Rare earth elements (REE) are essential to the manufacturing of contemporary technologies. Alloys that contain REE are used in everyday life such as computer memory, DVDs, rechargeable batteries, cell phones, catalytic converters, magnets, fluorescent lighting, and much more. A growing transition towards a carbon-free economy is coincidentally occurring with the use of REE. However, these metals are difficult to mine because it is unusual to find them in concentrations high enough for economical extraction. REE are naturally abundant in sedimentary basin fluids and may be used as natural tracers of fluid sources, pathways, and fluid-rock reactions. This study utilizes recently-collected REE data from formation waters in the Paradox Basin on the Colorado Plateau to investigate concentrations, patterns, and sources of REE. Preliminary results indicate that brines sourced from paleo-evaporated seawater have the highest REE (sum REE values as high as 7.514 ppb), and are particularly enriched in light, more readily-extractable REE. Brines that are sourced from salt dissolution by topographically-driven meteoric recharge that has interacted with siliciclastic rocks have different REE patterns compared to salt- derived brine seeps that have been diluted by snowmelt. REE may be abundant in these brines that have interacted with siliciclastic rocks and/or the salt-derived seeps diluted by snowmelt. The conclusions will convey the possible sources of REE and how REE interacts with these different sources
