Chapter I
Calculus Meets Shape
When Newton and Leibniz made calculus in the late seventeenth century, curvature was one of the first things it could measure. The curvature of a plane curve at a point is the reciprocal of the radius of the circle that best hugs it there: . Huygens had already used such circles to study pendulum clocks, and Clairaut soon extended the idea to curves twisting through space.
Surfaces were harder, because a surface curves differently in different directions. A cylinder is curved around its circumference and flat along its length. A saddle curves up one way and down the other. Leonhard Euler showed in 1760 that all of this is controlled by two numbers, the principal curvatures and , which occur in perpendicular directions. Gaspard Monge's school in France then built a whole descriptive theory of surfaces on that idea. For curves the story was essentially finished by the 1850s. Frenet and Serret showed that two functions, curvature and torsion , determine any curve in space.
Up to here, this is still Euclid's space. Curves and surfaces are objects sitting in flat three-dimensional space, and their curvature describes how they bend within it.
Chapter II
The Remarkable Theorem
The turn came from surveying. In the 1820s Gauss ran a geodetic survey of the Kingdom of Hanover, measuring huge triangles on the curved Earth. That work led to his Disquisitiones generales circa superficies curvas (1827). In it, he described a surface entirely by how distances are measured on it, the first fundamental form:
He then proved what he called the Theorema Egregium, the "remarkable theorem." The product , now called the Gaussian curvature, can be computed from , , and their derivatives alone. Each principal curvature depends on how the surface sits in space, but their product does not. Rolling a sheet of paper into a cylinder changes from to something nonzero, yet stays , which is why paper rolls without stretching. A sphere has everywhere, which is why no flat map of the Earth can keep all distances correct. Gauss the surveyor had proved why every map must distort.
Chapter III
Intrinsic Geometry
The consequence was philosophical as much as technical: a surface has a geometry of its own, independent of any surrounding space. Pierre Ossian Bonnet made the link to angles explicit in 1848. For a triangle made of shortest paths (geodesics) on a surface,
Look at what this says. On a surface of constant negative curvature, the angles of every triangle add up to less than , and the shortfall is proportional to area. That is exactly the rule of the non-Euclidean geometry that Lobachevsky and Bolyai had just found by pure logic. The two new branches were describing the same thing from opposite sides.
Riemann was the one who joined them. His 1854 lecture took Gauss's intrinsic view, extended it to any number of dimensions, and made the non-Euclidean geometries special cases. That is where Riemannian geometry begins.
Chapter IV
A Closer Look: Measuring Curvature Without Leaving the Surface
The Theorema Egregium says curvature can be measured from inside a surface. Here is how a flat creature living on a sphere of radius could do it with nothing but a rope.
Fix one end of a rope of length at a point and walk around with the other end taut, tracing a circle. On a flat plane the circle's circumference would be . On the sphere, the "circle" is a line of latitude around the pole where the rope is fixed, and its circumference is
a little shorter than . The shortfall reveals the curvature. In general, Gauss's curvature is
and for the sphere this gives . On a saddle the circle comes out longer than , and is negative. On a cylinder it is exactly , and , which is why a cylinder can be unrolled flat while a sphere cannot.
This is why every flat map of the Earth distorts. A map that kept all distances would carry the creature's rope-and-circle experiment over unchanged, but on paper the circle comes out and on the globe it comes out shorter. No choice of projection can reconcile the two.
Chapter V
Surfaces Today
Surfaces in ordinary space remain an active subject. The questions have moved on from "how curved is it?" to "what is the best possible shape?" Examples are minimal surfaces, the shapes of soap films, which locally have the least possible area, and surfaces that bend as little as possible overall. These problems sit where geometry meets nonlinear partial differential equations. Some of them were settled only in the last decade and a half.