanded at .
- — "curve matches the field": that is what makes an antiderivative.
Step 3 — Slide it up: the slope never changes
WHAT. Take the bold curve and shift it straight up by a fixed amount . Call the new curve . Check its tilt against the arrows.
WHY. Sliding vertically moves height but drags no tilt with it — a raised hill is the same shape. To see this in symbols we use the single fact that the slope of a flat, constant line is :
PICTURE. Two curves, coral above lavender, offset by the vertical gap . At the marked their little rulers are parallel — same tilt, different height. The raised copy still hugs the same arrows.

- — a constant, the fixed vertical gap (the amount we slid).
- — a horizontal line has zero slope, so shifting adds nothing to the tilt.
- — the shifted curve is also a valid antiderivative.
So there are at least as many antiderivatives as there are choices of — infinitely many.
Step 4 — Are there sneaky other curves, not just vertical slides?
WHAT. Suppose someone claims a second antiderivative that is not a plain vertical copy of . We test that claim by subtracting: define the gap function .
WHY. If and both match the field, their difference should carry no tilt at all. Subtracting cancels the shared slope and isolates whatever "extra shape" might secretly have:
PICTURE. Top panel: two candidate curves. Bottom panel: their gap , drawn as a green track whose ruler is flat everywhere — slope at every .

- — the vertical distance between the two candidates at each .
- — that distance has zero slope; it never tilts.
Step 5 — Zero slope everywhere forces a flat line (the MVT step)
WHAT. We prove the gap cannot secretly rise or fall — it must be a perfectly flat, constant line.
WHY. This is the one place we need a named theorem. The Mean Value Theorem says: between any two points, a smooth curve must somewhere have a ruler tilted at the average steepness between them. But every ruler on reads . So the average steepness between any two points is — meaning the two points sit at the same height. Same height for every pair ⇒ the whole thing is one level line.
PICTURE. Pick two points on . The dashed "average-slope" chord between them is drawn — and because all rulers are flat, that chord is horizontal, forcing the right point down to the left point's height. Slide the pair anywhere: always horizontal.

- The dashed chord — the average slope the MVT promises must be achieved somewhere.
- Horizontal chord — average slope , so no height change is possible.
- — the gap is a single constant.
Putting Step 4 and Step 5 together: Any "other" antiderivative was a vertical slide all along. The family is exactly — no more, no less.
Step 6 — The degenerate case: what if the domain has a hole?
WHAT. Everything above quietly assumed one connected interval . Now break the ground: remove a point, so the domain is two separate stretches (the classic case is , undefined at ).
WHY. The MVT of Step 5 only compares two points if you can travel between them without leaving the domain. Across a gap there is no chord to draw — so the constant on the left piece and the constant on the right piece need not agree. Each connected island gets its own .
PICTURE. A domain split by a shaded forbidden strip. Left island: a curve raised by . Right island: an independently raised curve by . Both hug the same arrows on their own turf; nothing ties their heights together.

- shaded strip — the hole (), where no curve and no chord may cross.
- — two independent constants, one per island.
- / — the antiderivative shape on each side; see Logarithmic & Exponential Integrals for why the log appears exactly at the power-rule exception .
Step 7 — Choosing which curve: a single point pins
WHAT. Out of the infinite stack, demand the curve pass through one known point .
WHY. The stack has exactly one free knob, (Steps 3–5). One equation determines one unknown, so a single point selects a single member. This is the whole idea behind an initial value problem.
PICTURE. The pastel stack of parallel curves, with one coral point marked. Only one curve threads that dot; the rest are dimmed.

The one-picture summary
WHAT. One figure compresses the whole walkthrough: the arrow field (Step 1), the infinite stack of parallel curves all tangent to it (Steps 2–5), the vertical gap labelled between two of them (Step 3), and one highlighted member chosen by a point (Step 7).

- arrow field — the given slope-report .
- the stack — the family ; every curve shares the same tilt at each .
- the gap — the one and only freedom, proven complete by Steps 4–5.
- the coral dot — an initial condition selecting a single curve.
Recall Feynman retelling — the whole walkthrough in plain words
Somebody tells you the tilt of a hill at every step but never the height you started at. First you scatter those tilts as tiny dashes across the field (Step 1). You thread a curve that leans exactly along them (Step 2). Then you notice: lift that whole curve straight up and it still leans the same way — because a flat lift adds no tilt (Step 3). Could a totally different-shaped curve also fit? Subtract it from yours; the leftover has zero tilt everywhere (Step 4), and a thing with zero tilt everywhere on one stretch cannot go up or down — it's dead flat, a constant (Step 5, the Mean Value Theorem). So the "different" curve was just yours slid up by some fixed . The only trap: if the ground has a gap you can't walk across, the two sides can float at different heights, one each (Step 6). Finally, tell me the height at just one spot and I pick the exact curve from the infinite stack (Step 7). That unknown starting height, and nothing else, is the .
Connections
- Parent topic — Antiderivative & the family +C
- Mean Value Theorem — the engine of Step 5.
- Fundamental Theorem of Calculus — where a chosen curve meets areas.
- Power Rule (Integration) & Logarithmic & Exponential Integrals — the hole in Step 6.
- Differential Equations — Initial Value Problems — Step 7 formalised.
- Definite Integral — where harmlessly cancels.