DATUM: WGS 84 / EPSG:4326
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Category: Distortion Math

Tissot Distortion Crucible

"Compute local scale distortion $h, k$, area factor $hk$, and angular shear $2\theta'$ across 14 map projections"

Select any projection and latitude to calculate Nicolas Auguste Tissot's infinitesimal deformation ellipse, visualizing the trade-offs between conformality and equivalence.

THE PROJECTION DISTORTION CRUCIBLE

Mercator Projection (1569)

Inventor: Gerardus Mercator · Family: Cylindrical

TEST LATITUDE:60° North
0° (Equator)30° (Subtropics)60° (Greenland)85° (Arctic)
Conformal (Angles)
Equal-Area (Sizes)
Compromise Map
Uninterrupted
CONTINENTAL SCALE DISTORTION RATIO:
True geographic area of Greenland (2.16M km²) is 1/14th (0.07×) of Africa (30.37M km²).
Projected Visual Ratio:1:1 (Equal Size!)
TISSOT INDICATRIX (Lat: 60°N)Area: 4.00×
h=2.00k=2.00
MERIDIAN (h)
2.00
PARALLEL (k)
2.00
ANGULAR (2θ')
0.0°
Cartographic & Political Critique:

"When co-opted into classrooms and wall atlases, Mercator visually inflates imperial powers in North America and Europe while drastically shrinking the African continent, South America, and the equatorial belt."

Formula: h = k = \sec \phiFull Mathematical Dossier

Operating Instructions

  • Select a target projection from the dropdown menu (e.g. Mercator, Gall-Peters, Robinson, Winkel Tripel).
  • Adjust the latitude slider from 0° (Equator) to 85° (Polar).
  • Observe the Tissot ellipse deform in real time, comparing local meridian scale ($h$) and parallel scale ($k$).
  • Inspect the calculated Area Factor ($hk$) and Maximum Angular Deformation ($2\theta'$).

Mathematical & Geodetic Theory

Tissot's theorem proves that an infinitesimal circle on a sphere is transformed into an ellipse on a map projection with semi-major axis $a$ and semi-minor axis $b$. The area scale is $a \cdot b = hk \cos \theta'$, and maximum angular deformation is $\sin \theta' = \frac{a - b}{a + b}$.

Mathematical Baseline: Tissot, A. (1881)