Diamonds in Colorado, Kansas, Montana and Wyoming - the Wyoming Craton
Of the 40 kimberlites mapped in the State Line district alone, all yielded diamonds, but the grade of the deposits remains unresolved. Just in 2006-07, Hausel found several prviously unknown kimberlites in this region along with more than 300 high-quality cryptovolcanic structures - many are likely kimberlites and a few represent two of the largest in the world.
14.2 carat octahedron from Kelsey Lake Colorado.
Hundreds of other KIM anomalies were identified to the west in a region covering >250 square miles where diamondiferous lamprophyres were discovered. KIM anomalies & diamonds have also been identified in the Front Range, Laramie Range, Hartville uplift, Seminoe Mountains, Medicine Bow Mountains, Green River Basin, Powder River Basin, Sweetgrass Hills, Bighorn Mountains etc.
Raw Wyoming diamond showing excellent trigons on surface of stone.
In the Leucite Hills lamproite field and other localities, several diamond-stability indicator minerals were recovered and no follow-up work ever conducted (as of 2009).
The Wyoming Craton, based on these discoveries, is a major (unexplored) kimberlite-lamproite-lamprophyre province. During the past 30 years, we have collected a very sizable data base on these anomalies. In addition to the kimberlites found in Colorado and Wyoming, other kimberlites, lamproites and lamprophyres were discovered in Montana and Kansas within the Wyoming Craton. Hausel (1998) also described kimberlites, lamproites, lamprophyres and other potentially diamondiferous rocks along with reported placer diamonds throughout portions of the US.
Assortment of kimberlitic indicator minerals including purple pyrope, red, orange and pink pyrope garnets (Cape rubies), chromian diopside (Cape emeralds), picroilmenite and chromite.
Below - two faceted Cape rubies from diamondiferous lamprophyres and anthills in the Cedar Mountain region, Green River Basin, southwestern, Wyoming.