Trujillo Formation
{{Short description|Geologic formation in Texas and New Mexico, US}}
{{Infobox rockunit
| name = Trujillo Formation
| image = Lighthouse Palo Duro.JPG
| caption = Trujillo Formation in Texas
| type = Formation
| age = Late Triassic,
{{Geological range|216|203}}
| period = Triassic
| prilithology = Sandstone
| otherlithology = conglomerate, mudstone
| namedfor = Trujillo Creek
| namedby = C.N. Gould
| year_ts = 1907
| region = Texas
New Mexico
| country = United States
| coordinates = {{coord|35.2501|N|103.0318|W|display:inline}}
| unitof = Dockum Group
| subunits =
| underlies =
| overlies = Tecovas Formation
| thickness = {{convert|45-210|feet|meters}}
| extent =
| area =
| map = {{Location map+ | United States#Texas
| relief = 1
| width = 250
| float = center
| places =
{{Location map~ | United States#Texas
| lat_deg = 35.2501
| lon_deg = -103.0318
| mark = Purple pog.svg
| marksize = 12
}}
}}
| map_caption =
}}
The Trujillo Formation is a geologic formation in Texas{{cite journal |last1=Gould |first1=C.N. |year=1907 |title=Geology and water resources of the western portion of the Panhandle of Texas |journal=U.S. Geological Survey Water-Supply Paper |volume=191}} and New Mexico.{{cite book |last1=Barnes |first1=V.E. |year=1983 |title=Geologic atlas of Texas |page=Tucumcari sheet |publisher=University of Texas-Austin, Bureau of Economic Geology}} It preserves fossils dating back to the upper Triassic period. It is also known as the Trujillo Sandstone.
Description
The formation consists mostly of gray to brown or red sandstone, but with some conglomerate and mudstone. Conglomerate is more common in the middle beds while mudstone is more common in the middle and upper beds. The sandstone is typically crossbedded and is fine-grained in the lower beds and more coarse in the middle and upper beds. The lower sandstone beds tend to form a prominent cliff. The total thickness varies from {{convert|45-210|feet|meters}}. The formation overlies the Tecovas Formation.
The Cuervo Sandstone Member is preempted by the Trujillo Formation.{{cite book |last1=Lucas |first1=S.G. |title=Dawn of the age of dinosaurs in the American southwest |last2=Hunt |first2=A.P. |publisher=New Mexico Museum of Natural History and Science |year=1989 |pages=150–170 |chapter=Revised Triassic stratigraphy in the Tucumcari basin, east-central New Mexico |access-date=12 November 2021 |chapter-url=https://books.google.com/books?id=Ar1hCgAAQBAJ&dq=Revised+Triassic+stratigraphy+in+the+Tucumcari+basin%2C+east-central+New+Mexico&pg=PA150}}
The formation crops out along Palo Duro Canyon and the Canadian River and their tributaries. It is also widespread in the Sangre de Cristo Mountains.{{cite journal |last1=Lucas |first1=S.G. |last2=Hunt |first2=A.P. |last3=Huber |first3=P. |year=1990 |title=Triassic stratigraphy in the Sangre de Cristo Mountains, New Mexico |journal=New Mexico Geological Society Field Conference Guidebook |volume=41 |pages=305–318 |url=https://nmgs.nmt.edu/publications/guidebooks/downloads/41/41_p0305_p0318.pdf |accessdate=17 September 2020}}
The formation is interpreted as deposition in a braided stream system.{{cite journal |last1=Asquith |first1=George B. |last2=Cramer |first2=Scott L. |title=Transverse Braid Bars in the Upper Triassic Trujillo Sandstone of the Texas Panhandle |journal=The Journal of Geology |date=September 1975 |volume=83 |issue=5 |pages=657–661 |doi=10.1086/628148|s2cid=140676202 }} The lower beds at Palo Duro Canyon contain unusual cone-shaped iron concretions that likely formed in the vadose zone.{{cite journal |last1=Dinwiddie |first1=C. L. |last2=Chan |first2=M. A. |last3=McGINNIS |first3=R. N. |last4=Myers |first4=J. L. |last5=Holliday |first5=W. S. |title=Chronicles of vadose zone diagenesis: cone-shaped iron oxide concretions, Triassic Trujillo Formation, Palo Duro Canyon, Texas: Cone-shaped iron oxide concretions |journal=Geofluids |date=February 2011 |volume=11 |issue=1 |pages=87–96 |doi=10.1111/j.1468-8123.2010.00321.x}}
Fossils
The formation contains Typothorax scutes{{cite journal |last1=Lucas |first1=Spencer G. |last2=Heckert |first2=Andrew B. |last3=Hunt |first3=Adrian P. |title=A new species of the aetosaur Typothorax (Archosauria:Stagonolepididae) from the upper Triassic of east-central New Mexico |journal=New Mexico Museum of Natural History and Science Bulletin |date=2002 |volume=21 |url=https://books.google.com/books?id=imIfCgAAQBAJ&dq=%22trujillo+formation%22&pg=PA215 |accessdate=17 September 2020}} and the unusual cycad Sanmiguelia.{{cite journal |last1=Ash |first1=Sidney R. |title=Occurrence of the Controversial Plant Fossil Sanmiguelia in the Upper Triassic of Texas |journal=Journal of Paleontology |volume=50 |number=5 |year=1976 |pages=799–804 |jstor=1303573}}
History of investigation
The formation was first named as the upper formation of the Dockum Group in 1907 by C.N. Gould.
See also
{{Portal|Earth sciences|Texas|Paleontology}}
References
{{Reflist}}
Category:Triassic geology of Texas
Category:Triassic formations of New Mexico
Category:Sandstone formations of the United States
Category:Conglomerate formations
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