Long Walk Tracksite: Early Cenomanian, Utah
collected 1989

List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Reptilia
Kirkland et al. 1997
Lockley and Hunt 1995
Kirkland et al. 1997
see common names

Geography
Country:United States State/province:Utah County:Emery
Coordinates: 39.2° North, 111.0° West (view map)
Paleocoordinates:46.3° North, 69.1° West (Wright 2013)
Basis of coordinate:estimated from map
Geographic resolution:outcrop
Time
Period: Cretaceous Epoch: Late Cretaceous
Stage: Cenomanian 10 m.y. bin: Cretaceous 5
*Period:Late/Upper Cretaceous
*International age/stage:Albian
Key time interval: Early Cenomanian
Age range of interval: 100.5 - 93.9 m.y. ago
* legacy (obsolete) database fields
Stratigraphy
Geological group:Dakota Formation:Cedar Mountain Member:Mussentuchit
Stratigraphic resolution:group of beds
Stratigraphy comments: site is 10 m below contact with "Dakota" Formation

A radiometric age of 98.37 ± 0.07 Ma was obtained by the OMNH from volcanic ash within the Mussentuchit Member (Cifelli and others, 1997, 1999). Additional ages by Garrison and others (2007) ranging from 96.7 ± 0.5 to 98.2 ±0.6 Ma indicate that the Mussentuchit Member was deposited over an interval of 1.5 Ma during the early Cenomanian and supports a correlation with the siliceous marine Mowry Shale to the north, which is well-constrained from 40Ar/39Ar sanidine ages obtained from bentonite beds that bracket the Mowry in Wyoming; the basal Arrow Creek Bentonite is 98.5 ± 0.5 Ma and the capping Clay Spur Bentonite is 97.2 ± 0.7 Ma (Obradovich, 1993; Ogg and Hinnov, 2012; Sprinkel and others, 2012) near the base of the Upper Cretaceous. Tucker et al. 2020 also suggested a likely depositional age of ~96-94Ma for the Musseuntuchit member.
Lithology and environment
Primary lithology: carbonaceous mudstone
Secondary lithology:lenticular,current ripples,"cross stratification",medium,coarse sandstone
Includes fossils?Y
Includes fossils?Y
Lithology description: carbonaceous mudstone in association with numerous thin, lenticular sandstone bodies. Sandstone is a medium to coarse-grained subarenite with fluvial ripple cross-lamination and large-scale trough cross-bedding.
Environment:fluvial indet.
Taphonomy
Modes of preservation:cast,trace
Size of fossils:macrofossils
Spatial orientation:life position
Associated major elements:some
Disassociated major elements:some
Temporal resolution:snapshot
Spatial resolution:autochthonous
Collection methods and comments
Collection methods:surface (float),surface (in situ),observed (not collected)
Reason for describing collection:taxonomic analysis
Collection dates:1989
Metadata
Database number:27048
Authorizer:M. Carrano Enterer:M. Carrano
Modifier:G. Varnham Research group:vertebrate
Created:2002-11-14 14:28:59 Last modified:2025-02-22 15:12:02
Access level:the public Released:2002-11-14 14:28:59
Creative Commons license:CC0
Reference information

Primary reference:

63747. F. L. DeCourten. 1991. The Long Walk Quarry and Tracksite: unveiling the mysterious Early Cretaceous of the Dinosaur Triangle region. In W. R. Averett (ed.), Guidebook for Dinosaur Quarries and Tracksites Tour, Western Colorado and Eastern Utah 19-25 [M. Carrano/M. Carrano]

Secondary references:

2087 J. I. Kirkland, B. Britt, D. L. Burge, K. Carpenter, R. Cifelli, F. DeCourten, J. Eaton, S. Hasiotis, and T. Lawton. 1997. Lower to Middle Cretaceous dinosaur faunas of the central Colorado Plateau: a key to understanding 35 million years of tectonics, sedimentology, evolution and biogeography. Brigham Young University Geology Studies 42(2):69-103 [M. Carrano/J. Alroy/M. Carrano]
61886 M. G. Lockley and A. P. Hunt. 1995. Dinosaur Tracks and Other Fossil Footprints of the Western United States xxi-338 [M. Carrano/M. Carrano]
13287ETE M. G. Lockley, J. I. Kirkland, F. L. DeCourten, B. B. Britt, and S. T. Hasiotis. 1999. Dinosaur tracks from the Cedar Mountain Formation of eastern Utah: a preliminary report. In D. D. Gillette (ed.), Vertebrate Paleontology in Utah, Utah Geological Survey Miscellaneous Publication 99-1:253-257 [A. Behrensmeyer/M. Carrano/M. Carrano]