Industrial and com. use of chlorinated ethenes (CEs) such as cis-1,2-dichlrorethene (cis-DCE) and trichloroethene (TCE) for cleaning purposes has led to groundwater contamination causing harm to human and environmental health. Iron(II) minerals within the surrounding soil have been shown to degrade these contaminants abiotically into nonharmful carbon gases (ethane, ethene, and acetylene). However, the minerals and conditions in the subsurface that lead to degradation of CEs are often poorly understood, or have only been observed in the laboratory under extreme conditions of pH and iron(II) or mineral concentrations To determine iron(II)-minerals ability to reduce CEs, we conducted experiments with ferrous sulfide (FeS), iron(II) hydroxide (Fe(OH)2), and chukanovite (ferrous hydroxy-carbonate) over a range of pHs and iron(II) concentrations We measured cis-DCE and TCE loss and carbon gas production using gas chromatog. The rate of CE degradation varies for each of the different pHs and iron(II) concentrations, but is slow with 55.9% carbon products (12% ethane, 41% ethene, 0% acetylene) observed for Fe(OH)2 at pH of 8.3 over three months and 31.4% carbon products (7% ethane, 18% ethene, 2% acetylene) for FeS at pH 10.3 with 2 mM excess iron(II) over three months. So far, we have observed most rapid production of products with Fe(OH)2 and FeS, however in comparison, little reduction of CEs has been observed at with chukanovite over time. Our work suggests that conditions favoring the precipitation of Fe(OH)2 is most likely to result in significant CE reduction