The function whose graph is the surface takes positive values between the two parabolas and, and negative values elsewhere. At the origin, the three-dimensional point on the surface that corresponds to the intersection point of the two parabolas, the surface has a saddle point. The surface itself has positive Gaussian curvature in some parts and negative curvature in others, separated by another parabola, implying that its Gauss map has a Whitney cusp. Although the surface does not have a local maximum at the origin, its intersection with any vertical plane through the origin is a curve that has a local maximum at the origin, a property described by Earle Raymond Hedrick as "paradoxical". In other words, if a point starts at the origin of the plane, and moves away from the origin along any straight line, the value of will decrease at the start of the motion. Nevertheless, is not a local maximum of the function, because moving along a parabola such as will cause the function value to increase. The Peano surface is a quartic surface.
As a counterexample
In 1886 Joseph Alfred Serret published a textbook with a proposed criteria for the extremal points of a surface given by Here, it is assumed that the linear terms vanish and the Taylor series of has the form where is a quadratic form like, is a cubic form with cubic terms in and, and is a quartic form with a homogeneousquartic polynomial in and. Serret proposes that if has constant sign for all points where then there is a local maximum or minimum of the surface at. In his 1884 notes to Angelo Genocchi's Italian textbook on calculus, Calcolo differenziale e principii di calcolo integrale, Peano had already provided different correct conditions for a function to attain a local minimum or local maximum. In the 1899 German translation of the same textbook, he provided this surface as a counterexample to Serret's condition. At the point, Serret's conditions are met, but this point is a saddle point, not a local maximum. A related condition to Serret's was also criticized by, who used Peano's surface as a counterexample to it in an 1890 publication, credited to Peano.
Models of Peano's surface are included in the Göttingen Collection of Mathematical Models and Instruments at the University of Göttingen, and in the mathematical model collection of TU Dresden. The Göttingen model was the first new model added to the collection after World War I, and one of the last added to the collection overall.