Hessian — where it appears
Named by 3 essays across 3 fields — each of them below, with the objects they name alongside it.
Where the surface curves the other way
The impossibility of a perfect map is usually argued on surfaces whose curvature is positive everywhere. The surface a map of the ground actually depicts is not one of them: a stated terrain is saddle-shaped over 79 per cent of its curved area, its curvature runs to twenty-two thousand times the Earth's own, and even a single smooth hill is concave over 89 per cent of itself.
The basins have widths as well as depths
Measuring the height of the pass left one thing owed: shape means widths too. Measured, the basin has three of them — 32°, 16° and 7° at Japan — it gets wider rather than narrower as the region grows, and the exponent it predicts overshoots the measured one by half again.
What the page cannot move
Six rungs measure what a page does to a field's readings and every one of them moves. The critical points do not: found on the sphere and found again in a projection's own page coordinates with nothing shared between the searches, they agree to 10⁻⁷ degrees and in type at every point, on every projection. What the page does move is their shape, by a factor bounded exactly by the indicatrix's axis ratio squared.
Named alongside it
The objects these essays reach for when they reach for this one.
SaddleVerificationAnisotropyAspectAspect searchBasinConformalityCoordinate independenceCritical pointCurvatureDevelopableEuler characteristic