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11.9" Triceratops Nose Horn - Bowman, North Dakota
This is a fossil Triceratops nose horn collected from our partners' lease in the Late Cretaceous Hell Creek Formation near Bowman, North Dakota last year, making it about 66 million years old. It comes with the pictured metal display stand.
This gorgeous specimen is quite stable with relatively small amounts of crack repaired and restoration. The most notable restoration is between the proximal end of the horn and the nasal bridge. There appears to be a repaired crack between the proximal end of the horn and the upper beak. A unique feature to this specimen is an unexplained, indented line that goes across the anterior-proximal portion of the horn. This line can be seen in the above pictures.
This gorgeous specimen is quite stable with relatively small amounts of crack repaired and restoration. The most notable restoration is between the proximal end of the horn and the nasal bridge. There appears to be a repaired crack between the proximal end of the horn and the upper beak. A unique feature to this specimen is an unexplained, indented line that goes across the anterior-proximal portion of the horn. This line can be seen in the above pictures.
About Triceratops
Triceratops is one of the most recognized and intriguing of the North American ceratopsid dinosaurs. They stomped around the Late Cretaceous (around 68-66 mya), brandishing their three-pronged and bony frilled skulls, chewing on fibrous plants. They struggled against large predators, stood their ground, and tried not to be devoured by the ferocious Tyrannosaurus rex.
An artist's rendering of Triceratops.
The head on a Triceratops may have been an intimidating show rather than a stabbing, defensive trident and imposing shield for inter-species jousting. Researchers have given close scrutiny to the holes, or fenestrae, of other ceratopsid crests. In the past, the holes within the shield were used to confirm separate species.
Individual Triceratops are estimated to have reached up to 9 meters (29.5 feet) in length, 3 meters (9.8 feet) in height, and weighed up to 26,000 pounds. The largest known skull is estimated to have been 2.5 meters (8.2 feet) long and would have extended almost a third of the length of the mature individual. The pointed horns were approximately 1 meter (3 feet) long. With its sturdy build and powerful legs, Triceratops could have ripped open the predator that wanted this herbivore for dinner.
One of the most abundant of the large Cretaceous fauna, Triceratops plucked low growth with its beak-tipped jaws. Triceratops teeth were arranged in groups, called batteries, of 36 to 40 tooth columns, in each side of each jaw. Each column contained about 3 to 5 stacked teeth, depending on the individual’s size. This produced a range of 432 to 800 teeth, of which only a fraction were in use at any given time (due to tooth replacement). The great size and quantity of teeth suggests that they ate large volumes of fibrous plants. These were possibly palms, cycads, and ferns.
Closeup of the jaws and teeth of Triceratops.
Triceratops was designated as the state fossil of South Dakota in 1988.
Triceratops is one of the most recognized and intriguing of the North American ceratopsid dinosaurs. They stomped around the Late Cretaceous (around 68-66 mya), brandishing their three-pronged and bony frilled skulls, chewing on fibrous plants. They struggled against large predators, stood their ground, and tried not to be devoured by the ferocious Tyrannosaurus rex.
An artist's rendering of Triceratops.
The head on a Triceratops may have been an intimidating show rather than a stabbing, defensive trident and imposing shield for inter-species jousting. Researchers have given close scrutiny to the holes, or fenestrae, of other ceratopsid crests. In the past, the holes within the shield were used to confirm separate species.
Individual Triceratops are estimated to have reached up to 9 meters (29.5 feet) in length, 3 meters (9.8 feet) in height, and weighed up to 26,000 pounds. The largest known skull is estimated to have been 2.5 meters (8.2 feet) long and would have extended almost a third of the length of the mature individual. The pointed horns were approximately 1 meter (3 feet) long. With its sturdy build and powerful legs, Triceratops could have ripped open the predator that wanted this herbivore for dinner.
One of the most abundant of the large Cretaceous fauna, Triceratops plucked low growth with its beak-tipped jaws. Triceratops teeth were arranged in groups, called batteries, of 36 to 40 tooth columns, in each side of each jaw. Each column contained about 3 to 5 stacked teeth, depending on the individual’s size. This produced a range of 432 to 800 teeth, of which only a fraction were in use at any given time (due to tooth replacement). The great size and quantity of teeth suggests that they ate large volumes of fibrous plants. These were possibly palms, cycads, and ferns.
Closeup of the jaws and teeth of Triceratops.
Triceratops was designated as the state fossil of South Dakota in 1988.
Because of its age and sedimentary composition, the Hell Creek Formation has become one of the most paleontologically studied areas in the world. 158 genera of animals and 64 genera of plants are known from the formation and new discoveries are made frequently. In addition to Tyrannosaurs, Ceratopsids, and Hadrosaurs, the formation has yielded remains of amphibians, reptiles, lizards, snakes and turtles, fish and sharks, avian and non-avian dinosaurs, and mammals. The Hell Creek Formation gives the most complete understanding of the environment just before the Cretaceous-Paleogene extinction.
SPECIES
Triceratops horridus
LOCATION
Bowman County, North Dakota
FORMATION
Hell Creek Formation
SIZE
11.9 x 9.6", 13.7" on stand
CATEGORY
SUB CATEGORY
ITEM
#131351
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