Lincolnshire Formation
The Lincolnshire Formation, often known as the Lincolnshire Limestone, is an Ordovician-age geological formation in the Appalachian region of the Eastern United States.[1][2]
Lincolnshire Formation | |
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Stratigraphic range: Late Ordovician | |
Type | Formation |
Underlies | Edinburg Formation |
Overlies | New Market Limestone |
Location | |
Region | Tennessee, Virginia |
Country | ![]() |
Type section | |
Named for | Lincolnshire Branch of the Clinch River in Tazewell, Virginia |
Named by | Cooper & Prouty, 1943 |
References
- Read, J. Fred; Eriksson, Kenneth A. (2012). "Paleozoic Sedimentary Successions of the Virginia Valley & Ridge and Plateau" (PDF). Virginia Tech Scholarly Works, Department of Geosciences.
{{cite web}}
: CS1 maint: url-status (link) - Cooper, Byron N.; Cooper, G. Arthur (1946). "Lower Middle Ordovician Stratigraphy of the Shenandoah Valley, Virginia". Bulletin of the Geological Society of America. 57: 35–114.
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