Carnegie Quarry, also known as Dinosaur Quarry or Douglass Quarry, [1] is a fossil site in Utah that dates to the Jurassic Period. It is located in the Morrison Formation. It is part of Dinosaur National Monument, which was founded to protect the site. A portion of the quarry remains unexcavated, and the fossils remain in the ground where they can be viewed by the public at the Quarry Visitor Center.
Carnegie Quarry is considered "one of the most important localities" in the Morrison Formation. [2] Hundreds of specimens have been collected from the site, representing at least ten different dinosaur species and several other kinds of reptile.
In 1909, the Carnegie Museum sent Earl Douglass to search for fossils. After months of unsuccessful searching, on Tuesday, August 17, near Vernal, Utah, Douglass came across a series of tail vertebrae that he identified as Brontosaurus . The discovery immediately attracted local attention. Douglass soon began excavations, and the series of caudal vertebrae proved to belong to a nearly complete skeleton of Apatosaurus. It became apparent that this was one of many specimens in the quarry. [3]
On October 4, 1915, President Woodrow Wilson signed a proclamation establishing Dinosaur National Monument. This took Douglass by surprise, and he was uncertain of how it would affect excavation. Holland was critical of the decision, saying "there are ten thousand other places in the mountains of the West where there are fossils sticking out of the rock...which are just as well worthy of being consecrated as 'national monuments' as is this spot." Holland was subsequently assured by the secretary of the interior that designating the land a national monument was the only way to protect it from private interests. The Carnegie Museum was granted permission to continue excavations at the site. [3] By 1917, the fragmentary condition of many of the fossils being excavated led Holland to become discouraged about the prospect of finding much more material, and Holland considered making 1918 the last year of excavations, but ultimately continued renewing the permit for a few more years. [3] After Andrew Carnegie's death in 1919, funding for the excavation decreased and the Carnegie Museum ceased excavations in 1922. [4] In 1923, the Smithsonian Institution and University of Utah conducted excavations at the site. The collection of fossils from the site then ceased for several decades until the National Park Service resumed excavations in the 1950s. [4]
In 1957, construction of the quarry visitor center began, which was opened in 1958. Approximately 2,000 bones are displayed in the building, left in the rock where they were found. [4] Work on the quarry wall was completed in 1999. [3]
Carnegie Quarry is located in the Brushy Basin Member of the Morrison Formation. The site has been dated to between 150.91 and 150.04 million years ago. [5] The quarry is located in a sandstone bed known as the Quarry Sandstone. The Quarry Sandstone is unusual for the upper Morrison Formation in being relatively coarse-grained. [6] The depositional environment has been subject to various interpretations. Kenneth Carpenter considered it to have been deposited in a braided river that he called the Quarry River, which he compared to the modern-day Platte River. [7] In contrast, Brezinski and Kollar interpreted the Quarry Sandstone to represent a crevasse splay, with the accumulation of skeletons at Carnegie Quarry having been deposited within one of the distributary channels over the course of at least two flooding events. [6] The quarry bed is tilted 67° from horizontal. [3]
Carnegie Quarry is the type locality of seven species: the turtles Glyptops utahensis [8] [a] and Dinochelys whitei [9] and the dinosaurs Apatosaurus louisae , [10] Uintasaurus douglassi [11] [b] , Camarasaurus annae [12] [c] Camptosaurus aphanoecetes , [14] [d] and Dryosaurus elderae . [15]
Numerous scientifically important fossils have been recovered from the quarry, including the most complete sauropod fossil ever found, the juvenile Camarasaurus specimen CM 11338, and the largest nearly complete dinosaur skeleton ever found, [16] the Apatosaurus specimen CM 3018, which was the specimen that led Douglass to discover the site.
Sauropod skeletons from the quarry are displayed at the Smithsonian Museum of Natural History, Royal Ontario Museum, Carnegie Museum of Natural History, American Museum of Natural History, and Denver Museum of Nature and Science.
Apatosaurus is a genus of herbivorous sauropod dinosaur that lived in North America during the Late Jurassic period. Othniel Charles Marsh described and named the first-known species, A. ajax, in 1877, and a second species, A. louisae, was discovered and named by William H. Holland in 1916. Apatosaurus lived about 152 to 151 million years ago (mya), during the late Kimmeridgian to early Tithonian age, and are now known from fossils in the Morrison Formation of modern-day Colorado, Oklahoma, New Mexico, Wyoming, and Utah in the United States. Apatosaurus had an average length of 21–23 m (69–75 ft), and an average mass of 16.4–22.4 t. A few specimens indicate a maximum length of 11–30% greater than average and a mass of approximately 33 t.
Dinosaur National Monument is an American national monument located on the southeast flank of the Uinta Mountains on the border between Colorado and Utah at the confluence of the Green and Yampa rivers. Although most of the monument area is in Moffat County, Colorado, the Dinosaur Quarry is located in Utah, north of the town of Jensen, Utah. The nearest Colorado town is Dinosaur while the nearest city is Vernal, Utah.
Camarasaurus was a genus of quadrupedal, herbivorous dinosaurs and is the most common North American sauropod fossil. Its fossil remains have been found in the Morrison Formation, dating to the Late Jurassic epoch, between 155 and 145 million years ago.
Barosaurus was a giant, long-tailed, long-necked, plant-eating sauropod dinosaur closely related to the more familiar Diplodocus. Remains have been found in the Morrison Formation from the Upper Jurassic Period of Colorado, Utah, South Dakota, and eastern Wyoming at Como Bluff. It is present in stratigraphic zones 2–5.
Dryosaurus is a genus of an ornithopod dinosaur that lived in the Late Jurassic period. It was an iguanodont. Fossils have been found in the western United States and were first discovered in the late 19th century. Valdosaurus canaliculatus and Dysalotosaurus lettowvorbecki were both formerly considered to represent species of Dryosaurus.
Camptosaurus is a genus of plant-eating, beaked ornithischian dinosaurs of the Late Jurassic period of western North America and possibly also Europe. The name means 'flexible lizard'.
Como Bluff is a long ridge extending east–west, located between the towns of Rock River and Medicine Bow, Wyoming. The ridge is an anticline, formed as a result of compressional geological folding. Three geological formations, the Sundance, the Morrison, and the Cloverly Formations, containing fossil remains from the Late Jurassic of the Mesozoic Era are exposed.
Jurassic National Monument, at the site of the Cleveland-Lloyd Dinosaur Quarry, well known for containing the densest concentration of Jurassic dinosaur fossils ever found, is a paleontological site located near Cleveland, Utah, in the San Rafael Swell, a part of the geological layers known as the Morrison Formation.
Brontosaurus is a genus of herbivorous sauropod dinosaur that lived in present-day United States during the Late Jurassic period. It was described by American paleontologist Othniel Charles Marsh in 1879, the type species being dubbed B. excelsus, based on a partial skeleton lacking a skull found in Como Bluff, Wyoming. In subsequent years, two more species of Brontosaurus were named: B. parvus in 1902 and B. yahnahpin in 1994. Brontosaurus lived about 156 to 146 million years ago (mya) during the Kimmeridgian and Tithonian ages in the Morrison Formation of what is now Utah and Wyoming. For decades, the animal was thought to have been a taxonomic synonym of its close relative Apatosaurus, but a 2015 study by Emmanuel Tschopp and colleagues found it to be distinct. It has seen widespread representation in popular culture, being the archetypal "long-necked" dinosaur in general media.
Marshosaurus is a genus of medium-sized carnivorous theropod dinosaur, belonging to the family Piatnitzkysauridae, from the Late Jurassic Morrison Formation of Utah and possibly Colorado.
Camarasaurus supremus is a species of sauropod dinosaur that lived during the Jurassic period in what is now the western United States. It is the type species of Camarasaurus, which also includes the species Camarasaurus grandis, Camarasaurus lentus, and Camarasaurus lewisi. C. supremus was discovered by the paleontologist Edward Drinker Cope in 1877, at the outset of the Bone Wars, a period of scientific competition between Cope and his rival Othniel Marsh. C. supremus is the largest and geologically youngest species in its genus, and was contemporary with several other exceptionally large dinosaurs, such as Saurophaganax and Maraapunisaurus. Despite being the first discovered species of Camarasaurus, C. supremus is relatively rare and poorly known.
Apatosaurinae is a subfamily of diplodocid sauropods, an extinct group of large, quadrupedal dinosaurs, the other subfamily in Diplodocidae being Diplodocinae. Apatosaurines are distinguished by their more robust, stocky builds and shorter necks proportionally to the rest of their bodies. Several fairly complete specimens are known, giving a comprehensive view of apatosaurine anatomy.
Camarasaurus lentus is an extinct species of sauropod dinosaur that lived during the Jurassic period in what is now the western United States. It is one of the four valid species of the well-known genus Camarasaurus. C. lentus fossils have been found in Wyoming, Colorado, and Utah. It is the species of Camarasaurus found in Dinosaur National Monument and the middle layers of the Morrison Formation. Camarasaurus lentus is among the best-known sauropod species, with many specimens known. A juvenile specimen of C. lentus, CM 11338, is the most complete sauropod fossil ever discovered.
Glyptops is an extinct genus of pleurosternid freshwater turtle known from the Late Jurassic of North America.
Diplodocus is an extinct genus of diplodocid sauropod dinosaurs known from the Late Jurassic of North America. The first fossils of Diplodocus were discovered in 1877 by S. W. Williston. The generic name, coined by Othniel Charles Marsh in 1878, is a Neo-Latin term derived from Greek διπλός (diplos) "double" and δοκός (dokos) "beam", in reference to the double-beamed chevron bones located in the underside of the tail, which were then considered unique.
Uteodon is a genus of herbivorous iguanodontian dinosaur. It is a basal iguanodontian which lived during the late Jurassic period in what is now Uintah County, Utah. It is known from the middle of the Brushy Basin Member, Morrison Formation. The genus was named by Andrew T. McDonald in 2011 and the type species is U. aphanoecetes.
Osmakasaurus is a genus of herbivorous iguanodontian dinosaur. It is a basal iguanodontian which lived during the Early Cretaceous period in what is now Buffalo Gap of South Dakota, United States. It is known from the Chilson Member of the Lakota Formation. This genus was named by Andrew T. McDonald in 2011 and the type species is O. depressus.
Paleontology in Utah refers to paleontological research occurring within or conducted by people from the U.S. state of Utah. Utah has a rich fossil record spanning almost all of the geologic column. During the Precambrian, the area of northeastern Utah now occupied by the Uinta Mountains was a shallow sea which was home to simple microorganisms. During the early Paleozoic Utah was still largely covered in seawater. The state's Paleozoic seas would come to be home to creatures like brachiopods, fishes, and trilobites. During the Permian the state came to resemble the Sahara desert and was home to amphibians, early relatives of mammals, and reptiles. During the Triassic about half of the state was covered by a sea home to creatures like the cephalopod Meekoceras, while dinosaurs whose footprints would later fossilize roamed the forests on land. Sand dunes returned during the Early Jurassic. During the Cretaceous the state was covered by the sea for the last time. The sea gave way to a complex of lakes during the Cenozoic era. Later, these lakes dissipated and the state was home to short-faced bears, bison, musk oxen, saber teeth, and giant ground sloths. Local Native Americans devised myths to explain fossils. Formally trained scientists have been aware of local fossils since at least the late 19th century. Major local finds include the bonebeds of Dinosaur National Monument. The Jurassic dinosaur Allosaurus fragilis is the Utah state fossil.
Earl Douglass was an American paleontologist who discovered the dinosaur Apatosaurus, playing a central role in one of the most important fossil finds in North America. By 1922 Earl had unearthed and shipped more than 700,000 pounds of material including nearly 20 complete skeletons of Jurassic dinosaurs such as Diplodocus, Dryosaurus, Stegosaurus, Barosaurus, Camarasaurus and Brontosaurus.