02/21/2023
These nodules are from the Cedar Mountain Formation, a Cretaceous aged rock in southeast Utah. The nodules are frequently identified as Coprolite (Fossil p**p) but they are really soil nodules (more on why they are not p**p is a topic for another conversation). The nodules form as calcite precipitation around roots and such in a fairly arid soil. The nodules were part of the depositional environment and are found anywhere that this part of the Cedar Mountain Formation is present (called the Ruby Ranch Member). However, in many places, there are minerals in these nodules. Around the Henry Mountains near Hanksville and Yellowcat north of Moab they can be found with colorful Agate. These nodules that I found not too far from the Reed view area on I70 have some nice pink, red, white and even orange Agate. Some of them formed geodes with Calcite crystals and others have chalcopyrite in them. The minerals are precipitated into fractures in the nodules by mineral rich ground water. The minerals in the groundwater can be different from one place to another and at different times throughout history. Much of the mineralization in these nodules is associated with hydrothermal activity that also deposited the abundant uranium and copper minerals in the area. This location was not on any rockhounding map. But if you learn the geology and geologic maps, you can find areas that are off the beaten path, and often have much more stuff because they are not flooded with people. It is an important note, however, that often the Ruby Ranch Member is mapped incorrectly. In this area, it was mapped as part of the Jurassic Morrison Formation. But by learning the geology and the associated rocks, you can find some really cool areas.