Wasatch Formation Explained

Wasatch Formation
Type:	Formation
Period:	Ypresian
Age:	Early Eocene (Clarkforkian-Bridgerian) (typically Wasatchian) ~
Prilithology:	Mudstone, shale, siltstone, sandstone
Otherlithology:	Claystone, lignite
Namedfor:	Wasatch Range
Namedby:	Hayden
Year Ts:	1873
Location Ts:	Echo Canyon, Summit County & Weber Canyon, Ogden, Utah
Coordinates Ts:	40.88°N -110.97°W (Echo Canyon) 41.1358°N -111.9039°W (Weber Canyon)
Region Ts:	Utah
Region:
Coordinates:	41.2°N -108.8°W
Paleocoordinates:	46°N -92.6°W
Subunits:	See text
Underlies:	Green River & Fowkes Formations, Santa Fe Group
Overlies:	Fort Union, Williams Fork, Torrejon & Evanston Formations
Thickness:	Variable, up to 1500m (4,900feet)
Extent:	Powder River, Green River, Wind River, Bighorn, Piceance & Uinta Basins

The Wasatch Formation (Tw)^[1] is an extensive highly fossiliferous geologic formation stretching across several basins in Idaho, Montana, Wyoming, Utah and western Colorado.^[2] It preserves fossils dating back to the Early Eocene period. The formation defines the Wasatchian or Lostcabinian (55.8 to 50.3 Ma), a period of time used within the NALMA classification, but the formation ranges in age from the Clarkforkian (56.8 to 55.8 Ma) to Bridgerian (50.3 to 46.2 Ma).

Wasatch fauna consists of many groups of mammals, including numerous genera of primates, artiodactyls, perissodactyls, rodents, carnivora, insectivora, hyaenodonta and others. A number of birds, several reptiles and fish and invertebrates complete the diverse faunal assemblages. Fossil flora and ichnofossils also have been recovered from the formation.

The formation, first named as Wasatch Group in 1873 by Ferdinand Vandeveer Hayden, was deposited in alluvial, fluvial and lacustrine environments and comprises sandstones, siltstones, mudstones and shales with coal or lignite beds representing wet floodplain settings.

The Wasatch Formation is an unconventional tight gas reservoir formation in the Uinta and Piceance Basins of Utah and the coal seams of the formation are mined in Wyoming. At the Fossil Butte National Monument, the formation crops out underlying the Green River Formation. In the Silt Quadrangle of Garfield County, Colorado, the formation overlies the Williams Fork Formation.^[3]

Description

Definition

The Wasatch Formation was first named as the Wasatch Group by Ferdinand Vandeveer Hayden in the 1873 edition of his original 1869 publication titled "Preliminary field report of the United States Geological Survey of Colorado and New Mexico: U.S. Geological and Geographical Survey of the Territories", based on sections in the Echo and Weber Canyons, of the Wasatch Mountains.^[4] In the language of the native Ute people, Wasatch means "mountain pass" or "low pass over high range."^{[5] [6]} According to William Bright, the mountains were named for a Shoshoni leader who was named with the Shoshoni term wasattsi, meaning "blue heron".^[7]

Outcrops

At the base of Fossil Butte are the bright red, purple, yellow and gray beds of the Wasatch Formation. Eroded portions of these horizontal beds slope gradually upward from the valley floor and steepen abruptly. Overlying them and extending to the top of the butte are the much steeper buff-to-white beds of the Green River Formation, which are about 300feet thick. The Wasatch Formation ranges from about 3000feet in the western part of the Uinta Basin, thinning to 2000feet in the east. In the Silt Quadrangle of Garfield County, Colorado, the formation overlies the Williams Fork Formation.^[3] The formation is exposed in the Desolation and Gray Canyons pertaining to the Colorado Plateau in northeastern Utah,^[8] and in Flaming Gorge National Recreation Area at the border of southwestern Wyoming and northeastern Utah.^[9]

Extent

The Wasatch Formation is found across six states in the northwestern United States, from Montana^[10] and Idaho in the north across Utah^[11] and Wyoming to Colorado in the southwest. The formation is part of several geologic provinces; the eponymous Wasatch uplift, Uinta uplift, Green River, Piceance, Powder River, Uinta and Paradox Basins and the Colorado Plateau sedimentary province and Yellowstone province.^[12]

In Montana, the formation overlies the Fort Union Formation and is overlain by the White River Formation.^[13] There is a regional, angular unconformity between the Fort Union and Wasatch Formations in the northern portion of the Powder River Basin.^[14]

Subdivision

Many local subdivisions of the formation exist, the following members have been named in the literature:^[12]

Member	States	Lithologies	Notes
Alkali Creek Tongue		Mudstones and sandstones	align=center	^[15]
Atwell Gulch		Sandstones and mudstones	align=center
Bullpen			align=center
Cathedral Bluffs Tongue		Mudstones and sandstones	align=center
Chappo			align=center
Cowley Canyon			align=center
Desertion Point Tongue			align=center
Hiawatha			align=center
Kingsbury Conglomerate		Feldspathic conglomerates	align=center
Knight			align=center
La Barge			align=center
Lookout Mountain Conglomerate		Conglomerates	align=center
Luman Tongue			align=center	^[16]
Main Body		Mudstones	align=center	^[17]
Molina		Sandstones	align=center
Moncrief		Feldspathic conglomerates	align=center
New Fork Tongue			align=center
Nightingale			align=center
Niland Tongue			align=center
Ramsey Ranch			align=center
Red Desert Tongue			align=center
Renegade Tongue			align=center
Shire		Sandstones and mudstones	align=center
Tunp			align=center

Lithologies and facies

In the Fossil Basin at the Fossil Butte National Monument, Wyoming, the Wasatch Formation consists primarily of brightly variegated mudstones with subordinate interbedded siltstones, sandstones, and conglomerates and represents deposition on an intermontane alluvial plain.^[18] In Mesa County, Colorado, the formation comprises interbedded purple, lavender, red, and gray claystones and shales with local lenses of gray and brown sandstones, conglomeratic sandstones, and volcanic sandstones that are predominantly fluvial and lacustrine in origin.^[19] Along the western margin of the Powder River Basin, the Wasatch Formation contains two thick conglomeratic members (in descending order, the Moncrief Member and Kingsbury Conglomerate Member).^[20]

The Molina Member of the formation is a zone of distinctly sandier fluvial strata. The over- and underlying members of the Molina are the Atwell Gulch and Shire members, respectively. These members consist of infrequent lenses of fluvial-channel sandstones interbedded within thick units of variegated red, orange, purple and gray overbank and paleosol mudstones.^[21]

The Molina Member represents a sudden change in the tectonic and/or climatic regimes, that caused an influx of laterally-continuous, fine, coarse and locally conglomeratic sands into the basin. The type section of the Molina is located near the small town of Molina on the western edge of the basin and is about 90m (300feet) thick. These sandy strata of the Molina Member form continuous, erosion-resistant benches that extend to the north of the type section for approximately 25km (16miles). The benches are cut bycanyons or "gulches", from which the Atwell Gulch and Shire Gulch members get their names. The Molina forms the principle target within the Wasatch Formation for natural gas exploration, although it is usually called the "G sandstone" in the subsurface.^[21]

Provenance

Detrital zircons collected from the middle part of the formation in the Powder River Basin of Wyoming, where the Wasatch Formation reaches a thickness of more than 1500m (4,900feet) were gathered for U-Pb geochronological analysis. The detrital zircon age spectrum ranged from 1433 to 2957 Ma in age, and consisted of more than 95% Archean age grains, with an age peak of about 2900 Ma. The 2900 Ma age peak is consistent with the age of Archean rocks at the core of the Bighorn Mountains. The sparse Proterozoic grains were likely derived from the recycling of Paleozoic sandstone units. The analysis concluded that the Wasatch sandstone is a first cycle sediment, the Archean core of the Bighorn uplift was exposed and shedding sediment into the Powder River Basin during time of deposition of the Wasatch Formation and the Powder River Basin Wasatch detrital zircon age spectra are distinct from the coeval Willwood Formation in the Bighorn Basin west of the Bighorn Mountains.^[22] Cobbles and pebbles in the Wasatch are rich in feldspathic rock fragments, with individual samples containing as much as 40 percent,^[23] derived from erosion of the Precambrian core of the Bighorn Mountains.^[20] Part of the feldspar has been replaced by calcite cement.^[24] Glauconite is present in the Wasatch, although always in volumes of less than1 percent of the grains. It most probably was derived from the nearby, friable, glauconite-bearing Mesozoic strata of the eastern Bighorn Mountains.^[25]

The presence of the Kingsbury Conglomerate at the base of the Wasatch Formation indicates that tectonic activity in the immediate vicinity of the Powder River Basin was intensifying. The conglomerate consists of Mesozoic and Paleozoic rock fragments. The lack of Precambrian fragments indicates that the metamorphic core of the Bighorn Mountains had not been dissected by this early deformation.^[26] Deformation in the upper part of the formation has been interpreted as the result of the last phase of uplift during the Laramide orogeny.^[27]

Correlations

The basal part of the Wasatch Formation is equivalent to the Flagstaff Formation in the southwest part of the Uinta Basin.^[28] The Wasatch Formation is correlated with the Sentinel Butte and Golden Valley Formations of the Williston Basin.^{[29] [30]}

Paleontological significance

The Wasatch Formation is the defining formation for the Wasatchian, ranging from 55.8 to 50.3 Ma, within the NALMA classification. The Wasatchian followed the Clarkforkian stage (56.8-55.8 Ma) and is defined by the simultaneous first appearance of adapid and omomyid euprimates, hyaenodontid creodonts, perissodactyls and artiodactyls.^[31] The deposits of the formation were laid down during a period of globally high temperatures during the Paleocene-Eocene Thermal Maximum (PETM). Mean annual temperatures were around 25C and temperature variations were minimal during this time.^[32]

At the Fossil Butte National Monument, the Wasatch Formation preserved ichnofossils attributed to arthropods and described as Lunulichnus tuberosus. Trace fossils are common within the upper part of the Main Body Member. These traces occur in three distinct alluvial depositional settings: flood basin/alluvial plain, crevasse splay, and fluvial channel. Flood basin deposits (dominated by alluvial paleosols with pronounced color variegation) are characterized by common Planolites, rare Skolithos and small, meniscate plug-shaped burrows, possibly Celliforma.^[33]

Crevasse splay deposits (current-rippled to planar laminated, fine-grained sandstone to siltstone) are characterized by a mixed assemblage of vertical (Arenicolites, Skolithos, unwalled sinuous shafts, shafts with discoidal lenses of sediment), sub-vertical (Camborygma and Thalassinoides) and horizontal (Scoyenia, Rusophycus, Taenidium, Planolites and Palaeophycus) burrows. Large, vertically oriented burrows (Camborygma, cf. Ophiomorpha, Spongeliomorpha and Thalassinoides) are the dominant forms within fluvial channel deposits.^[33]

Fossil content

Among the following fossils have been found in the formation:^[2]

Mammals

Primates

• Absarokius abbotti^[34]
• A. gazini^[35]
• Anaptomorphus aemulus^[36]
• Anemorhysis sublettensis
• Arapahovius gazini
• Artimonius nocerai
• A. witteri^[37]
• Cantius frugivorus^{[38] [39]}
• C. mckennai
• C. nunienus
• Carpodaptes cf. hazelae
• Chiromyoides minor^[40]
• Chlororhysis knightensis
• Copelemur australotutus^{[41] [39]}
• C. praetutus
• C. tutus^[42]
• Ignacius frugivorus^[40]
• Loveina minuta^[34]
• L. sheai
• L. zephyri^[43]
• Microsyops angustidens
• M. knightensis
• M. latidens^{[35] [44]}
• M. cf. elegans
• M. cf. scottianus
• Notharctus robinsoni
• N. venticolus
• Omomys carteri^[36]
• O. lloydi
• Plesiadapis dubius^[45]
• Plesiadapis cf. cookei^[46]
• Plesiadapis cf. rex^[40]
• Simpsonlemur cf. jepseni
• Smilodectes sororis^[47]
• Steinius cf. vespertinus
• Tetonius matthewi
• Tetonoides pearcei
• cf. Trogolemur myodes^[34]
• Uintanius rutherfurdi
• Utahia carina^[37]
• Walshina mcgrewi^[36]
• Washakius insignis
• W. izetti
• cf. Choctawius sp.
• Cantius sp.
• Carpolestes sp.
• Chlororhysis sp.^[34]
• Loveina sp.
• Microsyops sp.
• Notharctus sp.^[48]
• Omomys sp.
• Phenacolemur sp.^[39]
• Picrodus sp.^[49]
• Tetonius sp.
• Trogolemur sp.^[37]
• Uintasorex sp.
• Phenacolemurinae indet.

Artiodactyls

• Antiacodon pygmaeus^[36]
• Bunophorus cf. etsagicus
• B. grangeri
• B. macropternus
• B. sinclairi^[50]
• Diacodexis secans^[51]
• Gagadon minimonstrum^[52]
• Hexacodus pelodes
• H. uintensis^[53]
• Antiacodon sp.
• Bunophorus sp.
• Diacodexis sp.
• Hexacodus sp.
• Microsus sp.
• Dichobunidae indet.

Perissodactyls

• Arenahippus pernix^[54]
• Cardiolophus semihians
• cf. Dilophodon destitutus^[55]
• Eotitanops borealis
• Heptodon calciculus^[56]
• H. posticus
• Homogalax protapirinus
• Hyrachyus modestus^[36]
• Hyracotherium vasacciense^[57]
• Lambdotherium popoagicum^[56]
• Minippus index
• Orohippus proteros
• Orohippus cf. pumilus^[58]
• Palaeosyops fontinalis^[58]
• Protorohippus venticolum^[59]
• Xenicohippus craspedotum^[60]
• Eotitanops borealis
• Helaletes sp.
• Heptodon sp.
• Homogalax sp.
• Hyrachyus sp.^[58]
• Hyracotherium sp.
• Lambdotherium sp.
• Orohippus sp.
• Palaeosyops sp.
• Equidae indet.^[60]
• Helaletidae indet.^[58]
• Isectolophidae indet.
• Perissodactyla indet.
• Tapiroidea indet.^[61]

Hyaenodonta

• Gazinocyon vulpeculus^[62]
• Iridodon datzae^[63]
• Prolimnocyon antiquus^[63]
• Prototomus secundarius
• Tritemnodon cf. strenuus
• Prolimnocyon sp.
• Sinopa sp.
• Thinocyon sp.
• Tritemnodon sp.
• Hyaenodontidae indet.^[64]

Acreodi

• Dissacus cf. praenuntius^[45]
• Hapalodectes leptognathus
• Pachyaena ossifraga^[61]
• Wyolestes dioctes^[65]
• Dissacus sp.
• ?Mesonyx sp.
• Mesonychidae indet.

Carnivora

• Miacis latidens
• Vulpavus australis^[66]
• V. canavus^[67]
• Miacis sp.
• Vulpavus sp.
• Miacidae indet.^[68]

Cimolesta

• Amaramnis gregoryi^[61]
• Esthonyx acutidens
• Esthonyx cf. bisulcatus^[69]
• Palaeoryctes cruoris
• Palaeoryctes cf. punctatus
• ?Trogosus cf. latidens^[61]
• Esthonyx sp.
• Trogosus sp.

Dinocerata

• cf. Bathyopsis fissidens
• Probathyopsis cf. harrisorum^[45]
• Bathyopsis sp.

Erinaceomorpha

• Adunator meizon

Eutheria

• Aceroryctes dulcis^[70]
• Arctocyon nexus^[71]
• Bessoecetor cf. septentrionalis^[72]
• Chriacus oconostotae
• Lambertocyon gingerichi
• Palaeosinopa incerta^[73]
• P. lacus
• Palaeosinopa cf. didelphoides^[61]
• cf. Palaeosinopa lutreola^[61]
• Thryptacodon australis
• T. pseudarctos^[74]
• Chriacus sp.
• Claenodon sp.

Ferae

• Ambloctonus major^[61]
• Brachianodon westorum
• Didymictis altidens^[61]
• D. cf. protenus^[75]
• Oxyaena forcipata
• O. lupina^[64]
• Protictis agastor
• P. paralus
• Raphictis cf. gausion
• Tubulodon pearcei
• Tytthaena parrisi
• Uintacyon asodes
• Viverravus cf. acutus^[61]
• V. gracilis
• V. lutosus^[61]
• V. minutus^[58]
• V. sicarius
• Didymictis sp.
• Patriofelis sp.
• Viverravus sp.^[75]

Glires

• Acritoparamys francesi
• Knightomys depressus^[76]
• K. huerfanensis^{[76] [77]}
• Leptotomus parvus^[58]
• Lophiparamys murinus
• Microparamys hunterae
• M. minutus^[36]
• Mysops fraternus^[36]
• ?Notoparamys blochi
• Paramys copei^[61]
• P. delicatior^[36]
• P. delicatus^[36]
• P. excavatus^[61]
• P. taurus
• P. wyomingensis
• Pauromys schaubi^[36]
• Pseudotomus robustus^[78]
• Reithroparamys delicatissimus^{[36] [78]}
• R. huerfanensis^{[36] [78]}
• R. cf. debequensis
• Sciuravus bridgeri^[36]
• S. nitidus^[58]
• S. wilsoni^[61]
• Thisbemys perditus^[76]
• Tuscahomys ctenodactylops^{[76] [79]}
• Microparamys sp.^[36]
• Paramys sp.^[80]
• Reithroparamys sp.^{[36] [81]}
• Tillomys sp.^[36]
• Cylindrodontidae indet.
• Paramyidae indet.^[36]
• Rodentia indet.^[64]
• Sciuravidae indet.^[36]

Insectivora

• Apatemys bellulus
• A. bellus^[36]
• A. cf. whitakeri^[82]
• Labidolemur soricoides
• Unuchinia dysmathes
• Apatemys sp.^[83]

Leptictida

• Palaeictops cf. bicuspis
• Prodiacodon cf. concordiarcensis
• Prodiacodon cf. furor
• Prodiacodon cf. tauricinerei

Lipotyphla

• Cedrocherus aceratus
• Eoictops novaceki^[84]
• Entomolestes sp.^[85]
• Adapisoricinae indet.^[83]

Macroscelidea

• Aletodon cf. quadravus
• Apheliscus nitidus^[80]
• Apheliscus cf. insidiosus^[86]
• Dorraletes diminutivus
• Haplomylus speirianus^{[61] [57] [70]}
• Haplomylus cf. scottianus^[86]
• Litocherus lacunatus
• Scenopagus priscus^[36]
• Scenopagus sp.

Multituberculata

• Ectypodus cf. powelli
• Neoplagiaulax cf. hazeni
• Neoplagiaulax cf. hunteri
• Ptilodus kummae
• Mesodma sp.
• Ectypodus sp.
• Parectypodus sp.^[83]
• ?Prochetodon sp.^[80]
• Ptilodus sp.

Pantodonta

• Barylambda faberi
• Coryphodon armatus^[87]
• C. lobatus^[87]
• C. radians^[61]
• Coryphodon sp.^[81]

Pholidota

• Palaeanodon sp.^[69]

Placentalia

• Copecion brachypternus^[88]
• Ectocion collinus
• E. osbornianus^[45]
• E. superstes^[89]
• Hyopsodus loomisi^[90]
• H. minor^[42]
• H. minusculus^{[36] [58]}
• H. paulus
• H. powellianus^{[90] [42]}
• H. wortmani
• H. cf. mentalis^[81]
• H. cf. walcottianus^[51]
• Meniscotherium chamense^[91]
• M. cf. robustum^[89]
• M. cf. tapiacitum^{[90] [57]}
• Phenacodus grangeri
• P. intermedius^[90]
• P. trilobatus^[86]
• P. vortmani^[90]
• Ectocion sp.
• Hyopsodus sp.^[90]
• Phenacodus sp.^[90]

Soricomorpha

• Leptacodon cf. munusculum
• Nyctitherium serotinum^[36]
• Leptacodon sp.
• Wyonycteris sp.

Taeniodonta

• Stylinodon mirus^[92]

Theriiformes

• Copedelphys innominata^[93]
• Herpetotherium knighti^{[90] [78]}
• H. innominatum^[90]
• Peradectes elegans
• P. chesteri^[90]
• Peratherium edwardi^[81]
• P. marsupium^[90]
• Ectoganus sp.^{[90] [81] [69]}
• Oodectes sp.
• Paleotomus sp.^[90]
• Stylinodon sp.^[94]
• Uintacyon sp.
• Epoicotheriidae indet.
• Leptictidae indet.
• Marsupialia indet.^[61]
• Metacheiromyidae indet.
• Nyctitheriidae indet.^[83]
• Oxyaenidae indet.
• Pantolestidae indet.
• Stylinodontidae indet.

Birds

• Eocrex primus^[95]
• Limnofregata hutchisoni^[96]
• Presbyornis sp.

Reptiles

• Anosteira ornata
• Apodosauriscus minutus
• Arpadosaurus gazinorum^[97]
• A. sepulchralis^[98]
• Baena arenosa^[99]
• Boavus occidentalis
• Boverisuchus vorax
• Calamagras primus
• Dunnophis microechinus
• Echmatemys stevensoniana
• Echmatemys cf. cibollensis^[100]
• Emys wyomingensis^[100]
• Entomophontes incrustatus^[98]
• Eodiploglossus borealis
• cf. Eoglyptosaurus donohoei^[101]
• Glyptosaurus agmodon^[98]
• G. sylvestris
• Machaerosaurus torrejonensis
• Notomorpha testudinea
• Palaeoxantusia amara^[98]
• Palepidophyma lilliputiana^[98]
• Parasauromalus olseni^[100]
• Provaranosaurus fatuus^[98]
• Psilosemys wyomingensis
• Restes rugosus
• Saniwa ensidens
• Scincoideus grassator^[98]
• Suzanniwana revenanta^[98]
• Trionyx aequa^[102]
• Xenochelys lostcabinensis^[103]
• Xestops savagei^[98]
• X. vagans^[102]
• cf. Crocodylus affinis^[100]
• Allognathosuchus sp.^[100]
• Anolbanolis sp.
• Coniophis sp.^[102]
• Echmatemys sp.
• Tinosaurus sp.
• Palaeoxantusia sp.^[102]
• Paranolis sp.
• Parasauromalus sp.
• Procaimanoidea sp.^[102]
• Stylinodon sp.^[104]
• Suzanniwana sp.
• Tinosaurus sp.^[102]
• cf. Jepsibaena sp.
• cf. Restes sp.
• cf. Saniwa sp.
• Amphisbaenidae indet.^[102]
• Anguidae indet.
• Anguimorpha indet.^[105]
• Baenidae indet.^[102]
• Crocodylia indet.
• Crocodylidae indet.^[100]
• Emydidae indet.^[102]
• Gerrhonotinae indet.
• Glyptosaurinae indet.^[102]
• Helodermatidae indet.
• Iguania indet.
• Lacertilia indet.^[106]
• Squamata indet.
• Trionychidae indet.

Amphibians

• Caudata indet.

Fish

• Goniobasis carterii
• G. tenera
• Diplomystus sp.^[107]
• Lepisosteus sp.^[108]
• ?Notogoneus sp.^[107]
• Centrarchidae indet.^[107]
• aff. Amblyopsidae indet.^[107]
• Actinopterygii indet.^[108]

Invertebrates

Bivalves

• Asimina vesperalis^[109]
• Davidia antiqua^[110]
• Unio wasatchensis^[111]

Gastropods

• Viviparus paludinaeformis^[111]
• Ferrissia cf. minuta^[111]

Mollusks

• Mollusca indet.^[112]

Flora

• Allantodiopsis erosa^{[109] [113]}
• Allophylus flexifolia
• Ampelopsis acerifolia^[109]
• Beringiaphyllum cupanioides^[114]
• Carya antiquorum^[109]
• Castanea intermedia^[109]
• Cercidiphyllum arcticum^[109]
• Cissus marginata^[109]
• Dillenites garfieldensis^[109]
• Dombeya novimundi
• Ficus artocarpoides^[109]
• Ficus planicostata^[109]
• Fraxinus eocenica^[109]
• Hovenia cf. oregonensis
• Metasequoia occidentalis^[113]
• Nyssa alata^[109]
• Osmunda greenlandica^[109]
• Penosphyllum cordatum^[109]
• Platanus raynoldsi^[109]
• Platycarya americana
• Populus wyomingiana
• Prunus corrugis^[109]
• Rhamnus goldiana^[109]
• cf. Schoepfia republicensis
• Stillingia casca
• Syzygioides americana
• Ternstroemites aureavallis^[113]
• Zizyphus fibrillosus^[109]
• Alnus sp.
• Celtis sp.^[112]
• Cinnamomophyllum sp.^[115]
• Sloanea sp.^[115]
• Apocynaceae indet.^[115]
• Dicotyledonae indet.^[115]
• Lauraceae indet.^[115]
• cf. Magnoliales indet.^[115]

Ichnofossils

• Lunulichnus tuberosus^[116]
• Arenicolites^[33]
• Camborygma^[33]
• Celliforma^[33]
• Palaeophycus^[33]
• Planolites^[33]
• Rusophycus^[33]
• Scoyenia^[33]
• Skolithos^[33]
• Spongeliomorpha^[33]
• Taenidium^[33]
• Thalassinoides^[33]
• cf. Ophiomorpha^[33]

Herbivore expansion

The mammal fauna of the formation is part of the fourth phase of herbivore expansion spanning about 115 Ma from the Aptian to Holocene,^[117] and correlated with the Wind River and Wilcox Formations of the United States and the Laguna del Hunco Formation of Argentina.^[118]

Economic geology

Petroleum geology

The Wasatch Formation is a tight gas reservoir rock in the Greater Natural Buttes Field in the Uinta Basin of Utah and Colorado. The formation is characterized by porosity ranging from 6 to 20% and permeability of up to 1 mD. Based on 409 samples from the Wasatch Formation, average porosity is 8.75 percent and average permeability is 0.095 mD.^[119] The production rates after 2 years are 100–1,000 mscf/day for gas, 0.35–3.4 barrel per day for oil, and less than 1 barrel per day for water. The water:gas ratio ranges from 0.1 to 10 barrels per million standard cubic feet, indicating that free water is produced along with water dissolved in gas in the reservoir.^[120] Oil in the Bluebell-Altamont Field in the Uinta Basin and gas in the Piceance Creek Field in the Piceance Basin are produced from the Wasatch Formation.^[121]

As of May 2019, tight gas from the Wasatch Formation and underlying Mesaverde Group has been produced more than 1.76 trillion cubic feet (TCF) of gas from over 3,000 wells in the Uinta Basin, mostly from the Natural Buttes gas field in the eastern part of the basin. In the Piceance Basin, the Mesaverde Group and Wasatch Formation produced more than 7.7 TCF from over 12,000 wells, mostly from the central part of the basin.^[122]

Mining

Coal

Coal is mined from the Wasatch Formation in Wyoming. Together with the Fort Union Formation, the Wasatch Formation represents the thickest coal bed deposits in the state.^[123]

Uranium

See main article: Uranium mining in Wyoming. The fluvial sandstones contain uranium roll front deposits. The formation is the main producer of uranium in the state.^[124] Ore zones contain uraninite and pyrite. Oxidized ores include uranophane, meta-autunite, and phosphuranylite.^[125]

Wasatchian correlations

Wasatchian correlations in North America

Formation																						Ypresian (IUCS) • Itaboraian (SALMA) Bumbanian (ALMA) • Mangaorapan (NZ)
Basin		Piceance	Colorado Plateau	Wind River	Green River																	align=center rowspan=14
Copelemur	align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center
Coryphodon	align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center
Diacodexis	align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center
Homogalax	align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center
Oxyaena	align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center
Paramys	align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center
Primates	align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center
Birds	align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center
Reptiles	align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center
	align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center
Insects	align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center
	align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center		align=center
	Alluvial-fluvio-lacustrine	Fluvial				Fluvial	Fluvio-lacustrine	Fluvial	Lacustrine		Fluvio-lacustrine		Deltaic-paludal	Shallow marine		Fluvial	Shallow marine	Fluvial		Fluvial
Volcanic	Yes	No							Yes	No	Yes	No	Yes	No						Yes	No

See also

• List of fossiliferous stratigraphic units in Colorado
• List of fossiliferous stratigraphic units in Wyoming
• List of fossiliferous stratigraphic units in Utah
• Paleontology in Colorado
• Paleontology in Utah
• Paleontology in Wyoming
• 2014 West Salt Creek landslide

References

Bibliography

Geology publications

Maps

State maps

Quadrangle maps

Other maps

Paleontology publications

Notes and References

1. Shroba & Scott, 2001, p.3
2. http://www.fossilworks.org/cgi-bin/bridge.pl?action=displayStrata&geological_group=&formation=Wasatch&group_formation_member=Wasatch Wasatch Formation
3. Shroba & Scott, 2001, p.18
4. https://ngmdb.usgs.gov/Geolex/UnitRefs/WasatchRefs_11061.html Wasatch
5. https://www.uen.org/utah_history_encyclopedia/w/WASATCH_COUNTY.shtml Wasatch County
6. Van Cott, 1990, p.390
7. Bright, 2004, p.549
8. Web site: Desolation Canyon and Gray Canyon Stratigraphy. gotbooks.miracosta.edu.
9. Web site: Flaming Gorge National Recreation Area Stratigraphy. gotbooks.miracosta.edu.
10. https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=MTTw%3B0 Wasatch Formation - Montana
11. https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=UTT1%3B3 Wasatch Formation - Utah
12. https://gotbooks.miracosta.edu/gonp/coloradoplateau/lexicon/wasatch_group.htm Wasatch "Group"
13. Widmayer, 1977, p.18
14. Widmayer, 1977, p.105
15. Roehler, 1991, B16
16. http://www.fossilworks.org/cgi-bin/bridge.pl?action=collectionSearch&formation=Wasatch&member=%22Luman%20Tongue%22 Luman Tongue Member
17. http://www.fossilworks.org/cgi-bin/bridge.pl?action=collectionSearch&formation=Wasatch&member=%22Main%20Body%22 Main Body Member
18. Gunnells et al., 2016, p.984
19. Carrara, 2000, p.8
20. Whipkey et al., 1991, D1
21. Lorenz et al., 1996, p.3
22. Anderson et al., 2017
23. Whipkey et al., 1991, D5
24. Whipkey et al., 1991, D11
25. Whipkey et al., 1991, D15
26. Widmayer, 1977, p.11
27. Shroba & Scott, 2001, p.23
28. Sanborn, 1981, p.259
29. Widmayer, 1977, p.19
30. Pocknall, 1987, p.30
31. Anemone & Dirks, 2009, p.116
32. Pocknall, 1987, p.172
33. Zonneveld et al., 2006, p.88
34. Covert & Hamrick, 1993
35. Bown & Rose, 1987
36. West & Dawson, 1973
37. Muldoon & Gunnell, 2002
38. Honey, 1988
39. Gunnell et al., 2016, p.991
40. Gunnell, 1994
41. Beard, 1988
42. Gunnell et al., 2016, p.992
43. Bown, 1979
44. Gunnell et al., 2016, p.990
45. Holroyd & Rankin, 2014
46. Gazin, 1942
47. Gunnell, 2002
48. Roehler, 1991
49. Scott & Fox, 2005
50. Stucky & Krishtalka 1990
51. Krishtalka & Stucky, 1985
52. Stucky & Covert, 2014
53. Gunnell et al., 2016, p.1004
54. Gingerich, 1991
55. Zonneveld & Gunnell, 2003
56. Gunnell et al., 2016, p.1003
57. Dorr, 1978
58. Clyde et al., 1997
59. Froehlich, 2002
60. Gunnell et al., 2016, p.1001
61. Gazin, 1965
62. Polly, 1996
63. Morlo & Gunnell, 2003
64. Gunnell, 1998
65. Gingerich, 1982
66. Gunnell et al., 2016, p.1000
67. Guthrie, 1971
68. Roehler, 1987
69. Gunnell et al., 2016, p.989
70. Rankin & Holroyd, 2014
71. Gazin, 1956
72. Scott et al., 2002
73. Bown & Schankler, 1982
74. Secord, 2008
75. Gunnell et al., 2016, p.999
76. Korth, 1984
77. Gunnell et al., 2016, p.998
78. Black & Sutton, 1984
79. Anemone et al., 2012
80. Rose, 1981
81. Gazin, 1962
82. Gunnell et al., 2016, p.987
83. Savage et al., 1972
84. Gunnell et al., 2016, p.985
85. Hamrich & Covert, 1991
86. Gunnell et al., 2016, p.994
87. Lucas, 1998
88. Thewissen, 1990
89. Gunnell et al., 2016, p.995
90. Alroy, 2002
91. Williamson & Lucas, 1992
92. Schoch & Lucas, 1981
93. Gunnell et al., 2016, p.984
94. Schoch, 1986
95. Wetmore, 1931
96. Stidham, 2014
97. Holroyd & Strait, 2008
98. Smith & Gauthier, 2013
99. Hay, 1908
100. Zonneveld et al., 2000
101. Sullivan, 1979
102. Gunnell & Bartels, 2002
103. Hutchison, 1991
104. West, 1973
105. Strait et al., 2016
106. Smith & Holroyd, 2003
107. Divay & Murray, 2016
108. Foster, 2001
109. Brown, 1962
110. Manchester, 2002
111. Yen, 1948
112. Dorr & Steidtmann, 1970
113. Wilf, 2000
114. Manchester et al., 1999
115. Wilf et al., 2006
116. Zonneveld et al., 2006, p.90
117. Labandeira, 2006, p.421
118. Labandeira, 2006, p.434
119. Nelson & Hoffman, 2009, p.8
120. Nelson & Hoffman, 2009, p.5
121. Sanborn, 1981, p.260
122. Drake II et al., 2019, p.1
123. https://www.wsgs.wyo.gov/energy/coal-geology.aspx Wyoming's Coal Geology
124. Langden, 1973
125. Heinrich, 1958