Currently working on meteorite based patterns — this one's on barred olivine chondrules, a constituent of stony or chondritic meteorites. Chondrites are the oldest unaltered rocks in our solar system, and contain some of the earliest materials to have condensed from the early solar nebula (chondrules, CAIs). Some even contain presolar grains which come from interstellar sources.
Chondrules are flash heated silicate grains with igneous textures. Of these, barred olivine chondrules are arguably the prettiest, exhibiting a form of skeletal growth (which in turn indicates a large degree of supercooling).
Some reference examples (how pretty!):









