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and so on and so forth. The agate and calcedony or jasper or native opal basically fills those voids up. And when it does, that's where you get your agates. And so you get all kinds of different formations from the Troido agate to waterline agate to all kinds of neat stuff. And so, but yeah, it's a long, age-long process that the rightolytic ash is super silica. And so that silica precipitates out and into the voids and then that fills up. And then because of that natural round air pocket type thing, you get these little round chunks that, you know, thunder eggs that form. So there you go. Dachty, Jack, K-D7, papawisky-browler the high-dose-repriorate radio. Alright, well, thank you.