Given a CPOS polygon P1P2…P2n and a real number λ, we define its λ-equidistant polygon P(λ) by the vertices which split the great diagonals in the ratio λ:(1- λ). More explicitly, the vertices of P(λ) are
Pi(λ)=Pi + λ(Pn+i-Pi), i=1,2,…,2n
It is easy to see that:
When the λ-triangle Pi-1PiPi+1 has a different orientation than the original Pi-1PiPi+1, we say that Pi(λ) is a cusp of the λ-equidistant.
The 0.2-equidistant of a CPOS polygon (pink). Labeled green vertices are cusps.
In this next Geogebra Applet, you can construct your 10-sided CPOSP as before (moving P1-P9) and play with the λ-equidistants (drag the λ-slider or press the “play” button on the lower left corner; you can use the mouse wheel to zoom in or out AND erase previous cusp traces, if you wish). Whenever a vertex of the equidistant turns into a cusp, we mark it green. As you move λ, what do they trace?
This is a Java Applet created using GeoGebra from www.geogebra.org – it looks like you don’t have Java installed, please go to www.java.com
In fact (see [1] for proofs):
· Consecutive edges of the equidistant form a cusp if, and only if, such edges do not cross the corresponding great diagonal;
· The cusps of the equidistants form the Central Symmetry Set of the original CPOSP.
[1] M. Craizer, R. Teixeira and M. Horta, “Parallel Opposite Sides Polygons”, preprint.