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Cedar Mountain Formation facts for kids

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Cedar Mountain Formation
Stratigraphic range: Late Berriasian-Cenomanian
~140–95Ma
Type Geological formation
Unit of Dakota Group
Sub-units See text
Underlies Naturita Formation
Overlies Morrison Formation
Thickness Varies, some sections over 1000 metres
Lithology
Primary Conglomerate, sandstone, mudstone
Location
Coordinates 39°15′00″N 110°49′05″W / 39.250°N 110.818°W / 39.250; -110.818
Approximate paleocoordinates 40°12′N 69°00′W / 40.2°N 69.0°W / 40.2; -69.0
Region  Utah
Country  United States
Type section
Named for Cedar Mountain
Named by Stokes
Year defined 1944

The Cedar Mountain Formation is a special type of rock layer found in eastern Utah. It's named after Cedar Mountain, where it was first studied in 1944 by William Lee Stokes. This formation is important because it holds many fossils, especially dinosaurs, from a time long ago.

What is the Cedar Mountain Formation?

CMF-oucrop
The drab-colored lower part of the Cedar Mountain Formation, sitting on top of the brighter Morrison Formation.

This rock formation is made of sediments that were laid down on land, not in the ocean. Imagine ancient rivers, lakes, and floodplains – that's where these rocks formed! Scientists believe the Cedar Mountain Formation was created during the last half of the Early Cretaceous period, about 127 to 98 million years ago. We know this thanks to radiometric dating, which is a way to figure out the age of rocks using natural radioactivity.

The Cedar Mountain Formation sits between two other rock layers: the Morrison Formation below it and the Naturita Formation above it.

Layers of the Formation

CMF-stratcol-revised
This chart shows the different layers (members) that make up the Cedar Mountain Formation and how old they are. Some layers might be missing because they were never deposited or were worn away later.

The Cedar Mountain Formation is made up of several smaller layers, called "members." Scientists sometimes disagree on whether there are four or five members. Most agree that the Buckhorn Conglomerate is the very bottom layer. Above it are the Yellow Cat Member, Poison Strip Sandstone, Ruby Ranch Member, and the Mussentuchit Member. Each of these layers tells us something different about the ancient environment.

Buckhorn Conglomerate

This is the lowest layer of the Cedar Mountain Formation. It's named after the Buckhorn Reservoir. It's made of conglomerate, which is rock made of rounded pebbles and stones cemented together.

Yellow Cat Member

This layer is named after the Yellow Cat mining area, near Arches National Park. It's mostly made of dull gray mudstones, which are rocks formed from ancient mud. These mudstones show signs of old soils, meaning the area was once a floodplain with rivers. This layer is thought to be about 140 to 133 million years old.

Poison Strip Sandstone

Named for the Poison Strip uranium area, this layer has prominent sandstone cliffs. It formed from ancient river channels, with some mud and limestone from floodplains and small ponds. This layer is famous for "Tony's Bone Bed."

  • Tony's Bone Bed: This is a very important spot where many dinosaur bones were found in 1998. The bones were not connected, and some looked like they had been trampled or chewed by scavengers. This suggests the bones gathered slowly over time, perhaps during dry seasons when river water was low.

Ruby Ranch Member

This is the most widespread and easy-to-spot layer of the Cedar Mountain Formation. It's named after the Ruby Ranch. It's mostly maroon-colored mudstones with round, hard lumps called carbonate nodules. These nodules formed in ancient soils during a time when the climate was dry with strong seasons. The rivers in this period flowed northeast, towards an ancient sea.

Mussentuchit Member

This is the top layer of the Cedar Mountain Formation, named after Mussentuchit Wash. It's mostly gray mudstones with lots of fossilized plant material and volcanic ash. This suggests it was a wet coastal plain with plenty of rain. This layer is about 104 to 98 million years old.

Fossils Found Here

The Cedar Mountain Formation is a treasure chest of Early Cretaceous fossils, especially dinosaurs! Scientists have only really started studying these fossils since the 1990s. The discoveries here are helping us understand how dinosaurs changed over time and how the North American continent moved.

Dinosaurs

CMF-dinos
Example of dinosaurs from the Cedar Mountain Formation include the armored Gastonia (top left), the fierce Utahraptor (top right), a large meat-eating dinosaur tooth (bottom left), and the plant-eating Tenontosaurus (bottom right).

Scientists have found at least two, and possibly three, different groups of dinosaurs in the Cedar Mountain Formation.

The older dinosaurs, found in the Yellow Cat, Poison Strip, and lower Ruby Ranch layers, include dinosaurs like Nedcolbertia (a small meat-eater) and Cedarosaurus (a long-necked plant-eater). Other dinosaurs like the armored Gastonia and an unnamed iguanodontid are similar to dinosaurs found in England from the same time. This tells us that North America and Europe were still connected back then.

However, the younger dinosaurs, found in the upper Ruby Ranch and Mussentuchit layers, are more like dinosaurs found in Asia! For example, the armored Cedarpelta is related to dinosaurs from Mongolia. This shows that as the North American continent drifted westward, it eventually connected with Asia, bringing new types of dinosaurs. This upper group also includes early tyrannosaurs, ceratopsians (horned dinosaurs), and pachycephalosaurs (dome-headed dinosaurs).

Armored Dinosaurs (Ankylosaurs)

Armored Dinosaurs from the Cedar Mountain Formation
Genus Species Member What was found Notes Images
Animantarx Animantarx ramaljonesi Mussentuchit Member Part of a skull and skeleton.
Gastonia burgei dinosaur
Gastonia burgei
Cedarpelta Cedarpelta bilbeyhallorum Mussentuchit Member Skull and body bones.
Gastonia Gastonia burgei Upper Yellow Cat Member Two skulls, two partial skulls, and four or five partial skeletons.
G. lorriemcwhinneyae Ruby Ranch Member
Peloroplites Peloroplites cedrimontanus Mussentuchit Member
Sauropelta Indeterminate Ruby Ranch Member

Beaked Dinosaurs (Neornithischians)

Beaked Dinosaurs from the Cedar Mountain Formation
Genus Species Member What was found Notes Images
Cedrorestes Cedrorestes crichtoni Upper Yellow Cat Member
Eolambia restoration
Eolambia
Life restoration of Hippodraco
Hippodraco
Life restoration of Iguanacolossus
Iguanocolossus
Deinonychus (Raptor Prey Restraint)
Zephyrosaurus being attacked by a Deinonychus
Eolambia Eolambia caroljonesa Mussentuchit Member
Hippodraco Hippodraco scutodens Upper Yellow Cat Member
Iguanacolossus Iguanacolossus fortis Lower Yellow Cat Member
Iguanodon Iguanodon ottingeri Teeth. Doubtful.
Planicoxa Planicoxa venenica Poison Strip Member Connected body bones.
Tenontosaurus Tenontosaurus tiletti Mussentuchit Member Most common beaked dinosaur in the area.
Indeterminate Ruby Ranch Member Most common beaked dinosaur in the area.
Zephyrosaurus Zephyrosaurus schaffi Mussentuchit Member

Long-necked Dinosaurs (Sauropods)

Long-necked Dinosaurs from the Cedar Mountain Formation
Genus Species Member What was found Notes Images
Abydosaurus Abydosaurus mcintoshi Mussentuchit Member
Abydosaurus NT
Abydosaurus
Brontomerus utahraptor2
Brontomerus
Moabosaurus utahensis restoration
Moabosaurus
cf. Astrodon Indeterminate Ruby Ranch Member.
Brontomerus Brontomerus mcintoshi Ruby Ranch Member
Cedarosaurus Cedarosaurus weiskopfae Upper Yellow Cat Member Body skeleton.
Mierasaurus Mierasaurus bobyoungi Lower Yellow Cat Member
Moabosaurus Moabosaurus utahensis Poison Strip Member Remains of at least 18 partial individuals.
Venenosaurus Venenosaurus dicrocei Poison Strip Member Partial body skeleton.

Meat-eating Dinosaurs (Theropods)

Meat-eating Dinosaurs from the Cedar Mountain Formation
Genus Species Member What was found Notes Images
cf. Acrocanthosaurus Indeterminate Ruby Ranch Member.
Falcarius Restoration
Falcarius
Geminiraptor NT
Geminiraptor
Moros intrepidus reconstruction
Moros
Nedclobertia
Nedcolbertia
Siats reconstruction
Siats
Yurgovuchia
Yurgovuchia
Deinonychus Indeterminate Mussentuchit Member.
Falcarius Falcarius utahensis Lower Yellow Cat Member.
Geminiraptor Geminiraptor suarezarum Lower Yellow Cat Member.
Martharaptor Martharaptor greenriverensis Upper Yellow Cat Member.
Moros Moros intrepidus Mussentuchit Member.
Nedcolbertia Nedcolbertia justinhofmanni Upper Yellow Cat Member. Partial skeletons of three individuals.
cf. Richardoestesia Indeterminate Mussentuchit Member.
Siats Siats meekerorum Mussentuchit Member. Partial body skeleton of a young individual.
Utahraptor Utahraptor ostrommaysi Upper Yellow Cat Member. Skull and body fragments.
Indeterminate Poison Strip Member.
Yurgovuchia Yurgovuchia doellingi Lower Yellow Cat Member.

Other Fossils

CMF-utah
Map of Utah showing the location of the Cedar Mountain Formation (red).

Besides dinosaurs, the Cedar Mountain Formation has many tiny fossils, mostly teeth from different animals. These "microfossils" are found by washing rock through screens.

  • Fish: Scientists have found teeth from ancient freshwater sharks (like Hybodus), rays, lungfish (Ceratodus), and other bony fish. Lungfish are cool because they can breathe air when water has low oxygen!
  • Amphibians: Some salamanders and frogs have been found, but they are rare.
  • Reptiles: Many reptile fossils are present, including aquatic turtles (Glyptops, Naomichelys), at least one type of snake (Coniophis), and several different lizards. Crocodiles are also found, but only in pieces. There's even a fragment of a large flying reptile called a pterosaur.
  • Birds: Bird fossils are very rare because their bones are delicate. At least one ancient aquatic bird has been found.
  • Mammals: Many small mammal fossils have been discovered, including early types of mammals like triconodonts, symmetrodonts, multituberculates, and even one of the earliest marsupials (Kokopellia).

Other types of fossils include:

  • Charophytes: These are distinctive structures from freshwater algae. They are so unique that they help scientists match rock layers of similar ages.
  • Ostracods: These are tiny crustaceans with shells that look like clams.
  • Pollen: Found in the Mussentuchit Member, pollen helps scientists figure out what the environment was like long ago.
  • Petrified Wood: In some places, large petrified (fossilized) logs are found, especially in the Poison Strip. These logs are from ancient conifer trees that were over 30 meters (100 feet) tall! The unique wood of the tree fern Tempskya is also sometimes found.

Other Reptiles

Fragments of pterosaurs (flying reptiles) have been found in the Mussentuchit Member.

Crocodilians
Crocodilians of the Cedar Mountain Formation
Genus Species Member What was found Notes Images
cf. Bernissartia cf. Bernissartia sp. Mussentuchit Member
Bernissartia BW
Bernissartia
Dakotasuchus Dakotasuchus kingi Mussentuchit Member.
Lizards and Snakes
Lizards and Snakes of the Cedar Mountain Formation
Genus Species Member What was found Notes Images
Toxolophosaurus Toxolophosaurus sp. Yellow Cat Member.
Harmodontosaurus Harmodontosaurus emeryensis Mussentuchit Member.
Dimekodontosaurus Dimekodontosaurus madseni Mussentuchit Member.
Dicothodon Dicothodon moorensis Mussentuchit Member.
Pseudosaurillus Pseudosaurillus sp. Mussentuchit Member.
Bicuspidon Bicuspidon numerosus Mussentuchit Member.
Bothriagenys Bothriagenys mysterion Mussentuchit Member.
Primaderma Primaderma nessovi Mussentuchit Member.
Coniophis Coniophis sp. Mussentuchit Member.
Turtles
Turtles of the Cedar Mountain Formation
Genus Species Member What was found Notes Images
Glyptops Glyptops sp. Yellow Cat Member, Mussentuchit Member
Left posterior Baenid turtle pleurals and peripherals
Peripherals
Naomichelys Naomichelys sp. Mussentuchit Member.
gen. nov. sp. nov. Yellow Cat Member

Amphibians

Amphibians of the Cedar Mountain Formation
Genus Species Member What was found Notes Images
Albanerpeton Albanerpeton cf. A. nexuosus Mussentuchit Member
Albanerpeton BW
Albanerpeton

Fish

Bony Fish
Bony Fish of the Cedar Mountain Formation
Genus Species Member What was found Notes Images
Semionotus? Semionotus? sp. Yellow Cat Member
Semionotus
Semionotus
Ceratodus
Ceratodus
Ceratodus C. kempae Yellow Cat Member
C. kirklandi Yellow Cat Member
C. molossus Mussentuchit Member
Cartilaginous Fish
Cartilaginous Fish of the Cedar Mountain Formation
Genus Species Member What was found Notes Images
Hybodus Hybodus sp. Ruby Ranch Member, Mussentuchit Member
Hybodus NT
Hybodus
Polyacrodus Polyacrodus parvidens Mussentuchit Member
Lissodus Lissodus sp. Mussentuchit Member
Ischyrhiza Ischyrhiza sp. Mussentuchit Member
Pseudohypolophus Pseudohypolophus sp. Mussentuchit Member
cf. Baibisha New species Mussentuchit Member
Cretorectolobus Indeterminate Mussentuchit Member

Mammals

Mammals of the Cedar Mountain Formation
Genus Species Member What was found Notes Images
Ameribaatar Ameribaatar zofiae Mussentuchit A type of early mammal called a multituberculate.
Astroconodon Astroconodon delicatus Mussentuchit A meat-eating triconodont.
Bryceomys Bryceomys intermedius Mussentuchit Another type of multituberculate.
Cedaromys Cedaromys bestia Mussentuchit
Cedaromys parvus Mussentuchit
Cifelliodon Cifelliodon wahkermoosuch Yellow Cat Member An early mammal-like animal.
Corviconodon Corviconodon utahensis Mussentuchit
Dakotadens Dakotadens pertritus Mussentuchit
Janumys Janumys erebos Mussentuchit
Jugulator Jugulator amplissimus Mussentuchit
Kokopellia Kokopellia juddi Mussentuchit Possibly one of the earliest marsupials.
Paracimexomys Paracimexomys perplexus Mussentuchit
Paracimexomys robisoni Mussentuchit
Spalacolestes Spalacolestes cretulablatta Mussentuchit
Spalacolestes inconcinnus Mussentuchit
Spalacotheridium Spalacotheridium noblei Mussentuchit

Images for kids

See also

Kids robot.svg In Spanish: Formación Cedar Mountain para niños

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