Relevant bibliographies by topics / Valley of Dinosaurs

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  2. Dissertations / Theses
  3. Books
  4. Book chapters
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Academic literature on the topic 'Valley of Dinosaurs'

Author: Grafiati
Published: 4 June 2021
Last updated: 13 February 2022

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Journal articles on the topic "Valley of Dinosaurs"

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PEMBERTON, S. GEORGE, and ERIN A. PEMBERTON. "ROLE OF ICHNOLOGY IN THE HISTORY OF PHOTOGRAPHY." Earth Sciences History 37, no. 1 (2018): 63–87. http://dx.doi.org/10.17704/1944-6178-37.1.63.

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ABSTRACT Vertebrate ichnology in North America has a long and distinguished history, starting with the remarkable discoveries by Edward Hitchcock of dinosaur footprints and trackways in the Connecticut River Valley. Hitchcock assembled a unique collection that is currently housed in the Beneski Museum of Natural History, Amherst College, and his work essentially constituted the beginnings of ichnology as a viable sub-discipline of paleontology. Although his original interpretation that these Late Triassic locomotion traces were bird tracks was incorrect, he indirectly linked birds and dinosaur
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Bouzekraoui, Hicham, Ahmed Barakat, Mohammed El Youssi, et al. "Mapping Geosites as Gateways to the Geotourism Management in Central High-Atlas (Morocco)." Quaestiones Geographicae 37, no. 1 (2018): 87–102. http://dx.doi.org/10.2478/quageo-2018-0007.

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Abstract Demnate commune and High-Tessaout valley are located in the Moroccan central High-Atlas. They have a great and much diversified geological and geomorphological heritage and exceptional landscapes of high mountains. The data obtained from the current work indicate that the studied area present high tourist vocation, in the fact that this territory preserves a large number of geosites linked to many witnesses fossils of extinct animals such dinosaurs footprints, outcropping rock formations of the Precambrian and Mesozoic. Further, it has many remarkable landforms and geosites such as ca
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Abrahams, Miengah, Emese M. Bordy, Lara Sciscio, and Fabien Knoll. "Scampering, trotting, walking tridactyl bipedal dinosaurs in southern Africa: ichnological account of a Lower Jurassic palaeosurface (upper Elliot Formation, Roma Valley) in Lesotho." Historical Biology 29, no. 7 (2017): 958–75. http://dx.doi.org/10.1080/08912963.2016.1267164.

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Martz, Jeffrey, James Kirkland, Andrew Milner, William Parker, and Vincent Santucci. "Upper Triassic lithostratigraphy, depositional systems, and vertebrate paleontology across southern Utah." Geology of the Intermountain West 4 (April 21, 2017): 99–180. http://dx.doi.org/10.31711/giw.v4.pp99-180.

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The Chinle Formation and the lower part of the overlying Wingate Sandstone and Moenave Formation were deposited in fluvial, lacustrine, paludal, and eolian environments during the Norian and Rhaetian stages of the Late Triassic (~230 to 201.3 Ma), during which time the climate shifted from subtropical to increasingly arid. In southern Utah, the Shinarump Member was largely confined to pre-Chinle paleovalleys and usually overprinted by mottled strata. From southeastern to southwestern Utah, the lower members of the Chinle Formation (Cameron Member and correlative Monitor Butte Member) thicken d
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Martz, Jeffrey W., James I. Kirkland, Andrew R. C. Milner, William G. Parker, and Vincent L. Santucci. "Upper Triassic lithostratigraphy, depositional systems, and vertebrate paleontology across southern Utah." Geology of the Intermountain West 4 (August 2, 2017): 99–180. http://dx.doi.org/10.31711/giw.v4i0.13.

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The Chinle Formation and the lower part of the overlying Wingate Sandstone and Moenave Formation were deposited in fluvial, lacustrine, paludal, and eolian environments during the Norian and Rhaetian stages of the Late Triassic (~230 to 201.3 Ma), during which time the climate shifted from subtropical to increasingly arid. In southern Utah, the Shinarump Member was largely confined to pre-Chinle paleovalleys and usually overprinted by mottled strata. From southeastern to southwestern Utah, the lower members of the Chinle Formation (Cameron Member and correlative Monitor Butte Member) thicken d
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O'Hara, Sarah L., and Ian A. Campbell. "Holocene geomorphology and stratigraphy of the lower Falcon valley, Dinosaur Provincial Park, Alberta, Canada." Canadian Journal of Earth Sciences 30, no. 9 (1993): 1846–52. http://dx.doi.org/10.1139/e93-162.

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A tributary of the Red Deer River in Dinosaur Provincial Park, southern Alberta, contains evidence of a sequence of valley cutting and the deposition of three alluvial fills and one eolian deposit. With the exception of the eolian deposit and minor amounts of Shield and Cordilleran rocks, the sediments are derived from local bedrock. Incision of the bedrock valley occurred in the early postglacial period about 14 000 – 12 000 BP by rapid drainage of proglacial lakes and meltwaters. The valley was subsequently partly infilled as locally fed stream discharges declined during the early to middle
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Averett, Walter R. "Dinosaur Valley: Colorado's New Paleontological Museum." Rocks & Minerals 61, no. 2 (1986): 79–83. http://dx.doi.org/10.1080/00357529.1986.11768443.

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Utley, Dan K. "Dinosaur Highway: A History of Dinosaur Valley State Park (review)." Southwestern Historical Quarterly 113, no. 3 (2010): 420–21. http://dx.doi.org/10.1353/swh.2010.0057.

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Eberth, David A., and Sandra L. Kamo. "High-precision U–Pb CA–ID–TIMS dating and chronostratigraphy of the dinosaur-rich Horseshoe Canyon Formation (Upper Cretaceous, Campanian–Maastrichtian), Red Deer River valley, Alberta, Canada." Canadian Journal of Earth Sciences 57, no. 10 (2020): 1220–37. http://dx.doi.org/10.1139/cjes-2019-0019.

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The non-marine Horseshoe Canyon Formation (HCFm, southern Alberta) yields taxonomically diverse, late Campanian to middle Maastrichtian dinosaur assemblages that play a central role in documenting dinosaur evolution, paleoecology, and paleobiogeography leading up to the end-Cretaceous extinction. Here, we present high-precision U–Pb CA–ID–TIMS ages and the first calibrated chronostratigraphy for the HCFm using zircon grains from (1) four HCFm bentonites distributed through 129 m of section, (2) one bentonite from the underlying Bearpaw Formation, and (3) a bentonite from the overlying Battle F
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Tandon, S. K., A. Sood, J. E. Andrews, and P. F. Dennis. "Palaeoenvironments of the dinosaur-bearing Lameta Beds (Maastrichtian), Narmada Valley, Central India." Palaeogeography, Palaeoclimatology, Palaeoecology 117, no. 3-4 (1995): 153–84. http://dx.doi.org/10.1016/0031-0182(94)00128-u.

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Dissertations / Theses on the topic "Valley of Dinosaurs"

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Silva, Eduardo Pordeus. "Políticas culturais e economia da cultura no sertão paraibano: o caso vale dos dinossauros." Universidade Federal da Paraí­ba, 2009. http://tede.biblioteca.ufpb.br:8080/handle/tede/4392.

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Made available in DSpace on 2015-05-07T14:27:12Z (GMT). No. of bitstreams: 1 parte1.pdf: 296029 bytes, checksum: 44561e6fea9187a38d7264f99e940982 (MD5) Previous issue date: 2010-01-26<br>Coordenação de Aperfeiçoamento de Pessoal de Nível Superior<br>The culture and cultural politics have become considerable topics from the economic point of view, and mainly, from the social development. In this context, the cultural patrimony, particularly, no matter its denomination (historical, artistic, archaeological and paleontological patrimony) or its way of expression (material or non material), dese
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Davis, Nathan Robert. "Sequence Stratigraphy of the Lower Pennsylvanian (Bashkirian, Morrowan) Round Valley Limestone, Split Mountain Anticline (Dinosaur National Monument) and in the Eastern Uinta Mountains, Utah." BYU ScholarsArchive, 2010. https://scholarsarchive.byu.edu/etd/2377.

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The Early Pennsylvanian (Bashkirian/Morrowan) Round Valley Limestone of northeastern Utah was deposited on the Wyoming shelf, a slowly subsiding depositional surface located between the Eagle and Oquirrh basins. The 311-foot-thick Round Valley Limestone displays a distinct cyclicity formed by stacked, meter-scale parasequences, comprised of a limited suite of open- to restricted-marine limestones with minor interbeds of siltstone and shale. Open-marine deposits are characterized by mudstone and heterozoan wackestone-packstone microfacies (MF1-4) and comprise the lower portions of parasequences
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Books on the topic "Valley of Dinosaurs"

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Kurokawa, Mitsuhiro. Dinosaur valley. Chronicle Books, 1992.

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Helfer, Andrew. Dinosaur Valley. Western Pub. Co., 1990.

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J, Fillmore Barbara, and Marquardt Lori, eds. Dinosaur lake: The story of the Purgatoire Valley dinosaur tracksite area. Colorado Geological Survey, 1997.

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ill, Enik Ted, ed. Monster of lost valley. Simon & Schuster, 1986.

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Bast, William, Jim O'Connolly, and Charles H. Schneer. The Valley of Gwangi. Warner Home Video, 2012.

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The valley of the ancients. Faber and Faber, 2008.

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Judy, Freudberg, Geiss Tony, and Don Bluth Productions, eds. The search for the Great Valley. Grosset & Dunlap, 1988.

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Razzi, Jim. The Land before time: The search for the great valley. Grosset & Dunlap, 1988.

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Hlady, Ernest. The valley of the dinosaurs: Its families and coal mines. East Coulee Community Association, 1988.

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Great day trips in the Connecticut Valley of the dinosaurs. Perry Heights Press, 2004.

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Book chapters on the topic "Valley of Dinosaurs"

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Bonde, Joshua W., David J. Varricchio, Frankie D. Jackson, David B. Loope, and Aubrey M. Shirk. "Dinosaurs and dunes! Sedimentology and paleontology of the Mesozoic in the Valley of Fire State Park." In GSA Field Guide 11: Field Guide to Plutons, Volcanoes, Faults, Reefs, Dinosaurs, and Possible Glaciation in Selected Areas of Arizona, California, and Nevada. Geological Society of America, 2008. http://dx.doi.org/10.1130/2008.fld011(11).

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Hankla, John, Samantha Sands, Megan Sims, and Jeremy Wyman. "Live science in the Valley of the Last Dinosaurs: A public window into the world of paleontology." In Museums at the Forefront of the History and Philosophy of Geology: History Made, History in the Making. Geological Society of America, 2018. http://dx.doi.org/10.1130/2018.2535(19).

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Hallam, Tony. "In search of possible causes of mass extinctions." In Catastrophes and Lesser Calamities. Oxford University Press, 2004. http://dx.doi.org/10.1093/oso/9780198524977.003.0004.

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When the subject of extinctions in the geological past comes up, nearly everyone’s thoughts turn to dinosaurs. It may well be true that these long-extinct beasts mean more to most children than the vast majority of living creatures. One could even go so far as to paraphrase Voltaire and maintain that if dinosaurs had never existed it would have been necessary to invent them, if only as a metaphor for obsolescence. To refer to a particular machine as a dinosaur would certainly do nothing for its market value. The irony is that the metaphor is now itself obsolete. The modern scientific view of dinosaurs differs immensely from the old one of lumbering, inefficient creatures tottering to their final decline. Their success as dominant land vertebrates through 165 million years of the Earth’s history is, indeed, now mainly regarded with wonder and even admiration. If, as is generally thought, the dinosaurs were killed off by an asteroid at the end of the Cretaceous, that is something for which no organism could possibly have been prepared by normal Darwinian natural selection. The final demise of the dinosaurs would then have been the result, not of bad genes, but of bad luck, to use the laconic words of Dave Raup. In contemplating the history of the dinosaurs it is necessary to rectify one widespread misconception. Outside scientific circles the view is widely held that the dinosaurs lived for a huge slice of geological time little disturbed by their environment until the final apocalypse. This is a serious misconception. The dinosaurs suffered quite a high evolutionary turnover rate, and this implies a high rate of extinction throughout their history. Jurassic dinosaurs, dominated by giant sauropods, stegosaurs, and the top carnivore Allosaurus, are quite different from those of the Cretaceous period, which are characterized by diverse hadrosaurs, ceratopsians, and Tyrannosaurus. Michael Crichton’s science-fiction novel Jurassic Park, made famous by the Steven Spielberg movies, features dinosaurs that are mainly from the Cretaceous, probably because velociraptors and Tyrannosaurus could provide more drama.
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Verschuur, Gerrit L. "On the Edge of Extinction." In Impact! Oxford University Press, 1996. http://dx.doi.org/10.1093/oso/9780195101058.003.0012.

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On the morning of June 30, 1908, civilization may have suffered the worst piece of luck in its history. A small cometlike object exploded in the atmosphere above the Tunguska river valley in Siberia. It did little more than scorch and flatten trees for 20 kilometers in all directions and kill a thousand reindeer. However, if that object had struck a heavily populated region, we would not now dwell under any illusion concerning how close to the edge of extinction the human species actually hovers. Because the Tunguska missile missed a populated area, the threat of impact did not really begin to enter the public imagination until after the 1980 announcement of the discovery of the iridium in the K/T boundary layer. Had the Tunguska object struck a large city, a million people or more might have perished, and the phenomenon would have raised everyone’s awareness to the threat of comet impact. Instead, nearly a century later, the threat of comet and asteroid impact is regarded as little more than an interesting anecdote. Very slowly the nature of the threat is being recognized, but only because of the somewhat esoteric discovery that the dinosaurs were wiped out by a major impact 65 million years ago. Such huge collisions are infrequent, perhaps about once every 50 to 100 million years. It is the smaller impacts that pose the greatest danger, and they occur far more frequently. About 800 years ago the South Island of New Zealand suffered widespread fires, which leveled the island and led to the extinction of the Moa bird. Maori legend says that a big explosion in the sky was the cause of the strange fire. Duncan Steel of the University of Adelaide and Peter Snow from Otago in New Zealand have pieced together a fascinating scenario that suggests that the Maori were correct. The fireball created by a comet impact may have ignited the forests of South Island. Near the town of Tapanui in the province of Otago there exists a crater that geologists have been slow to identify as extraterrestrial in origin.
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Paik, In Sung, Min Huh, Hyun Joo Kim, Sook Ju Kim, and David Newsome. "The Cretaceous fossil sites of South Korea identifying geosites, science and geotourism." In Geotourism: the tourism of geology and landscape. Goodfellow Publishers, 2010. http://dx.doi.org/10.23912/978-1-906884-09-3-1058.

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There are a range of natural resources for geotourism in Korea, including scenic mountains with variable geological histories, hot springs, and coastline environments. Many of the national and provincial parks and natural monuments in Korea have been designated because of their geological values. Three sites on Jeju Island have been inscribed on the World Heritage list largely for geological values such as volcanic features and landscape and associated scenic values. Furthermore, there are many geological heritage sites designated as natural monuments in Cretaceous sedimentary basins in Korea. They include dinosaur fossil sites and geologically scenic sites. The former are of great scientific importance and many have the potential to be developed into geotourism destinations of global significance. Five sites, on the Korean Cretaceous Deinosaur Coast which have been very important for regional tourism, are currently being nominated as World Heritage for their highly significant fossil trackways and dinosaur eggs. The full gambit of geotourism potential for Korean geological heritage has rarely been studied (Jeong, 2000; Heo et al., 2006a; Heo et al., 2006b; Heo, 2007). In this chapter the Cretaceous geosites in Korea are summarized in respect to their importance as globally significant geotourism resources.
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King, Sally, Anjana Ford, and Richard Edmonds. "The Jurassic Coast World Heritage Site understanding the nature of geotourism." In Geotourism: the tourism of geology and landscape. Goodfellow Publishers, 2010. http://dx.doi.org/10.23912/978-1-906884-09-3-1067.

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The Dorset and East Devon Coast World Heritage Site (also known as the ‘Jurassic Coast’), stretches for 155 km across the southern English coastline, encompassing one of the most spectacular geological sequences in the world. The internationally renowned coastal exposures of the Jurassic Coast were awarded World Heritage Site status in 2001 based on a near complete sequence of Mesozoic rocks, which record evidence and development of early reptiles through to the age of the dinosaurs. For a site to obtain World Heritage Site status, it must exhibit cultural or natural features that are of ‘outstanding universal value’ and must be protected for present and future generations of all humanity. Protecting the integrity (or condition) of the site is essential for maintaining the qualities that led to site inscription. Coastal erosion maintains the geological integrity of the Jurassic Coast by exposing fossils that are then washed out onto the beaches. The fossils are an important part of our geological heritage.
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Conference papers on the topic "Valley of Dinosaurs"

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Hankla, John, Tyler R. Lyson, Laura Helft, Samantha Richards, and Jeremy Wyman. "LIVE SCIENCE IN THE VALLEY OF THE LAST DINOSAURS: A PUBLIC WINDOW INTO THE WORLD OF PALEONTOLOGY." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-283117.

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Caputo, Mario V., and Stephen M. Rowland. "INTERPLAY BETWEEN EOLIAN SEDIMENTATION, WATER TABLE DYNAMICS, WET-DRY CLIMATE, THERAPOD DINOSAURS, AND PROTOMAMMALS PRESERVED IN THE LOWER JURASSIC AZTEC SANDSTONE, VALLEY OF FIRE STATE PARK, SOUTHERN NEVADA." In Joint 70th Annual Rocky Mountain GSA Section / 114th Annual Cordilleran GSA Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018rm-314036.

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Clark, Andrew J., Jennifer A. Lange, Stephen M. Rowland, and Cynthia Shroba. "NEWLY DISCOVERED THEROPOD DINOSAUR TRACKS IN THE LOWER JURASSIC AZTEC SANDSTONE, VALLEY OF FIRE STATE PARK, SOUTHERN NEVADA." In Joint 70th Annual Rocky Mountain GSA Section / 114th Annual Cordilleran GSA Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018rm-314260.

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Indriati, Maria, Tahrun, and Hanni Yukamana. "Values of Character Education in Disney’s Animated Featured “The Good Dinosaur” by Peter Shon." In International Conference on Education Universitas PGRI Palembang (INCoEPP 2021). Atlantis Press, 2021. http://dx.doi.org/10.2991/assehr.k.210716.257.

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