Edwards Group: Difference between revisions
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==References== |
==References== |
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* {{cite web|title= Fossilworks: Gateway to the Paleobiology Database|author= Various Contributors to the Paleobiology Database|url= http://www.fossilworks.org/|accessdate= 8 July 2014}} |
* {{cite web|title= Fossilworks: Gateway to the Paleobiology Database|author= Various Contributors to the Paleobiology Database|url= http://www.fossilworks.org/|accessdate= 8 July 2014|deadurl= yes|archiveurl= https://web.archive.org/web/20140731140924/http://fossilworks.org/|archivedate= 31 July 2014|df= }} |
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[[Category:Cretaceous geology of Texas]] |
[[Category:Cretaceous geology of Texas]] |
Revision as of 03:39, 18 September 2017
Edwards Group | |
---|---|
Stratigraphic range: Cretaceous | |
Type | Group |
Location | |
Region | Texas |
Country | United States |
![](http://upload.wikimedia.org/wikipedia/commons/thumb/d/d9/Austin_Chalk_stratigraphic_column_in_Texas.png/300px-Austin_Chalk_stratigraphic_column_in_Texas.png)
The Edwards Group is a geologic group in Texas. It preserves fossils dating back to the Cretaceous period.
A stratigraphic column at the Mount Bonnell Fault location starts with the Lower Cretaceous Trinity Group overlain by the Edwards Group. Upper Cretaceous formations follow, starting with the Del Rio Clay, Buda Limestone, and then the Eagle Ford Group. Formations within the Edwards Group include the Kainier Formation and the Person Formation. The Kainier Formation includes the Dolomitic, Kirschberg, and Grainstone Members.[1]
See also
References
- ^ Saribudak, Mustafa (September 2016). "Geophysical mapping of Mount Bonnell fault of Balcones fault zone and its implications on Trinity-Edwards Aquifer interconnection, central Texas, USA". The Leading Edge. 35 (9). Society of Exploration Geophysicists: 752–758. doi:10.1190/tle35090752.1. Retrieved 12 September 2016.
- Various Contributors to the Paleobiology Database. "Fossilworks: Gateway to the Paleobiology Database". Archived from the original on 31 July 2014. Retrieved 8 July 2014.
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