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The Mule Spring Limestone, as its name suggests, is mainly composed of limestone rocks. These rocks are medium-gray to light-medium-gray, as well as very fine to fine crystalline, and is thin to very thin-bedded in most areas. In the lower sections of the formation, there are also occasional layers, up to 500ft (150m) thick, of pale-yellowish-brown or greenish-gray shale, limy siltstone and silty limestone.[1] In the Split Mountain, the formation overlies the Harkless Formation and underlies the Emigrant Formation,[1][2] whilst in other areas it overlies the Saline Valley Formation and underlies the Monola Formation.[1]
The Mule Spring Limestone contains examples of Archaeocyatha, a clade of sponges that went extinct during this time,[3] as well as a collection of trilobites.[4][1]
123456Sundberg, Frederick A.; Webster, Mark (July 2022). ""Ptychoparioid" trilobites of the Harkless Formation and Mule Spring Limestone (Cambrian Series 2, Stage 4), Clayton Ridge, Nevada". Journal of Paleontology. 96 (4): 886–920. doi:10.1017/jpa.2021.124.
12Pruss, Sara B.; Karbowski, Grace; Zhuravlev, Andrey Yu; Webster, Mark; Smith, Emily F. (30 June 2024). "DEAD CLADE WALKING: THE PERSISTENCE OF ARCHAEOCYATHUS IN THE AFTERMATH OF EARLY CAMBRIAN REEF EXTINCTION IN THE WESTERN UNITED STATES". Palaios. 39 (6): 210–224. doi:10.2110/palo.2024.005.
12Sundberg, Frederick A.; McCollum, Linda B. (September 2003). "Early and Mid Cambrian trilobites from the outer‐shelf deposits of Nevada and California, USA". Palaeontology. 46 (5): 945–986. doi:10.1111/1475-4983.00328.