Point Lookout Sandstone
Geological formation in New Mexico and Colorado From Wikipedia, the free encyclopedia
Geological formation in New Mexico and Colorado From Wikipedia, the free encyclopedia
The Point Lookout Sandstone is a Cretaceous bedrock formation occurring in New Mexico and Colorado.
Point Lookout Sandstone | |
---|---|
Stratigraphic range: | |
Type | Formation |
Unit of | Mesaverde Group |
Sub-units | Hosta Tongue |
Underlies | Menefee Formation |
Overlies | Crevasse Canyon Formation |
Thickness | 300 ft (91 m) |
Lithology | |
Primary | Sandstone |
Other | Shale |
Location | |
Coordinates | 37.316°N 108.419°W |
Region | Paradox Basin, San Juan Basin |
Country | United States |
Type section | |
Named for | Point Lookout |
Named by | A. J. Collier |
Year defined | 1919 |
The formation consists of two informal members. The lower is a sequence of thinly bedded sandstone and shale,[1] while the upper is a massive medium- to fine-grained cross-bedded sandstone, light gray to buff in color, that is a conspicuous cliff-forming unit.[1][2] Maximum thickness is 131 meters (430 feet).[1]
The lower contact is placed at the first thin sandstone bed above the shale of the Mancos Shale. The formation is overlain by the Menefee Formation.[1]
The Point Lookout Sandstone was deposited in the Cretaceous Interior Seaway, as part of a regressive sequence as the seaway was receding. It is transitional between the marine environment of the underlying Mancos and the coastal plain environment of the overlying Menefee Formation.
Dinosaur remains are among the fossils that have been recovered from the formation, although none have yet been referred to a specific genus.[3]
The ammonite Clioscaphites vermiformis was identified in the formation.[4]
Exposures of the Point Lookout Sandstone at Apache Mesa in New Mexico contain heavy mineral deposits, rich in titanium, zirconium, rare earth elements, and other valuable metals. However, the deposits are much too small to be economical to mine as of 2021. The deposits represent a beach placer deposit similar to ones seen in the southeastern U.S. Atlantic coast, southeastern Australia, and India.[5]
The sandstone was first described by A. J. Collier for exposures in cliffs at Point Lookout, in Mesa Verde National Park, Montezuma County, Colorado, in the Paradox Basin,[6] and later described by Allen and Balk in 1954 as part of the Mesaverde Group in the San Juan Basin in New Mexico.[7]
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