Let
W
W
be a crystallographic group in
R
n
\mathbb R^n
generated by reflections and let
Ω
\Omega
be the fundamental domain of
W
.
W.
We characterize stationary sets for the wave equation in
Ω
\Omega
when the initial data is supported in the interior of
Ω
.
\Omega .
The stationary sets are the sets of time-invariant zeros of nontrivial solutions that are identically zero at
t
=
0
t=0
. We show that, for these initial data, the
(
n
−
1
)
(n-1)
-dimensional part of the stationary sets consists of hyperplanes that are mirrors of a crystallographic group
W
~
\tilde W
,
W
>
W
~
.
W>\tilde W.
This part comes from a corresponding odd symmetry of the initial data. In physical language, the result is that if the initial source is localized strictly inside of the crystalline
Ω
\Omega
, then unmovable interference hypersurfaces can only be faces of a crystalline substructure of the original one.