The mirror instability is prevalent in planetary and cometary magnetos
heaths and other high beta environments. We review the physics of the
linear instability. Although the instability was originally derived fr
om magnetohydrodynamic fluid theory, later work showed that there were
significant differences between the fluid theory and a more rigorous
kinetic approach. Here we point out that the instability mechanism hin
ges on the special behavior of particles with small velocity along the
field. We call such particles resonant particles by analogy with othe
r uses of the term, but there are significant differences between the
behavior of the resonant particles in this instability and in other in
stabilities driven by resonant particles. We comment on the implicatio
ns of these results for our understanding of the observations of mirro
r instability-generated signals in space.