Carmel Formation

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Carmel Formation
Stratigraphic range: Bajocian–Callovian
Temple Cap Formation, Nugget Sandstone
ThicknessFrom 200 feet (60 m) to 1,000 feet (300 m)[1]
Lithology
PrimaryMudstone
OtherSandstone, siltstone, limestone
Location
Coordinates37°15′04″N 112°39′47″W / 37.251°N 112.663°W / 37.251; -112.663
RegionWyoming, Utah, Colorado, north east Arizona and New Mexico
CountryUS
Type section
Named forMount Carmel
Named byGilluly and Reeside
Year defined1928
Carmel Formation is located in the United States
Carmel Formation
Carmel Formation (the United States)
Carmel Formation is located in Utah
Carmel Formation
Gunlock Reservoir
, southwestern Utah
Carmel Formation near Gunlock, Utah. The unconformably overlying dark unit is the Upper Cretaceous Iron Springs Formation.

The Carmel Formation is a

geologic formation in the San Rafael Group that is spread across the U.S. states of Wyoming, Utah, Colorado, north east Arizona and New Mexico. Part of the Colorado Plateau, this formation was laid down in the Middle Jurassic during the late Bajocian, through the Bathonian and into the early Callovian stages.[2]

Description

The Carmel Formation consists of up to 1,000 feet (300 m) of

Entrada Formation.[3]

In the type area of southern Utah, the Carmel Formation is divided into the Judd Hollow Member, a basal limestone member; the Crystal Creek Member, mostly mudstone and siltstone, which grades into the Page Sandstone to the east; the Paria River Member, which is also siltstone and mudstone but is separated from the Crystal Creek Member by gypsum beds; and the Winsor Member, which is mudstone, sandstone, and siltstone separated from the Paria River by a basal limestone. Further east, the limestone marker bed pinches out, and the Winsor Member and Paria River Member become indistinguishable and are informally termed the upper member. The upper member contains

volcaniclastic beds of rhyolite originating in a volcanic arc just off the edge of the Colorado Plateau.[4]

The formation preserves a Jurassic

hardground, rare for North America.[5]

Subunits

Members (alphabetical):

(Asterisks mean the name is used by the

US Geological Survey)[9]

History of investigation

rock formation in Capitol Reef National Park. Though the park is famous for white domes of the Navajo Sandstone
, this dome's color is a result of a lingering section of yellow Carmel Formation carbonate, which has stained the underlying rock.

In 1928 Gilluly and Reeside stated an intent to name the formation after the village of Mount Carmel, Utah but did not give a type locality. They noted it as a basal formation in the San Rafael Group in San Rafael Swell, in Emery County, Utah.[10] An overview along with a type locality and source of name was stated by Gregory and Moore in 1931.[11] Mackin revised the formation's description and assigned the Homestake Limestone Member to it in 1954.[12] Harshbarger and others created an overview in 1957.[13] Its eastern areal limits were described by Wright and others in 1962.[14] In 1963, western areal limits along with an overview were completed by Schultz and Wright.[15] Another revision was done by Phoenix in 1963 who also added a Judd Hollow Tongue member.[16] Isotopic dating was conducted by Marvin and others in 1965. The Kolob, Crystal Creek, Paria River, Winsor, and Wiggler Wash members were assigned by Thompson and Stokes in 1970. Areal limits were adjusted by O'Sullivan and Craig in 1973[17] and again in 1983 by Blakey and others.[3] An overview was completed by Chapman in 1989.[4] Hintze and others conducted isotopic dating and created an overview in 1994.[18]

Paleontological finds

There have been a number of paleontological finds within the Carmel Formation. Among these have been

dinosaur footprints.[20]

Hardground mollusc community

The formation preserves a rare Jurassic hardground interpreted as a carbonate

bivalves such as Liostrea, Plicatula, and Modiolus. The ichnofossil Gastro‐chaenolites is present, often with fossils of Lithophaga preserved inside. The rare bryozoan Arachnidium is found in attachment scars of Liostrea. Though bivalves were abundant, the community is lacking in the diversity seen in other Jurassic hardgrounds, suggesting a restricted shelf environment.[5]

Bryozoans

Bryozoans found within the Carmel Formation include seven species of calcareous

ctenostome bryozoan.[19]

Gallery


  • Cross-section of a carbonate hardground encrusted by oysters and bored by bivalves (Gastrochaenolites)
    Cross-section of a carbonate
    bivalves (Gastrochaenolites
    )
  • Biosparite/grainstone with crinoid columnals (Isocrinus nicoleti) from the Carmel Formation at Mount Carmel Junction, Utah.
    Mount Carmel Junction
    , Utah.
  • Ripplemarks in a biosparite/grainstone from the Carmel Formation, southwestern Utah.
    Ripplemarks in a
    biosparite
    /grainstone from the Carmel Formation, southwestern Utah.
  • Ooids and crinoid columnals (Isocrinus nicoleti) on the surface of Carmel Formation limestone.
    Ooids
    and crinoid columnals (Isocrinus nicoleti) on the surface of Carmel Formation limestone.
  • Ostreolith ("oyster ball") from the Carmel Formation, southwestern Utah.
    Ostreolith ("oyster ball") from the Carmel Formation, southwestern Utah.
  • Trace fossil Gyrochorte from the Carmel Formation (Middle Jurassic) of SW Utah.
    Trace fossil Gyrochorte from the Carmel Formation (Middle Jurassic) of SW Utah.

Places found

Geologic Province:[9]

References

  1. ^ a b "Carmel Formation (in San Rafael Group)". 6 September 2015. Archived from the original on 4 March 2016. Retrieved 6 September 2015.
  2. ^
    doi:10.3133/pp1035B
    .
  3. ^ a b c Blakey, R.C.; Peterson, Fred; Caputo, M.V.; Voorhees, B.J.; Geddes, D.J.; Geesaman, R.C. (1983). "Paleogeography of Middle Jurassic continental, shoreline, and shallow marine sedimentation, southern Utah". Society of Economic Paleontologists and Mineralogists, Rocky Mountain Section, Rocky Mountain Paleogeography Symposium. 2: 77–100. Retrieved 26 October 2021.
  4. ^
    doi:10.1130/0091-7613(1989)017<0281:IORIBI>2.3.CO;2
    .
  5. ^
    doi:10.1080/10420949409386375
    .
  6. ^ a b Doelling, H.H.; Davis, F.D. (1989). "The geology of Kane County, Utah". Utah Geological and Mineral Survey Bulletin. 124. Retrieved 25 October 2021.
  7. hdl:2346/64975
    .
  8. ^ a b c Thompson, A.E.; Stokes, W.L. (1970). "Stratigraphy of the San Rafael Group, southwest and south central Utah". Utah Geological and Mineral Survey Bulletin. 87.
  9. ^ a b GEOLEX database entry for Carmel, USGS (viewed 20 March 2006)
  10. doi:10.3133/pp150D
    .
  11. hdl:2027/uc1.32106006462755
    .
  12. doi:10.3133/mf14
    .
  13. doi:10.3133/pp291
    .
  14. doi:10.1306/BC74394B-16BE-11D7-8645000102C1865D
    .
  15. doi:10.3133/pp450E
    .
  16. doi:10.3133/b1137
    .
  17. doi:10.3133/pp525B
    .
  18. ^ Hintze, L.F.; Anderson, R.E.; Embree, G.F. (1994). "Geologic map of the Motoqua and Gunlock quadrangles, Washington County, Utah". U.S. Geological Survey Miscellaneous Investigations Series Map. I-2427. Retrieved 26 October 2021.
  19. ^
    doi:10.1017/S0022336000040671
    .
  20. doi:10.1080/10420949809386424
    .
  21. ^ a b O'Sullivan, R.B.; Craig, L.C. (1973). "Jurassic rocks of northeast Arizona and adjacent areas" (PDF). New Mexico Geological Society Field Conference Guidebook. 24: 79–85. Retrieved 25 October 2021.
  22. ^ Rowley, P.D.; Hansen, W.R. (1979). "Geologic map of the Plug Hat quadrangle, Moffat County, Colorado". U.S. Geological Survey Geologic Quadrangle Map. GQ-1514. Retrieved 25 October 2021.

External links

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