This dinosaur species was first known from a single partial horn, which
Marsh named Bison alticornis in 1889. John Bell
||The three distinctive facial horns and the frill-like fan
on the back of the skull make this dinosaur species one of the most
widely recognized fossils. The animal's large size - up to 8.7 yards (8 meters) long and about 8,800 to 11,000 pounds (4,000 to 5,000 kilograms) in weight for adults - combine to make this dinosaur fossil quite impressive.
Triceratops is known from eastern and western Wyoming, eastern Montana,
southwestern North Dakota, central Colorado,
Alberta and Saskatchewan in Canada, and northwestern South Dakota. In South Dakota, Triceratops specimens have been
found in Harding, Perkins, Corson, Dewey, Ziebach, Meade, and Butte counties.
This species is known by at least 50 complete or partial skulls and
some partial skeletons. The skulls demonstrate a wide
range of features, which is in part due to individual genetic variation, the oddities of preservation, and, perhaps, sexual
differences. No bonebeds have been found and juvenile material is not common.
How Old Are Triceratops Fossils?
The South Dakota Triceratops fossils have been found in rocks from the
Hell Creek Formation in the northwestern part of
the state. These fossils are from late in the Cretaceous Period, and are about 66 to 68 million years old.
Our knowledge of the natural history of fossil creatures comes from
the study of the geological deposits in which the
specimens were found and from analyses of the anatomical structures of the fossilized remains.
The sedimentary rocks that preserve the bones of Triceratops are typical
of coastal lowlands similar to that ranging from
the present southeastern Atlantic Coast and the Gulf Coast of the United States. Bald cypress and sequoia-like conifers,
ferns, cycads , palms, and many shrubs of flowering plants dominated this environment. The shrubs and ferns may have been
the primary sources of food for Triceratops .
The Triceratops skull was very distinctive, with two brow horns and
a single nasal horn. The latter was considerably
shorter than the brow horns. The eye socket was very large, suggesting that sight may have been an important sense to the
animal. The eyes were directed to the sides of the animal to widen the field of view.
In adults, the back of the head had a fan-like frill of very thick bone that served to protect the neck and give the animal the
appearance of being much larger when viewed from the front. Powerful jaw-closing muscles may have attached to the frill
as well. The neck ligaments and muscles were attached to the base of the frill above the opening for the spinal cord. The
outer edge of the frill had small triangular bones to give the frill a saw-toothed appearance. Skulls ranged in size from very
small baby skulls up to adult skulls 2.7 yards (2.5 meters) in length.
The beak, or mouth, of the animal was very well developed to aid in
the attachment of a tough turtle-like beak material. This
tough beak permitted Triceratops to snap off tough vegetation. The cheek teeth were crowded together to form a scissor-like
structure that could slice most vegetation that the animal encountered.
These animals had 10 neck vertebrae , 12 vertebrae between neck and
pelvis, 10 sacral vertebrae, and perhaps as many as
50 tail vertebrae (see Figure 1). The tail probably was held up off the ground.
Triceratops were obligatory quadrupeds , that is, their anatomy was
such that they needed to use all four legs in order to
walk. The front legs were not completely drawn under the body, but the rear ones were. The front feet had five toes each.
The pelvis was a massive structure, firmly attached to 10 sacral vertebrae. The hind legs were very robust, longer than the
fore legs, and each hind foot had four functional toes.
Triceratops is one of the most famous species of dinosaurs known, and
skeletons of the species are found in most
paleontology museums. A nearly complete Triceratops horridus skull was found in Harding County, South Dakota in 1927.
However, the species was not proclaimed the State Fossil of South Dakota by the legislature until February 14, 1989. The
Harding County specimen is on display in the Museum of Geology at the S.D. School of Mines and Technology in Rapid
Fossils are documents of the past and are valuable to museums for current
and future study, and as a resource for the public.
People are encouraged to participate with museums in protecting South Dakota's fossil heritage. Often, much of the valuable
information about a fossil is lost if the specimen is removed from the rock deposit before accurate records are made. In
addition, amateur collectors could inadvertently damage specimens when trying to remove them from surrounding rock and
soil. If you locate any significant fossil deposits, contact the S.D. Museum of Geology, before disturbing the site (see
Collectors must have permission from landowners in order to look for
and collect fossils from private land. It is illegal to
collect fossils from Tribal lands without permission from the Tribal authorities. For permission to fossil hunt along highway
right-of-ways, contact the nearest Department of Transportation Office (see the Rose Quartz fact sheet for addresses).
Regulations on public lands vary. People always should contact the land manager before disturbing geological formations.
Bonebeds - an accumulation of numerous bones in a single sedimentary
layer, and often dominated by one species.
Cretaceous - the geologic period that ranged from about 135 to 65 million years ago.
Cycads - large tropical plants resembling a palm and having fern-like leaves.
Ligaments - connective tissue that attaches bones to one another.
Paleontology - the scientific study of fossils.
Pelvis - the bones of the hips.
Quadrupeds - animals that walk on all four legs.
Sacral - the vertebrae that attach to the hips to insure solid support of the body by the back legs.
Sedimentary - rocks formed generally in one of three ways: by solidification of eroded rock fragments i.e. sandstone; by precipitation from a saturated water solution, i.e. rock salt; or by the secretion of organisms, i.e. coral limestone.
Vertebrae - the bones of the backbone; they protect the spinal column.
Hatcher, J.B., O.C. Marsh, and R.S. Lull, 1907. The Ceratopsia. U.S.
Geological Survey Monograph 49: 1-300 pp.
Weishapel, D.B., P. Dobson, and H. Osmolska, ed. 1990. The Dinosauria, University of California Press, 733 pp.
Dinosaurs of North America by Helen R. Sattler, 1981. Lothrop,
Lee and Shephard Books, NY.
Illustrated Encyclopedia of Dinosaurs by David Norman, 1994. Crescent Books. This volume has excellent pictures of
skeletons and reconstructions.
Museum of Geology Field Paleontology offerings are available
to teachers for credit and high school students for no-credit each summer.
Participants spend one to two weeks working at a fossil dig. For details
and costs contact the Museum of Geology for a brochure.
The Dinosaur Society Dinosaur Encyclopedia by Don Lessem and Donald Glut, 1993. Random House, New York. This
book is great for information relating dinosaurs and world geography.
Dr. Phil Bjork, Museum of Geology, S.D. School of Mines and Technology, Rapid City, SD 57701.
Dr. Erika Tallman, Northern State University, Aberdeen, SD 57401. 1995.
Dr. James E. Martin, Museum of Geology, S.D. School of Mines and Technology, Rapid City, SD 57701.
Publication of the Triceratops fact sheet was funded by the South
Dakota Department of Game, Fish and Parks, Division of
Wildlife, Pierre, SD.