Peptido
1074
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Ammolite, thin-film interference from the shell's nacreous structure (this is a mineraloid)
Another example of ammolite, this time showing its origin (an ammonite)
Pleochroism in andalusite
Pleochroism in axinite
Pleochroism in cordierite aka iolite
Pleochroism in epidote
Diffraction caused by the microscopically-banded structure of this agate results in vivid iridescence (agate is a type of rock)
Pleochroism in kornerupine
Interference of light caused by tiny exsolution lamellae of labradorite in this cabochon (technically a rock as the exsolution lamellae are labradorite within a labradorite-depleted matrix)
The same effect, so-called "labradoresence," in an unpolished slab
The opposite side of the same slab, polished
Pleochroism in tanzanite (top) and tourmaline (bottom)
Welo opal gets its iridescent fire from diffraction within its structure of packed silica spheres (opal is a mineraloid, not a mineral)
The sheet-like crystal growth in seraphinite (left) and charoite (right) cause a silky subsurface sheen that moves along the surface of the stones
Pleochroism in tanzanite
woopwoop85
https://giphy.com/gifs/breaking-bad-shocked-dump-UvtKiyeWYEhRC
Peptido
Hank's a pleb, called geodes minerals