Dinosaur National Monument

Dinosaur National Monument is an American national monument located on the southeast flank of the Uinta Mountains[3] 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 at 40°26′29″N 109°18′04″W. The nearest Colorado town is Dinosaur while the nearest city is Vernal, Utah.

Dinosaur National Monument
A dinosaur skull embedded in rock at Dinosaur National Monument
Location in the United States
LocationMoffat County, Colorado and Uintah County, Utah, U.S.
Nearest cityVernal, Utah
Coordinates40°32′N 108°59′W
Area210,844 acres (853.26 km2)
EstablishedOctober 4, 1915[1]
Visitors304,468 (in 2018)[2]
Governing bodyU.S. National Park Service
WebsiteDinosaur National Monument
Map showing the boundaries of Dinosaur National Monument

Originally preserved in 1915 to protect its famous Dinosaur Quarry,[4] the monument was greatly expanded in 1938 to include its wealth of natural history. The park's wild landscapes, topography, geology, paleontology, and history make it a unique resource for both science and recreation. The park contains over 800 paleontological sites and has fossils of dinosaurs including Allosaurus, Deinonychus, Abydosaurus, and various sauropods.[4] The Abydosaurus consists of a nearly complete skull, the lower jaw, and first four neck vertebrae. The specimen was found at the base of the Mussentuchit Member of the Cedar Mountain Formation and is the holotype for the description.

Paleontologist Earl Douglass of the Carnegie Museum discovered eight vertebra of an Apatosaurus on August 17, 1909,[1] which became the first dinosaur skeleton discovered and excavated at the new Carnegie Quarry. The area around the quarry was declared a national monument on October 4, 1915.[1] The International Dark-Sky Association designated Dinosaur National Monument an International Dark Sky Park in April 2019.[5]

Geology

Multicolored beds of the Brushy Basin Member of the Morrison Formation

The rock layer enclosing the fossils is a sandstone and conglomerate bed of alluvial or river bed origin known as the Morrison Formation from the Jurassic Period some 150 million years old. The dinosaurs and other ancient animals were carried by the river system which eventually entombed their remains in Utah.

The pile of sediments were later buried and lithified into solid rock. The layers of rock were later uplifted and tilted to their present angle by the mountain building forces that formed the Uinta Mountains[3] during the Laramide orogeny.[4] The relentless forces of erosion exposed the layers at the surface to be found by paleontologists.

History

Fremont people

Petroglyphs at McKee Spring in Dinosaur National Monument[6]

The Fremont people lived in the area of what is now Dinosaur National Monument before the 14th century, with archaeological evidence dating from c. 200 to c. 1300. Archaeologists first studied and named the Fremont culture along the Fremont River in south-central Utah and have since traced it through much of the Green and Colorado River drainages.[7]

The Fremont did not build large permanent dwellings; instead, they lived in small bands within natural shelters, such as rock overhangs or shallow caves, or small villages. They consumed plant foods, such as pine nuts, berries, and cactus fruits, as well as wild game, including mule deer, bighorn sheep, smaller mammals, and birds. They also grew corn, beans, and squash, sometimes using irrigation techniques.[7]

The fate of the Fremont culture is unclear. Recent theories suggest that the Fremont’s lifestyle may have changed due to drought or other climate factors, dwindling natural resources, or the influence of other neighboring cultures.[7] They left evidence of their presence in the form of petroglyphs and pictographs of human and animal figures, and abstract designs. Human figures typically have trapezoidal bodies and elaborate decorations that suggest headdresses, earrings, necklaces, or shields. The animal figures include bighorn sheep, birds, snakes, and lizards. Purely abstract or geometric designs, such as circles, spirals, and various combinations of lines, are common. Many designs in the monument are accessible for close viewing, along four trails in Utah, one of which is near the visitor center, and a fifth trail in Colorado.[8]

Early scientific explorations

Paleontologist chips rock matrix from a column of vertebrae in the Dinosaur Quarry.

The dinosaur fossil beds (bone beds) were discovered in 1909 by Earl Douglass, a paleontologist working and collecting for the Carnegie Museum of Natural History.[9] He and his crews excavated thousands of fossils and shipped them back to the museum in Pittsburgh, Pennsylvania for study and display.

National monument

President Woodrow Wilson proclaimed the dinosaur beds as Dinosaur National Monument in 1915. The monument boundaries were expanded in 1938 from the original 80 acres (0.13 sq mi; 0.32 km2) surrounding the dinosaur quarry in Utah, to 210,844 acres (329 sq mi; 853 km2) in Utah and Colorado, encompassing the river canyons of the Green and Yampa.[1]

Echo Park Dam controversy

Confluence of the Green and Yampa Rivers

The plans made by the U.S. Bureau of Reclamation on a ten-dam, billion dollar Colorado River Storage Project began to arouse opposition in the early 1950s when it was announced that one of the proposed dams would be at Echo Park, in the middle of Dinosaur National Monument. The controversy assumed major proportions, dominating conservation politics for years. David Brower, executive director of the Sierra Club, and Howard Zahniser of The Wilderness Society led an unprecedented nationwide campaign to preserve the free-flowing rivers and scenic canyons of the Green and Yampa Rivers. They argued that if a national monument was not safe from development, how could any wildland be kept intact?[10]

On the other side of the argument were powerful members of Congress from western states, who were committed to the project in order to secure water rights, obtain cheap hydroelectric power and develop reservoirs as tourist destinations. After much debate, Congress settled on a compromise that eliminated Echo Park Dam and authorized the rest of the project. The Colorado River Storage Project Act became law on April 11, 1956. It stated, "that no dam or reservoir constructed under the authorization of the Act shall be within any National Park or Monument."

Historians view the Echo Park Dam controversy as signaling the start of an era that includes major conservationist political successes such as the Wilderness Act and the Wild and Scenic Rivers Act.

Historic places

Places on the list of National Register of Historic Places include:[11]

Prehistoric sites
Other sites
Green River Canyon in Dinosaur National Monument

Climate

The Dinosaur National Monument sits on a vast area of desert land in Northwestern Colorado and Northeastern Utah. Typical of high deserts, summer temperatures can be exceedingly hot, while winter temperatures can be very cold. Snowfall is common, but the snow melts rapidly in the arid and sunny climates of these states. Rainfall is very low, and the evaporation rate classifies the area as desert, even though the rainfall exceeds 10 inches.

Climate data for Dinosaur National Monument
Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year
Average high °F (°C) 33.0
(0.6)
39.0
(3.9)
50.4
(10.2)
60.8
(16.0)
71.9
(22.2)
83.2
(28.4)
90.5
(32.5)
87.9
(31.1)
77.7
(25.4)
63.6
(17.6)
45.7
(7.6)
34.2
(1.2)
61.5
(16.4)
Average low °F (°C) 10.8
(−11.8)
15.2
(−9.3)
25.0
(−3.9)
31.8
(−0.1)
40.5
(4.7)
48.9
(9.4)
56.6
(13.7)
54.7
(12.6)
45.5
(7.5)
34.9
(1.6)
23.3
(−4.8)
12.7
(−10.7)
33.3
(0.7)
Average precipitation inches (mm) 0.64
(16)
0.56
(14)
0.88
(22)
1.17
(30)
1.30
(33)
1.06
(27)
1.01
(26)
0.89
(23)
1.24
(31)
1.46
(37)
0.80
(20)
0.62
(16)
11.64
(296)
Average snowfall inches (cm) 9.2
(23)
6.6
(17)
5.9
(15)
3.5
(8.9)
0.7
(1.8)
0.2
(0.51)
0.0
(0.0)
0.0
(0.0)
0.2
(0.51)
1.6
(4.1)
4.7
(12)
8.3
(21)
41.1
(104)
Source: The Western Regional Climate Center[13]

Features

The quarry

The Quarry Exhibit Hall

The "Wall of Bones" located within the Dinosaur Quarry building in the park consists of a steeply tilted (67° from horizontal) rock layer which contains hundreds of dinosaur fossils. The enclosing rock has been chipped away to reveal the fossil bones intact for public viewing. In July 2006, the Quarry Visitor Center was closed due to structural problems that since 1957 had plagued the building because it was built on unstable clay. The decision was made to build a new facility elsewhere in the monument to house the visitor center and administrative functions, making it easier to resolve the structural problems of the quarry building while still retaining a portion of the historic Mission 66 era exhibit hall.[14] It was announced in April 2009 that Dinosaur National Monument would receive $13.1 million to refurbish and reopen the gallery as part of the Obama administration's $750 billion stimulus plan.[15] The Park Service successfully rebuilt the Quarry Exhibit Hall, supporting its weight on 70-foot steel micropile columns that extend to the bedrock below the unstable clay.[16] The Dinosaur Quarry was reopened in Fall 2011.

Vertebrate fossils from Carnegie Quarry

Workers inside the Dinosaur Quarry building
Now enclosed by the Dinosaur Quarry building (Gilmore (1936), Foster (2003))
Reptilia
Testudines
Amphichelydia
Glyptops plicatus
Dinochelys whitei
Rhynchocephalia
Opisthias rarus
Crocodilia
Mesosuchia
Gonipholididae
Goniopholis sp.
Atoposauridae
Hoplosuchus kayi (h)
Dinosauria
Saurischia
Theropoda
Ceratosaurus sp.
Torvosaurus sp.
Allosaurus fragilis
Sauropoda
Apatosaurus louisae (h)
Barosaurus lentus
Camarasaurus lentus
Diplodocus longus
Uintasaurus douglassi (h) (now Camarasaurus lentus)
Ornithischia
Stegosauria
Stegosaurus ungulatus
Ornithopoda
Iguanodontia
Uteodon aphanoecetes (h)
Dryosauridae
Dryosaurus elderae (h)
(h) = holotype

See also

References

  1. "Dinosaur National Monument Statistics". NPS. January 11, 2008. Retrieved 2009-03-21.
  2. "NPS Annual Recreation Visits Report". National Park Service. Retrieved 2017-05-09.
  3. Hansen, Wallace (1969). The Geologic Story of the Uinta Mountains (USGS Bulletin 1291 ed.). U.S. Geological Survey.
  4. Gregson, J.D., Chure, D.J., Sprinkle, D.A. (2010). "Geology and Paleontology of Dinosaur National Monument". Geology of Utah's Parks and Monuments. UGA Publication 28 (third edition) (Utah Geological Association): 161–192.
  5. April 22, on; 2019 (2019-04-22). "Dinosaur National Monument Designated as an International Dark Sky Park". International Dark-Sky Association. Retrieved 2019-07-05.CS1 maint: numeric names: authors list (link)
  6. "Rainbow and Island Parks". Dinosaur National Monument. National Park Service. Retrieved 14 December 2020.
  7.  This article incorporates public domain material from the National Park Service document: "Fremont Culture". October 7, 2018. Retrieved January 29, 2020.
  8.  This article incorporates public domain material from the National Park Service document: "Viewing Petroglyphs and Pictographs". December 19, 2017. Retrieved January 29, 2020.
  9. Douglass, G.E. (2009). Iverson, Diane Douglass (ed.). Speak to the earth and it will teach you : the life and times of Earl Douglass, 1862-1931. Charleston, S.C.: BookSurge. ISBN 9781439244371.
  10. McPhee, John (1971). Encounters with the Archdruid. New York: Farrar, Straus and Giroux. p. 245. ISBN 0-374-51431-3.
  11. National Register of Historic Places in Moffat County American Dreams, Inc. Retrieved 2011-10-6.
  12. "Josie Bassett Morris Ranch Complex". National Archives Catalog. U.S. National Archives. Retrieved 13 December 2020.
  13. "Seasonal Temperature and Precipitation Information". Western Regional Climate Center. Retrieved May 3, 2013.
  14. "Draft Environmental Impact Statement for Quarry Visitor Center, Part 1" (PDF). National Park Service. March 2007. Archived from the original (PDF) on 2007-06-11. Retrieved 2008-02-11.
  15. "$13.1M in stimulus cash revives dino monument". Salt Lake Tribune. April 2009. Archived from the original on 2012-03-22. Retrieved 2009-04-23.
  16. "Visiting The Quarry In Fall And Winter". National Park Service. November 2011. Archived from the original on 2011-12-29. Retrieved 2012-03-21.

Further reading

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