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An ellipsoid is essentially a sphere that has been stretched or compressed independently along three perpendicular axes, giving it three (possibly different) semi-axis lengths a, b, and c instead of a single radius. Ellipsoids show up throughout science and engineering: the Earth itself is more accurately modeled as an oblate ellipsoid (slightly flattened at the poles) rather than a perfect sphere in geodesy and GPS systems, egg shapes and certain pharmaceutical capsules approximate ellipsoids, and statisticians use ellipsoids to visualize confidence regions in multivariate data.
How it works
Enter the three semi-axes a, b, and c — each measured from the ellipsoid's center to its surface along one of the three perpendicular directions (not the full end-to-end length). The calculator applies V = (4/3)πabc, which is the direct three-variable generalization of the sphere volume formula (4/3)πr³, replacing the single repeated r with three independent semi-axis lengths.
- Enter semi-axis a.
- Enter semi-axis b.
- Enter semi-axis c.
- Click Calculate to see your results.
Examples
a = b = c = 3
V = (4/3)π(3)(3)(3) ≈ 113.10, matching the sphere volume formula for radius 3 — as expected, since equal semi-axes make the ellipsoid a perfect sphere.
a = 5, b = 3, c = 2
V = (4/3)π(5)(3)(2) = (4/3)π(30) ≈ 125.66 cubic units — a flattened, egg-like shape rather than a sphere.
Common mistakes to avoid
- Entering full axis lengths (diameters, end-to-end) instead of semi-axes (center-to-surface, half-lengths) — this would double each dimension and inflate the volume by a factor of 8.
- Assuming the ellipsoid volume formula also gives the correct surface area — that's a much harder calculation with no simple closed form in general.
- Mixing up which semi-axis is a, b, or c when the ellipsoid has a specific orientation that matters for your application.