Why is Railroad Valley Unique?

Railroad Valley contains a mineral-rich evaporite deposit that formed over a 3 million year period.  The deposit contains both liquids (brine) and solid salts, and this makes the deposit quite unique.  It is one of the largest such deposits in the world, and the most significant in North America.  South America and China have similar deposits, and these locations are the worlds current source of lithium, a strategic mineral for the USA.

Cross Section

3PL has spent many millions of dollars on propietary research to find, delineate, and analyze the brine deposit in Railroad Valley. We offer only brief  glimpses of a few diagrams from our technical documents, without much explanation, but hope you enjoy what is shown.

MT Node Data

Structure Contour Map