Sugar Run Dolomite
| Sugar Run Dolomite | |
|---|---|
| Stratigraphic range: Silurian | |
 Chicago's Holy Name Cathedral, made of Sugar Run Dolomite, aka "Athens marble" or "Lemont limestone" | |
| Type | Formation |
| Lithology | |
| Primary | dolomite |
| Location | |
| Region |  Illinois |
| Country |  United States |
| Type section | |
| Named for | Sugar Run Stream |
The Sugar Run Dolomite is a geologic formation in Illinois. It is a finely-bedded dolomite, preserving fossils dating back to the Silurian period. This formation is named for the Sugar Run stream in Joliet, along which it is well exposed. The dolomite is off-white/grey on freshly cut surfaces, but over time oxidizes to a distinctive cream yellow color, due to trace presence of iron. It is a member of the Niagaran series.[1]
Use in architecture[edit]
This formation has been quarried for building material since the mid-19th century, sometimes sold under the misleading trade name of "Athens marble". It is also known as Joliet or Lemont limestone.[2] It was used widely in the construction of many Chicago homes and buildings from the 1850s-1880s, including the famous Chicago Water Tower. By the 1890s, it fell out of fashion as a building material in favor of more durable Indiana limestone.
See also[edit]
References[edit]
- ^ Bradbury, James (1988). Joliet-Lemont Limestone (PDF). Landmarks Preservation Council of Illinois. Retrieved 10 March 2023.
- ^ "Limestoned".
- Various Contributors to the Paleobiology Database. "Fossilworks: Gateway to the Paleobiology Database". Retrieved 17 December 2021.
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