“…Let us start by introducing the example hyperbolic material, which here is chosen to be crystal quartz. , This is a naturally occurring hyperbolic material with uniaxial anisotropy and low damping. In this crystal, the condition for hyperbolic dispersion is met in several regions across the infrared spectra due to infrared-active phonon resonances, making one of the principal components of the crystal’s permittivity tensor, , of opposite sign to the other two principal components. , These regions can be generally found between the transverse optical (TO) phonon frequencies and the longitudinal optical (LO) phonon frequencies. , Here, we will focus on the frequency range between 400 and 600 cm –1 (corresponding to free-space wavelengths between 16 and 25 μm) where there exist two regions where the component of parallel to the anisotropy, ε ∥ , is of an opposing sign to the two components perpendicular to it, ε ⊥ , as shown in Figure a.…”