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State Fossils
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Utah State Fossil
Theropod Dinosaur
(Allosaurus fragilis)
Adopted in 1988.
The Theropod Dinosaur, Allosaurus fragilis, was designated the State Fossil in 1988. There are different
meanings of the word allosaurus, "Different Lizard" and "Strange Reptile," are two examples. Allosaurus was a carnosaur,
one of the groups of theropod meat-eaters. This animal was large and probably too bulky to move at speed over any
distance, however, the large sauropods and stegosaurs on which it fed were not fast-moving themselves.
Description of the Utah State Fossil
One of the largest Jurassic Carnosaurs of North America. An average Allosaurus weighed about 4 tons (3.6 metric
tons) and measured 35 feet (10.5 m) from the tip of its nose to the end of its TAIL. The largest known was 45 feet
(13.5 m) long. When Allosaurus stood upright, it was 16.5 feet (5 m) tall.
Allosaurus was a carnivorous "lizard-hipped" dinosaur or theropod. It had a bony red crest above each eye, a
strong s-shaped neck. Its teeth were 5-10 cm long and curved backward with serrated front and back edges. Allosaurus'
strong back and neck aided its jaws in tearing off chunks of flesh.
Like all Theropods, Allosaurus Walked on two legs with its heavy tail stretched out behind for balance. Its strong
legs were built for speed; they had powerful muscles and heavy bones. Although its arms were short, each finger
on its three-fingered hands was armed with a sharp claw that could be up to 6 inches (15 cm) long. The three long
toes on its feet were equipped with eagle-like talons.
This meat eater had a strong neck. Its huge 3-foot (90 cm) long head had heavy bony knobs, or ridges, above its
eyes; its enormously powerful jaws were filled with saber-like teeth 2 to 4 inches (5 to 10 cm) long. The jaws were
hinged like those of a snake, so Allosaurus would have been able to swallow huge hunks of meat whole. Scientists
have found APATOSAURUS vertebrae with Allosaurus tooth marks on them, evidence of a Jurassic feast! Although not
really built for speed, it had two sturdy legs and a powerful tail. It was a fearsome predator of its time.
The genus Allosaurus is based on the virtually complete skeleton discovered by M. P. Felch in 1883.
More than 60 complete and partial Allosaurus skeletons have been recovered from the Morrison Formation between Wyoming
and New Mexico, in the USA. It is the largest and most common carnivore found in these widespread deposits. At the
Cleveland Lloyd Quarry in Utah, USA, Allosaurus is by far the most numerous fossil type and is represented by at
least 44 individuals. These ranged in size from adults to juveniles.
Geologic Time
145 to 150 million years ago (Late Jurassic)
Geographic Range
Wyoming, Montana, Colorado, New Mexico, South Dakota, Utah, and Oklahoma
Characteristics:
Allosaurus was the most common large carnivore of the Late Jurassic in North America. It
was a smaller predecessor of the Cretaceous Tyrannosaurus. Strong forelimbs with sharp claws, powerful hind legs
and recurved, dagger-like teeth are evidence that Allosaurus was a formidable predator. Although it was much smaller
than sauropods like Apatosaurus (Brontosaurus), which were also common at the time, quite possibly Allosaurus hunted
in packs to bring down larger prey. Like many meat eaters, it may also have been a scavenger.
Many Allosaurus specimens representing individuals of different ages have been recovered in exposures of the Morrison
Formation in the Rocky Mountain West. This specimen is interpreted as a subadult.
Adult Weight: 1.5 - 2 tons
Adult Length: 30 - 40 ft long
Habitat: Plains and lowlands
Diet: Meat
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State Fossils
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Most US states have made a state fossil designation, in many
cases during the 1980s. It is common to designate one species in which fossilization has
occurred, rather than a single specimen, or a category of fossils not limited to a single
species.
Some states that lack a "state fossil" have nevertheless singled out a fossil for formal
designation such as a state dinosaur, rock, gem or stone.
fossil (fŏs'əl)
n.
1. A remnant or trace of an organism of a past geologic age, such as a skeleton or
leaf imprint, embedded and preserved in the earth's crust.
2. One, such as a rigid theory, that is outdated or antiquated.
adj.
1. Characteristic of or having the nature of a fossil.
2. Being or similar to a fossil.
3. Belonging to the past; antiquated.
[From Latin fossilis, dug up, from fossus, past participle of fodere, to dig.]
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