|Skeletal mount of a T. prorsus specimen at the Natural History Museum of Los Angeles|
†T. horridus Marsh, 1889
Triceratops is a genus of herbivorous ceratopsid dinosaur that first appeared during the late Maastrichtian stage of the late Cretaceous period, about 68 million years ago (mya) in what is now North America. It is one of the last known non-avian dinosaur genera, and became extinct in the Cretaceous–Paleogene extinction event 66 million years ago.  The name Triceratops, which literally means "three-horned face", is derived from the Ancient Greek words τρί- (tri-) meaning "three", κέρας (kéras) meaning "horn", and ὤψ (ōps) meaning "face".  
It has been documented by numerous remains collected since the genus was first described in 1889, including at least one complete individual skeleton.  Paleontologist John Scannella observed: "It is hard to walk out into the Hell Creek Formation and not stumble upon a Triceratops weathering out of a hillside." Forty-seven complete or partial skulls were discovered in just that area from 2000 to 2010.  Specimens representing life stages from hatchling to adult have been found.  As the archetypal ceratopsid, Triceratops is one of the most popular dinosaurs, and has been featured in film, postal stamps, and many other types of media.
Bearing a large bony frill and three horns on its large four-legged body, and possessing similarities with the modern rhinoceros, Triceratops is one of the most recognizable of all dinosaurs and the best known ceratopsid. It shared the landscape with and was probably preyed upon by Tyrannosaurus,  though it is less certain that the two did battle in the manner often depicted in traditional museum displays and popular images. The functions of the frills and three distinctive facial horns on its head have long inspired debate. Traditionally, these have been viewed as defensive weapons against predators. More recent theories, noting the presence of blood vessels in the skull bones of ceratopsids, find it more probable that these features were primarily used in identification, courtship and dominance displays, much like the antlers and horns of modern reindeer, mountain goats, or rhinoceros beetles.  The theory would find additional support if Torosaurus were found to be the mature form of Triceratops, as this would mean the frill also developed holes ( fenestrae) as individuals reached maturity, rendering the structure more useful for display than defense. 
The exact placement of the genus Triceratops within the ceratopsid group has been debated by paleontologists. Two species, T. horridus and T. prorsus, are considered valid, although many other species have been named. Research published in 2010 suggested that the contemporaneous Torosaurus, a ceratopsid long regarded as a separate genus, represents Triceratops in its mature form.   The view was immediately disputed    and examination of more fossil evidence is expected to settle the debate.
- 1 Description
- 2 Discovery and identification
- 3 Classification
- 4 Paleobiology
- 5 Paleoecology
- 6 Depiction in popular media
- 7 References
- 8 External links
Individual Triceratops are estimated to have reached about 7.9 to 9.0 m (25.9–29.5 ft) in length, 2.9 to 3.0 m (9.5 to 9.8 ft) in height,   and 6.1–12.0 tonnes (13,000–26,000 lb) in weight.  The most distinctive feature is their large skull, among the largest of all land animals. The largest known skull (specimen MWC 7584, formerly BYU 12183) is estimated to have been 2.5 metres (8.2 ft) in length when complete,  and could reach almost a third of the length of the entire animal.  A specimen of T. horridus named Kelsey measured 7.3 metres (24 ft) long with a 1.98 metres (6.5 ft) skull, stood about 2.3 metres (7.5 ft) tall, and was estimated by the Black Hills institute to weight nearly 6 tonnes (5.9 long tons; 6.6 short tons).  A Triceratops 8 metres (26 ft) long has been estimated by Gregory S. Paul to have massed 9.3 tonnes (9.2 long tons; 10.3 short tons).  It bore a single horn on the snout, above the nostrils, and a pair of horns approximately 1 m (3.3 ft) long, with one above each eye.  In 2010, paleontologists revealed a fossil (named "Yoshi's Trike," MOR 3027) with 115-centimetre-long (3.77 ft) horn cores, housed and displayed at the Museum of the Rockies in Montana.   To the rear of the skull was a relatively short, bony frill, adorned with epoccipitals in some specimens. Most other ceratopsids had large fenestrae in their frills, while those of Triceratops were noticeably solid.  T. horridus can be distinguished from T. prorsus by having a shallower snout. 
Triceratops species possessed a sturdy build, with strong limbs, short hands with three hooves each, and short feet with four hooves each.  Although certainly quadrupedal, the posture of these dinosaurs has long been the subject of some debate. Originally, it was believed that the front legs of the animal had to be sprawling at angles from the thorax in order to better bear the weight of the head.  This stance can be seen in paintings by Charles Knight and Rudolph Zallinger. Ichnological evidence in the form of trackways from horned dinosaurs and recent reconstructions of skeletons (both physical and digital) seem to show that Triceratops and other ceratopsids maintained an upright stance during normal locomotion, with the elbows flexed and slightly bowed out, in an intermediate state between fully upright and fully sprawling (as in the modern rhinoceros).    
The hands and forearms of Triceratops retained a fairly primitive structure compared to other quadrupedal dinosaurs such as thyreophorans and many sauropods. In those two groups, the forelimbs of quadrupedal species were usually rotated so that the hands faced forward with palms backward ("pronated") as the animals walked. Triceratops, like other ceratopsians and the related quadrupedal ornithopods, walked with most of their fingers pointing out and away from the body, the primitive condition for dinosaurs also retained by bipedal forms like the theropods. In Triceratops, the weight of the body was carried by only the first three fingers of the hand, while digits 4 and 5 were vestigial and lacked claws or hooves.  The phalangeal formula is 2-3-4-3-1, meaning that the innermost finger of the forelimb has two bones, the next has three, etc. 
The first named specimen now attributed to Triceratops is a pair of brow horns attached to a skull roof, found near Denver, Colorado in the spring of 1887.  This specimen was sent to American paleontologist Othniel Charles Marsh, who believed that the formation from which it came dated from the Pliocene, and that the bones belonged to a particularly large and unusual bison, which he named Bison alticornis.   He realized that there were horned dinosaurs by the next year, which saw his publication of the genus Ceratops from fragmentary remains,  but he still believed B. alticornis to be a Pliocene mammal. It took a third and much more complete skull to change his mind. The specimen, collected in 1888 by John Bell Hatcher from the Lance Formation of Wyoming, was initially described as another species of Ceratops.  After reflection, Marsh changed his mind and gave it the generic name Triceratops, accepting his Bison alticornis as another species of Ceratops  (it would later be added to Triceratops ). The sturdy nature of the animal's skull has ensured that many examples have been preserved as fossils, allowing variations between species and individuals to be studied. Triceratops remains have subsequently been found in the American states of Montana and South Dakota (in addition to Colorado and Wyoming), and in the provinces of Saskatchewan and Alberta, Canada.
An earlier specimen, also recovered from the Lance Formation, was named Agathaumas sylvestris by Edward Drinker Cope in 1872. Originally identified as a hadrosaur, this specimen consists only of post-cranial remains and is only provisionally considered an example of Triceratops. 
Within the first decades after Triceratops was described, various skulls were collected, which varied to a lesser or greater degree from the original Triceratops, named T. horridus by Marsh (from the Latin horridus; "rough, rugose", suggesting the roughened texture of those bones belonging to the type specimen, later identified as an aged individual). This variation is unsurprising, given that Triceratops skulls are large three-dimensional objects, coming from individuals of different ages and both sexes, and which were subjected to different amounts and directions of pressure during fossilization.  Discoverers would name these as separate species (listed below), and came up with several phylogenetic schemes for how they were related to each other.
In the first attempt to understand the many species, Lull found two groups, although he did not say how he distinguished them: one composed of T. horridus, T. prorsus, and T. brevicornus; the other of T. elatus and T. calicornis. Two species (T. serratus and T. flabellatus) stood apart from these groups.  By 1933, and his revision of the landmark 1907 Hatcher-Marsh-Lull monograph of all known ceratopsians, he retained his two groups and two unaffiliated species, with a third lineage of T. obtusus and T. hatcheri that was characterized by a very small nasal horn.  T. horridus-T. prorsus-T. brevicornus was now thought to be the most conservative lineage, with an increase in skull size and a decrease in nasal horn size, and T. elatus-T. calicornis was defined by large brow horns and small nasal horn.   C. M. Sternberg made one modification, adding T. eurycephalus and suggesting that it linked the second and third lineages closer together than they were to the T. horridus lineage.  This pattern was followed until the major studies of the 1980s and 1990s.
With time, the idea that the differing skulls might be representative of individual variation within one (or two) species gained popularity. In 1986, Ostrom and Wellnhofer published a paper in which they proposed that there was only one species, Triceratops horridus.  Part of their rationale was that generally there are only one or two species of any large animal in a region (modern examples being the elephant and the giraffe in modern Africa). To their findings, Lehman added the old Lull-Sternberg lineages combined with maturity and sexual dimorphism, suggesting that the T. horridus-T. prorsus-T. brevicornus lineage was composed of females, the T.calicornis-T.elatus lineage was made up of males, and the T. obtusus-T. hatcheri lineage was of pathologic old males.  His reasoning was that males had taller, more erect horns and larger skulls, and females had smaller skulls with shorter, forward-facing horns.
These findings were contested a few years later by Catherine Forster, who reanalyzed Triceratops material more comprehensively and concluded that the remains fell into two species, T. horridus and T. prorsus, although the distinctive skull of T. ("Nedoceratops") hatcheri differed enough to warrant a separate genus.  She found that T. horridus and several other species belonged together, and T. prorsus and T. brevicornus stood alone, and since there were many more specimens in the first group, she suggested that this meant the two groups were two species. It is still possible to interpret the differences as representing a single species with sexual dimorphism.  
In 2009, John Scannella and Denver Fowler supported the separation of T. prorsus and T. horridus, and noted that the two species are also separated stratigraphically within the Hell Creek Formation, indicating that they did not live together at the same time. 
Some of the following species are synonyms, as indicated in parentheses ("=T. horridus" or "=T. prorsus"). All the others are considered nomina dubia ("dubious names") because they are based on remains too poor or incomplete to be distinguished from pre-existing Triceratops species.
- T. albertensis ( C. M. Sternberg, 1949)
- T. alticornis ( Hatcher, Marsh, and Lull, 1907 [originally Bison alticornis, Marsh 1887, and Ceratops alticornis, Marsh 1888])
- T. brevicornus (Hatcher, 1905) (=T. prorsus)
- T. calicornis (Marsh, 1898) (=T. horridus)
- T. elatus (Marsh, 1891) (=T. horridus)
- T. eurycephalus ( Schlaikjer, 1935)
- T. flabellatus (Marsh, 1889) (=T. horridus)
- T. galeus (Marsh, 1889)
- T. hatcheri (Lull, 1907) (contentious; see Nedoceratops below)
- T. ingens ( Lull, 1915)
- T. maximus ( Brown, 1933)
- T. mortuarius ( Cope, 1874) (nomen dubium; originally Polyonax mortuarius)
- T. obtusus (Marsh, 1898) (=T. horridus)
- T. serratus (Marsh, 1890) (=T. horridus)
- T. sulcatus (Marsh, 1890)
- T. sylvestris (Cope, 1872) (nomen dubium; originally Agathaumas sylvestris)
Triceratops is the best known genus of the Ceratopsidae, a family of large, mostly North American horned dinosaurs. The exact location of Triceratops among the ceratopsians has been debated over the years. Confusion stemmed mainly from the combination of short, solid frills (similar to that of Centrosaurinae), and the long brow horns (more akin to Chasmosaurinae).  In the first overview of horned dinosaurs, R. S. Lull hypothesized two lineages, one of Monoclonius and Centrosaurus leading to Triceratops, the other with Ceratops and Torosaurus, making Triceratops a centrosaurine as the group is understood today.  Later revisions supported this view, formally describing the first, short-frilled group as Centrosaurinae (including Triceratops), and the second, long-frilled group as Chasmosaurinae.  
In 1949, Charles M. Sternberg was the first to question this and proposed instead that Triceratops was more closely related to Arrhinoceratops and Chasmosaurus based on skull and horn features, making Triceratops a ceratopsine (chasmosaurine of his usage) genus.  He was largely ignored, with John Ostrom,  and later David Norman both placing Triceratops within Centrosaurinae. 
Subsequent discoveries and analyses upheld Sternberg's view on the position of Triceratops, with Lehman defining both subfamilies in 1990 and diagnosing Triceratops as ceratopsine (chasmosaurine of his usage) on the basis of several morphological features. In fact, it fits well into the ceratopsine subfamily, apart from its one feature of a shortened frill.  Further research by Peter Dodson, including a 1990 cladistic analysis  and a 1993 study using RFTRA (resistant-fit theta-rho analysis),  a morphometric technique which systematically measures similarities in skull shape, reinforces Triceratops' placement in the ceratopsine subfamily.
The cladogram below follows Longrich (2014), who named a new species of Pentaceratops, and included nearly all species of chasmosaurine. 
For many years after its discovery, the evolutionary origins of Triceratops remained largely obscure. In 1922, the newly discovered Protoceratops was seen as its ancestor by Henry Fairfield Osborn,  but many decades passed before additional findings came to light. Recent years have been fruitful for the discovery of several antecedents of Triceratops. Zuniceratops, the earliest known ceratopsian with brow horns, was described in the late 1990s, and Yinlong, the first known Jurassic ceratopsian, in 2005.
These new finds have been vital in illustrating the origins of horned dinosaurs in general, suggesting an Asian origin in the Jurassic, and the appearance of truly horned ceratopsians by the beginning of the late Cretaceous in North America.  As Triceratops is increasingly shown to be a member of the long-frilled subfamily Ceratopsinae, a likely ancestor may have resembled Chasmosaurus, which thrived some 5 million years earlier.
In phylogenetic taxonomy, the genus Triceratops has been used as a reference point in the definition of Dinosauria; dinosaurs have been designated as all descendants of the most recent common ancestor of Triceratops and Neornithes (i.e. modern birds).  Furthermore, the bird-hipped dinosaurs, Ornithischia, have all been designated dinosaurs with a more recent common ancestor to Triceratops than modern birds. 
Although Triceratops are commonly portrayed as herding animals, there is currently little evidence that they lived in herds. While several other genera of horned dinosaurs are known from bonebeds preserving bones from two to hundreds or thousands of individuals, to date there is only one documented bonebed dominated by Triceratops bones: a site in southeastern Montana with the remains of three juveniles. It may be significant that only juveniles were present.  In 2012, a group of three Triceratops in relatively complete condition, each of varying sizes from a full-grown adult to a small juvenile, were found in Wyoming, near Newcastle. The remains are currently under excavation by paleontologist Peter Larson and a team from the Black Hills Institute. It is believed that the animals were traveling as a family unit, but it remains unknown if the group consists of a mated pair and their offspring, or two females and a juvenile they were caring for. The remains also show signs of predation or scavenging from Tyrannosaurus, particularly on the largest specimen, with the bones of the front limbs showing breakage and puncture wounds from Tyrannosaurus teeth. 
For many years, Triceratops finds were known only from solitary individuals.  These remains are very common; for example, Bruce Erickson, a paleontologist of the Science Museum of Minnesota, has reported having seen 200 specimens of T. prorsus in the Hell Creek Formation of Montana.  Similarly, Barnum Brown claimed to have seen over 500 skulls in the field. :79 Because Triceratops teeth, horn fragments, frill fragments, and other skull fragments are such abundant fossils in the Lancian faunal stage of the late Maastrichtian ( late Cretaceous, 66 mya) Period of western North America, it is regarded as among the dominant herbivores of the time, if not the most dominant herbivore. In 1986, Robert Bakker estimated it as making up 5/6ths of the large dinosaur fauna at the end of the Cretaceous.  Unlike most animals, skull fossils are far more common than postcranial bones for Triceratops, suggesting that the skull had an unusually high preservation potential. 
Triceratops were herbivorous, and because of their low head, their primary food was probably low growth, although they may have been able to knock down taller plants with their horns, beak, and bulk.   The jaws were tipped with a deep, narrow beak, believed to have been better at grasping and plucking than biting. 
Triceratops teeth were arranged in groups called batteries, of 36 to 40 tooth columns in each side of each jaw, with 3 to 5 stacked teeth per column, depending on the size of the animal.  This gives a range of 432 to 800 teeth, of which only a fraction were in use at any given time (tooth replacement was continuous throughout the life of the animal).  They functioned by shearing in a vertical to near-vertical orientation.  The great size and numerous teeth of Triceratops suggests that they ate large volumes of fibrous plant material,  with some researchers suggesting palms and cycads,   and others suggesting ferns, which then grew in prairies. 
There has been much speculation over the functions of Triceratops' head adornments. The two main theories have revolved around use in combat and in courtship display, with the latter now thought to be the most likely primary function. 
Early on, Lull postulated that the frills may have served as anchor points for the jaw muscles to aid chewing by allowing increased size and thus power for the muscles.  This has been put forward by other authors over the years, but later studies do not find evidence of large muscle attachments on the frill bones. 
Triceratops were long thought to have used their horns and frills in combat with predators such as Tyrannosaurus, the idea being discussed first by Charles H. Sternberg in 1917 and 70 years later by Robert Bakker.   There is evidence that Tyrannosaurus did have aggressive head-on encounters with Triceratops, based on partially healed tyrannosaur tooth marks on a Triceratops brow horn and squamosal; the bitten horn is also broken, with new bone growth after the break. Which animal was the aggressor is not known.  Since the Triceratops wounds healed, it is most likely that the Triceratops survived the encounter. Tyrannosaurus is also known to have fed on Triceratops, as shown by a heavily tooth-scored Triceratops ilium and sacrum. 
In addition to combat with predators using horns, Triceratops are popularly shown engaging each other in combat with horns locked. While studies show that such activity would be feasible, if unlike that of present-day horned animals,  there is disagreement about whether they did so. Although pitting, holes, lesions, and other damage on Triceratops skulls (and the skulls of other ceratopsids) are often attributed to horn damage in combat, a 2006 study finds no evidence for horn thrust injuries causing these forms of damage (for example, there is no evidence of infection or healing). Instead, non-pathological bone resorption, or unknown bone diseases, are suggested as causes.  A newer study compared incidence rates of skull lesions and periosteal reaction in Triceratops and Centrosaurus and showed that these were consistent with Triceratops using its horns in combat and the frill being adapted as a protective structure, while lower pathology rates in Centrosaurus may indicate visual rather than physical use of cranial ornamentation, or a form of combat focused on the body rather than the head.  The frequency of injury was found to be 14% in Triceratops.  The researchers also concluded that the damage found on the specimens in the study was often too localized to be caused by bone disease.  Histological examination reveals that the frill of Triceratops is composed of fibrolamellar bone  which contains fibroblasts that play a critical role in wound healing, and are capable of rapidly depositing bone during remodeling.  
One skull was found with a hole in the jugal bone, apparently a puncture wound sustained while the animal was alive, as indicated by signs of healing. The hole has a diameter close to that of the distal end of a Triceratops horn. This, and other apparent healed wounds in the skulls of ceratopsians, has been cited as evidence of non-fatal intraspecific competition in these dinosaurs.  
The large frill also may have helped to increase body area to regulate body temperature.  A similar theory has been proposed regarding the plates of Stegosaurus,  although this use alone would not account for the bizarre and extravagant variation seen in different members of the Ceratopsidae, which would rather support the sexual display theory. 
The theory that frills functioned as a sexual display was first proposed by Davitashvili in 1961 and has gained increasing acceptance since.    Evidence that visual display was important, either in courtship or other social behavior, can be seen in the horned dinosaurs differing markedly in their adornments, making each species highly distinctive. Also, modern living creatures with such displays of horns and adornments use them similarly.  A 2006 study of the smallest Triceratops skull, ascertained to be a juvenile, shows the frill and horns developed at a very early age, predating sexual development and thus probably important for visual communication and species recognition in general.  The use of the exaggerated structures to enable dinosaurs to recognize their own species has been questioned, as no such function exists for such structures in modern species. 
In 2006, the first extensive ontogenetic study of Triceratops was published in the journal Proceedings of the Royal Society. The study, by John R. Horner and Mark Goodwin, found that individuals of Triceratops could be divided into four general ontogenetic groups, babies, juveniles, subadults, and adults. With a total number of 28 skulls studied, the youngest was only 38 cm (15 in) long. 10 of the 28 skulls could be placed in order in a growth series with one representing each age. Each of the four growth stages were found to have identifying features. Multiple ontogenetic trends were discovered, including the size reduction of the epoccipitals, development and reorientation of postorbital horns, and hollowing out of the horns. 
Torosaurus is a ceratopsid genus first identified from a pair of skulls in 1891, two years after the identification of Triceratops. The genus Torosaurus resembles Triceratops in geological age, distribution, anatomy and size and it has been recognised as a close relative.  Its distinguishing features are an elongated skull and the presence of two fenestrae, or holes, in the frill. Paleontologists investigating dinosaur ontogeny (growth and development of individuals over the life span) in the Hell Creek Formation, Montana, US, have recently presented evidence that the two represent a single genus.
John Scannella, in a paper presented in Bristol, UK at the conference of the Society of Vertebrate Paleontology (25 September 2009) reclassified Torosaurus as especially mature Triceratops individuals, perhaps representing a single sex. Jack Horner, Scannella's mentor at Bozeman Campus, Montana State University, noted that ceratopsian skulls consist of metaplastic bone. A characteristic of metaplastic bone is that it lengthens and shortens over time, extending and resorbing to form new shapes. Significant variety is seen even in those skulls already identified as Triceratops, Horner said, "where the horn orientation is backwards in juveniles and forward in adults". Approximately 50% of all subadult Triceratops skulls have two thin areas in the frill that correspond with the placement of "holes" in Torosaurus skulls, suggesting that holes developed to offset the weight that would otherwise have been added as maturing Triceratops individuals grew longer frills.  A paper describing these findings in detail was published in July 2010 by Scannella and Horner. It formally argues that Torosaurus and the similar contemporary Nedoceratops are synonymous with Triceratops. 
The assertion ignited debate. Andrew Farke had in 2006 stressed that, apart from the frill, no systematic differences could be found between Torosaurus and Triceratops.  He nevertheless disputed Scannella's conclusion by arguing in 2011 that the proposed morphological changes required to "age" a Triceratops into a Torosaurus would be without precedent among ceratopsids. Creatures would require the growth of epoccipitals, reversion of bone texture from adult to immature forms back to adult, and growth of frill holes at a later stage than usual.  A study by Nicholas Longrich and Daniel Field analyzed 35 specimens of both Triceratops and Torosaurus. The authors concluded that Triceratops individuals too old to be considered immature forms are represented in the fossil record, as are Torosaurus individuals too young to be considered fully mature adults. The synonymy of Triceratops and Torosaurus cannot be supported, they said, without more convincing intermediate forms than Scannella and Horner initially produced. Scannella's Triceratops specimen with a hole on its frill, they argued, could represent a diseased or malformed individual rather than a transitional stage between an immature Triceratops and mature Torosaurus form.  
Given the abundance of fossils, particularly of Triceratops, additional field discoveries are expected to settle the debate in time.
Opinion has varied on the validity of a separate genus for Nedoceratops. John Scannella and Jack Horner regarded it as an intermediate growth stage between Triceratops and Torosaurus.   Andrew Farke, in his 2011 redescription of the only known skull, concluded that it was an aged individual of its own valid taxon, Nedoceratops hatcheri.  Nicholas Longrich and Daniel Fields also did not consider it a transition between Torosaurus and Triceratops, suggesting that the frill holes were pathological. 
As described above, John Scannella had argued in 2010 that Nedoceratops should be considered a synonym of Triceratops.  Andrew Farke (2011) maintained that it represents a valid distinct genus.  Nick Longrich agreed with Scannella about Nedoceratops and made a further suggestion: that the recently described Ojoceratops was likewise a synonym. The fossils, he argued, are indistinguishable from the T. horridus specimens that were previously attributed to the defunct species T. serratus.
Longrich observed that another newly described genus, Tatankaceratops, displayed a strange mix of characteristics already found in adult and juvenile Triceratops. Rather than representing a distinct genus, Tatankaceratops could as easily represent a dwarf Triceratops or a Triceratops individual with a developmental disorder that caused it to stop growing prematurely. 
Triceratops lived during the Late Cretaceous of North America, its fossils coming from the Evanston Formation, Scollard Formation, Laramie Formation, Lance Formation, Denver Formation, and Hell Creek Formation.  These fossil formations date back to the time of the Cretaceous-Paleogene Extinction Event, and have been dated to 66 ± 0.07 million years ago.  Many animals and plants have been found in these formations, but mostly from the Lance Formation and Hell Creek Formation.  Triceratops was one of the last ceratopsian genera to appear before the end of the Mesozoic. The related Torosaurus, and the more distantly related diminutive Leptoceratops, were also present, though their remains have been rarely encountered. 
Theropods from these formations include genera of tyrannosaurids, ornithomimids, troodontids,  avialans,  caenagnathids,  and dromaeosaurids. Acheroraptor and Dakotaraptor are dromaeosaurids from the Hell Creek Formation. Indeterminate dromaeosaurs are known from other fossil formations. Common teeth previously referred to Dromaeosaurus and Saurornitholestes later were considered to be Acheroraptor.  The tyrannosaurids from the formation are Nanotyrannus and Tyrannosaurus, although the former might be a junior synonym of the latter. Among ornithomimids are the genera Struthiomimus as well as Ornithomimus,  although an undescribed animal named " Orcomimus" could be from the formation.  Troodontids are only represented by Pectinodon and Paronychodon in the Hell Creek Formation; with a possible species of Troodon from the Lance Formation. One species of coelurosaur is known from Hell Creek and similar formations by a single species, Richardoestesia. Only three oviraptorosaurs are from the Hell Creek Formation, Anzu, Leptorhynchos  and a giant species of caenagnathid, very similar to Gigantoraptor, from South Dakota. However, only fossilized foot prints were discovered.  The avialans known from the formation are Avisaurus,  multiple species of Brodavis,  and several other species of hesperornithoforms, as well as several species of true birds including Cimolopteryx. 
Ornithischians are abundant in the Scollard Lance, Laramie, Lance, Denver, and Hell Creek Formation. The main groups of ornithischians are ankylosaurians, ornithopods, ceratopsians, and pachycephalosaurians. Three ankylosaurians are known, Ankylosaurus, Denversaurus, and possibly a species of Edmontonia or an undescribed genus. Multiple genera of ceratopsians are known from the formation other than Triceratops, the leptoceratopsid Leptoceratops, and the chasmosaurine ceratopsids Torosaurus,  Nedoceratops and Tatankaceratops.  Ornithopods are common in the Hell Creek Formation, and are known from several species of the ornithopod Thescelosaurus, and the hadrosaurids Edmontosaurus,   and a possible species of Parasaurolophus. Several pachycephalosaurians have been found in the Hell Creek Formation and in similar formations. Among them are the derived pachycephalosaurids " Stygimoloch",  " Dracorex",  Pachycephalosaurus,  Sphaerotholus, and an undescribed specimen from North Dakota. The first two might be junior synonyms of Pachycephalosaurus.
Mammals are plentiful in the Hell Creek Formation. Groups represented include multituberculates, metatherians, and eutherians. The multituberculates represented include Paracimexomys,  the cimolomyids Paressonodon,  Meniscoessus, Essonodon, Cimolomys, Cimolodon, and Cimexomys; and the neoplagiaulacids Mesodma, and Neoplagiaulax. The alphadontids Alphadon, Protalphodon, and Turgidodon, pediomyids Pediomys,  Protolambda, and Leptalestes,  the stagodontid Didelphodon,  the deltatheridiid Nanocuris, the herpetotheriid Nortedelphys,  and the glasbiid Glasbius all represent metatherians of the Hell Creek Formation. A few eutherians are known, being represented by Alostera,  Protungulatum,  the cimolestids Cimolestes and Batodon, the gypsonictopsid Gypsonictops, and the possible nyctitheriid Paranyctoides. 
Triceratops is the official state fossil of South Dakota,  and the official state dinosaur of Wyoming.  The distinctive appearance of Triceratops has led to it being frequently depicted in films, computer games and documentaries, such as the 1993 film Jurassic Park and the 1999 BBC television documentary Walking with Dinosaurs. A recurring theme, especially in children's dinosaur books, is a climactic showdown or battle between Triceratops and Tyrannosaurus. In 1942, Charles R. Knight painted a mural incorporating a confrontation between the two dinosaurs in the Field Museum of Natural History for the National Geographic Society, establishing them as enemies in the popular imagination.  Paleontologist Bob Bakker said of the imagined rivalry between Tyrannosaurus and Triceratops, "No matchup between predator and prey has ever been more dramatic. It's somehow fitting that those two massive antagonists lived out their co-evolutionary belligerence through the very last days of the very last epoch of the Age of Dinosaurs." 
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- Works related to Notice of Gigantic Horned Dinosauria from the Cretaceous at Wikisource
- Data related to Triceratops at Wikispecies
- Triceratops at The Dinosaur Picture Database
- LiveScience: Facts about Triceratops at LiveScience.com
- on YouTube
- Dinosaur Mailing List post on Triceratops stance
- Smithsonian Exhibit
- Triceratops at the Internet Archive
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- Triceratops (short summary and good color illustration)
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- Triceratops, BBC Dinosaurs
- (in French) Triceratops - Liste de Dinosauria et Extinction