under linear coordinate changes of the variables. They show that the key to the classification is a certain "surface with whiskers" that they have named the "Holy Grail":
(Click on the window if your browswer can launch Geomview; you will get an image that you can manipulate interactively.) Roughly speaking, the surface consists of two bowls--one opening upward, the other downward--joined in the center by a tetrahedron with curved faces and edges. There is a pair of (red) whiskers inside each bowl. The image above is an animated GIF created by Pau Atela. See acknowledgment at the end.
If you look carefully (better, if you handle the interactive Geomview
image), you'll notice that the upper red whiskers continue through the
Grail surface along the seam between the upper bowl and the central
tetrahedron. Along this seam (actually, a curve of double points of the
surface), f has a pair of repeated factors, but the factors are
real instead of complex; f is like
Finally, at each the four points where the red whiskers join up with the
Grail surface, the surface has a swallowtail point.
The quartic form f associated with this point has a quadruple
factor and is therefore like
Question: What is f like on the different parts of the Grail surface itself? You should be able to figure this out using the fact that f has a double factor and is a transitional form between the types that lie in the open regions on either side.
In fact, the Grail is actually a developable surface; that is, the tangent planes to the surface at all points along a given line are the same). You can see this best in the Geomview image: Turn the surface until part of it is particularly shiny. Now the light comes from a point just behind you, so a piece of the surface is shiny if its tangent plane is perpendicular to your line of sight. Thus all shiny parts must have the same orientation. Finally, notice that, as you turn the surface, the shiniest parts of the surface always lie along a single generating line.
Next, consider the central tetrahedron. Its vertices are the four swallowtail points. Two of its six edges are the "seams" (the curves of double points) that join it to the upper and the lower bowls. The other four edges are cuspidal (that is, they have a cusp-shaped cross section) and they go from the top bowl to the bottom. These four edges make up a single curve with singular points at the vertices. The straight lines that generate the Grail are tangent to this boundary curve. (This is most evident in the Geomview image if you select the Inspect option, open the Appearances window, and choose to Show Edges.) Thus the Grail is the tangent developable of this curve, giving a second proof that the Grail is developable.
To understand the shape of the Grail, it helps to see that the surface "morphs" (or evolves) from a much simpler and more familiar surface--an ordinary cone. If you click on the image below, you'll see a Geomview animation that shows the cone on the left "morphing" into the Grail on the right. (Note: the animation file is large--1.8 MB.)
You can think of the metamorphosis this way. Start with a circle and its normals in a plane. The normals all meet in the center of the circle. If you lift the normals up 45° out of that plane, they generate a cone and meet at the vertex of the cone. Now perturb the circle into an oval, keeping the normals perpendicular to the oval and lifted up 45° out of the plane. The normals then generate the Grail.
The Holy Grail also appears in the work of Alberto
Castro on the space of Hermitian matrices in