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Natural minerals on Earth are as old as $\\mathcal{O}(1)\\,$Gyr and, in many minerals, the damage tracks left by recoiling nuclei are also preserved for timescales long compared to 1 Gyr once created. Thus, even reading out relatively small target samples of order 100 g, paleo-detectors would allow one to search for very rare events thanks to the large exposure, $\\varepsilon \\sim 100\\,{\\rm g}\\,{\\rm Gyr} = 10^5\\,{\\rm t}\\,{\\rm yr}$. 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