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// Workers AI · dad joke modeWhat did the Lone Mountain Formation say? "I'm a rock solid formation.

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Lone Mountain Formation
Stratigraphic range: Silurian
TypeGeologic formation
Unit ofGreat Basin carbonate platform sequence
UnderliesDevonian carbonate units (regional)
OverliesRoberts Mountains Formation (regional)
Lithology
PrimaryDolostone (dolomite)
OtherLimestone (protolith)
Location
RegionCentral Nevada
CountryUnited States
ExtentGreat Basin, Nevada
Type section
Named forLone Mountain, Nevada
Named byCharles W. Merriam
Year defined1973

The Lone Mountain Formation is a Silurian geologic formation in central Nevada. It consists mainly of thick-bedded dolostone that was originally deposited as shallow marine limestone and later altered through dolomitization. The formation is associated with a transition from deeper-water Silurian deposits below to Devonian carbonate units above. This makes it an important reference unit for understanding changes in sea level, sedimentation, and marine environments in the Great Basin during the late Paleozoic.[1]


While the unit forms part of a broader carbonate platform system in the Great Basin, it is significant for reconstructing Silurian paleogeography in Nevada, as it records the development of a shallow, warm, marine shelf along the margin of a larger carbonate basin. Fossils preserved within the dolomite include brachiopods and corals, which help establish its age and support regional correlations with other Silurian rock units.

See also

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References

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  1. Merriam, Charles Warren (1973). Paleontology and stratigraphy of the Rabbit Hill Limestone and Lone Mountain Dolomite of central Nevada (PDF). United States Geological Survey (U.S. Geological Survey Professional Paper). Washington, D.C.: United States Government Printing Office. Archived from the original (PDF) on 2017-02-16.