Jesús de la Peña Hernández
Thus, mountain and valley folds in Fig. 3 are what we need to get a flat-folded figure. We may
observe that the four marked angles are supplementary, for the double of their sum adds up to
360º. Fig. 4 shows the flattened quadrilateral with a view of its internal folds.
Interlude
B
I
A ́
C
3
A
view along X
I
A ́
A
A ́
X
4
B
C
A