Finlay Limestone Stratigraphic range: Albian | |
---|---|
Type | Formation |
Unit of | Fredericksburg Group |
Underlies | Del Norte Formation |
Overlies | Cox Sandstone |
Thickness | 130–426 feet (40–130 m) |
Lithology | |
Primary | Limestone |
Other | Sandstone |
Location | |
Coordinates | 31°22′N105°36′W / 31.36°N 105.60°W |
Region | New Mexico Texas Chihuahua |
Country | United States Mexico |
Type section | |
Named for | Finlay Mountains |
Named by | G.B Richardson |
Year defined | 1904 |
The Finlay Limestone is a geologic formation in western Texas, southern New Mexico, and northern Chihuahua. It preserves fossils dating back to the early Cretaceous period. [1] [2]
The formation is composed of massive gray limestone with a few thin beds of brown sandstone, with a total thickness of 130–426 feet (40–130 m). [1] [2] It is exposed in the Finlay Mountains ( 31°22′N105°36′W / 31.36°N 105.60°W ), [1] the Sierra de Juarez, [3] and the Cerro de Cristo Rey uplift ( 31°47′13″N106°32′46″W / 31.787°N 106.546°W ). [2] The formation overlies the Cox Sandstone [1] and is overlain by the Del Norte Formation. [2]
The formation is highly fossiliferous, containing fossils characteristic of early Cretaceous Albian and Comanchean age. [2]
The formation includes carbonate replacement deposits of lead, zinc, and silver in northern Mexico, along the Chihuahua CRD belt. [4]
The formation was first defined by G.B. Richardson in 1904 and assigned to the Fredericksburg Group. [1]
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The Del Norte Formation is a geologic formation in Mexico, New Mexico and Texas near the city of El Paso. It preserves fossils dating back to the early Cretaceous period.
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The Smeltertown Formation is a geologic formation in New Mexico. It preserves fossils dating back to the early Cretaceous period.
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