Idaho Strategic initially staked its Lemhi Pass Project to target an area with the greatest concentration of known veins where the Lemhi Pass, Dan Patch, and Bull Moose faults intersect or approach one another. The rare earth elements mineralization at Lemhi Pass has primarily been found in phosphate minerals such as monazite and xenotime. To date, Idaho Strategic has conducted geologic mapping, surface sampling programs, and a modest trenching program. Select results showing increased levels of rare earth mineralization (up to 6% TREO) have revealed a unique distribution of rare earths showing a relatively high level of magnet REEs, including neodymium, praseodymium, dysprosium, terbium, and samarium - which collectively account for more than 50% of the total rare earth elements grade on average. According to Virginia Gillerman of the Idaho Geological Survey, “The Lemhi Pass ores are unusual in that they consistently show a strong enrichment in the middle rare earths, especially neodymium. Electron microprobe analyses of monazite reveal as much as 35 weight percent Nd oxide, which is possibly the highest content known in the world.” –Gillerman, V.S., 2011, Idaho GeoNote 44: Rare Earth Elements and Other Critical Metals in Idaho