We compare laboratory and field examples of self-organized mineral precipitates in porous media. Laboratory tests of silver chromate precipitation in glass beads and glass bead ⁄ gel mixtures produce structures such as periodic banding and mm-size spherules. These are morphologically similar to the varied forms of iron oxide precipitates in the Jurassic Navajo Sandstone, Utah USA, that preserve records of former fluid redox boundaries in a porous and permeable sandstone. Experimental studies of periodic precipitates in porous media can provide valuable insight for understanding the diagenetic history of similar precipitates in natural environments.