North Dakota lignite has the potential to be a new source of mineral commodities that are vital to the economic and national security of the United States. There is little to no current domestic production for many of the raw mineral materials needed to manufacture many components in energy and defense applications, in addition to a wide array of modern electronic consumer goods. The U.S. currently relies on imports of many of these commodities, termed critical minerals, including the sixteen rare earth elements (REE). Some of the REEs (e.g., lanthanum and cerium) are relatively abundant and overproduced by traditional hard rock mines, but other, less abundant REEs (e.g., dysprosium, terbium, scandium) are highly valuable and thus may be economic at relatively low concentrations if cost-effective extraction methods can be developed. Broadly speaking, techniques which need to break down REE-bearing primary minerals to extract the elements are costly, but in coal, especially low ranks like lignite, an appreciable percentage of the REE content may be weakly bound into organic complexes and easily extracted. REE concentrations in U.S. coal are generally around three times lower than the average concentrations in rocks and sediment near the Earth's surface but occasionally can be found enriched or significantly enriched 5 to 10 times higher than average upper continental crust. Other high-value critical elements (e.g., gallium and germanium) may also occur in economic concentrations in lignite and could be co-produced with the REEs. With higher relative proportions of the more valuable REEs and other critical elements, easy extraction, and lower amounts of radioactive contaminants like thorium, lignite may be an economical source of REEs at far lower concentrations than traditional ores. The U.S. Department of Energy has proposed coal containing 300 ppm REE could be a potentially promising feedstock. The North Dakota Geological Survey (NDGS) has collected 324 samples of lignite and carbonaceous mudstone that exceed 300 ppm REE, from 1,706 samples collected from outcrops across western North Dakota. REEs are known to be mobilized by acidic waters during the weathering of clastic sediments. North Dakota lignites are found to be slightly enriched (364 to 910 ppm REE) where they occur below uplands that have experienced long-term, low-intensity modern weathering, and can be enriched (910 to 1,820 ppm REE) or even significantly enriched (over 1,820 ppm REE) where they occur below intervals of intense Paleocene weathering. The first REE-enriched lignite identified by the NDGS was from the Logging Camp Ranch area in Slope County, where several samples from the Harmon, Hanson, and H lignite interval showed elevated REE concentrations. The 768 sample analyses from 165 measured geologic sections in this report detail that initial elevated REE concentrations from the top of the Harmon lignite are very localized, likely the result of upland weathering as the slight REE enrichment is confined to a small terrace. The H lignite bed has been miscorrelated by previous authors, causing the name to previously be assigned to an REE-enriched coal in the Logging Camp Ranch area, but the detailed correlation in this report suggests an overlying, non-enriched lignite is the H bed, and the thinner REE-enriched lignite(s) below are unnamed coals within a zone of weathered strata known as the Rhame bed. The Rhame bed is a 10- to 30-foot (3 to 9 m) thick sequence of kaolinized sediment that was apparently weathered during an extended period of little to no deposition when the climate was much warmer than today, roughly 61 million years ago. Lignites below this thick bed of kaolinite can be significantly enriched in antimony, arsenic, barium, beryllium, germanium, lithium, molybdenum, uranium, and total REE, including the highest dry coal basis concentration (2,792 ppm REE) and dry ash basis concentration (5,642 ppm REE) from this project to date. [ABSTRACT FROM AUTHOR]