Leadville Limestone Explained

Leadville Limestone
Type:Formation
Age:Carboniferous
Namedfor:Leadville, Colorado
Region:Western U.S.
Country:United States
Subunits:Castle Butte Member, Red Cliff Member, Yule Marble (informal)
Underlies:Molas Formation
Overlies:Chaffee Formation
Thickness:220 feet (Marble Quadrangle, CO)
Extent:AZ, CO, NM, UT[1]

, including the Ouray Formation, Elbert Formation, and the Leadville Limestone]]

The Leadville Limestone is a Mississippian geologic formation in the western United States.[2] In Colorado, the upper part is oolitic limestone, while the lower part is primarily dolomite, and somewhat sandy beds indicate the bottom of the formation.

The formation is sparsely fossiliferous but contains many calcareous algae, Foraminifera (Endothyra), sponges, corals (Syringopora), Bryozoa, many brachiopods, gastropods (Bellerophon, Straparolus), Cephalopoda, fragments of ostracods, abundant fragments of crinoids, echinoid spines, and teeth of fish.[3]

A metamorphic facies of this formation is known as the Yule Marble and has been quarried for construction materials.

See also

Notes and References

  1. https://ngmdb.usgs.gov/Geolex/Units/Leadville_8669.html Leadville
  2. https://ngmdb.usgs.gov/Prodesc/proddesc_1828.htm Geologic map of the Marble quadrangle, Gunnison and Pitkin Counties, Colorado
  3. https://pubs.usgs.gov/bul/1142j/report.pdf Geology of Glenwood Springs Quadrangle and Vicinity, Northwestern Colorado