GENERATION AND TRANSPORT OF TOXIC METALS AT THE FORMOSA MINE SUPERFUND SITE, DOUGLAS COUNTY, OREGON
Geologic and hydrogeologic factors contribute to generation and transport of toxic metals. Rocks in the area are subaqueously deposited volcanics including dacitic and basaltic tuffs and basalt flows. These rocks contain negligible neutralization potential to counteract acid generation. Groundwater flow, controlled by secondary porosity, is locally modified by pipe flow through underground workings. Silver Butte receives annual precipitation of approximately 140 cm, mostly occurring between November and March. This causes marked seasonal fluctuations in the water table and seasonal inundation of backfilled mine wastes. This results in development and rinsing of vestigial acidity and metals, and seasonal flushes of concentrated mine water into the environment. Mine water discharges from adit portals and fractures located in tributary drainages downgradient from the mine. In the downstream environment, dissolved metals attenuate through precipitation, adsorption, and dilution, causing accumulation of toxic metals in aquatic ecosystems. Understanding the interrelationships between VMS mineralization, mining and mineral processing methods, and site-specific geologic and hydrogeologic factors is the first step in remediating the abandoned mine.