Look at the figure. The surface is the pastel sheet. At the marked point, the coral arrow is the direction "walk East" and its steepness is fx; the lavender arrow is "walk North" and its steepness is fy. A slope is just rise over run for a tiny step — nothing more mysterious than the tilt of a ramp.
Now the star of the show:
The whole theorem is the claim: twist measured East-then-North = twist measured North-then-East. We now prove it by never trusting the algebra until the picture forces it.
WHAT IT LOOKS LIKE: the four coloured dots on the base plane are the corners; the vertical sticks rising to the surface are the four heights. Name them:
far corner: East & Northf(a+h,b+k)East onlyf(a+h,b)North onlyf(a,b+k)basef(a,b)
WHAT IT LOOKS LIKE: the green (+) corners and coral (−) corners in the figure. Notice the magic property: swap the roles of East and North (swap h↔k, swap the axes) and the four terms just reorder — Δ is unchanged. It doesn't know or care which direction we call "first." That hidden symmetry is the entire engine of the proof.
WHAT IT LOOKS LIKE: the figure marks c1 somewhere inside the East interval (we don't know where — shown as a floating tick with a "?" ). At that column, we now hold x=c1 and look at how the East-slope fx changed between North-height b and b+k. That bracket is a difference of fx in y — begging for a second MVT.
WHAT IT LOOKS LIKE: the mystery point (c1,d1) sits somewhere inside the pastel rectangle — pinned down only to "inside," shown by the dashed box and a floating dot. Remember this: Δ=hk⋅(East-then-North twist there).
WHAT IT LOOKS LIKE: the same rectangle, now sliced the other way (horizontal-gap-first). A second mystery point (c2,d2) — generally a different interior point than (c1,d1), but also trapped inside the box.
WHAT IT LOOKS LIKE: a sequence of nested pastel rectangles shrinking to the single point (a,b), both mystery dots funnelling inward. Continuity is what guarantees the twist-values ride smoothly along to the centre instead of leaping.
Negative steps (h<0 or k<0): the rectangle just extends West or South instead. MVT works on [a+h,a] equally well; the factor hk carries the correct sign and cancels identically. Result unchanged. Picture: the box flips to the other side of (a,b) — same story.
h=0 or k=0 (a degenerate rectangle): then Δ=0 trivially (two pairs of corners coincide) — no information, so we never divide by zero because we take the limit h,k→0through nonzero values, never at zero.
Continuity FAILS — the crease case: if fxy or fyx is not continuous at (a,b), Step 7 breaks. The two hidden points can approach (a,b) along different paths and land on different limiting twist-values. This is not hypothetical:
f(x,y)=⎩⎨⎧x2+y2xy(x2−y2),0,(x,y)=(0,0)(x,y)=(0,0)⇒fxy(0,0)=−1=fyx(0,0)=1.
WHAT IT LOOKS LIKE: two panels. Left — the smooth surface: both mystery dots slide to the same twist value (curves meet). Right — the creased counterexample surface: the two dots approach along different ridges, twist-values split to −1 and +1. The crease is the culprit; smoothness is what forbids it.
Everything on one canvas: the tiny rectangle with its four signed corners feeds the single symmetric number Δ. Peel it East→North and out comes hkfxy; peel it North→East and out comes hkfyx. Since it's the sameΔ, divide by hk, shrink the box, and — provided the twist is continuous — both funnel to the identical value at (a,b).
Recall Feynman: retell the whole walkthrough
Draw a tiny rectangle on a bumpy sheet and measure the height at all four corners. Add the two far corners, subtract the two side corners — this magic combination throws away everything flat and keeps only the twist in that little patch. Call it Δ.
Now here's the trick: I can compute Δ by first comparing the two North edges, then seeing how that changes going East — that reading is the "East-then-North twist." OR I can first compare the two East edges, then see how that changes going North — the "North-then-East twist." But it's the exact same Δ either way! So the two twists, each equal to Δ divided by the area hk, must be equal — at least at some mystery point inside the box. Finally I shrink the box down to a point. As long as the twist doesn't suddenly jump nearby (that's continuity), both mystery readings slide onto the same value right at my point. That's Clairaut: fxy=fyx. And if the sheet has a crease — a spot where slopes leap — the two readings can refuse to meet, which is exactly why we need smoothness.