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・ Dinosaur Island
・ Dinosaur Island (1994 film)
・ Dinosaur Island (2002 film)
・ Dinosaur Island (Sea World)
・ Dinosaur Isle
・ Dinosaur Jr.
・ Dinosaur Jr. discography
・ Dinosaur King
・ Dinosaur King (video game)
・ Dinosaur Kingdom
・ Dinosaur Land
・ Dinosaur Land (Rügen)
・ Dinosaur man
・ Dinosaur Museum
・ Dinosaur Museum (Dorchester)
Dinosaur National Monument
・ Dinosaur nudibranch
・ Dinosaur paleobiogeography
・ Dinosaur Park
・ Dinosaur Park (novel)
・ Dinosaur Park (Prince George's County, Maryland)
・ Dinosaur Park Formation
・ Dinosaur Pile-Up
・ Dinosaur Planet
・ Dinosaur Planet (novel)
・ Dinosaur Planet (TV series)
・ Dinosaur Planet Survivors
・ Dinosaur plant
・ Dinosaur Provincial Park
・ Dinosaur renaissance


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Dinosaur National Monument : ウィキペディア英語版
Dinosaur National Monument

Dinosaur National Monument is a U.S. 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 just to the north of the town of Jensen, Utah.
The nearest communities are Vernal, Utah and Dinosaur, Colorado. This park contains over 800 paleontological sites and has fossils of dinosaurs including ''Allosaurus'', ''Deinonychus'', ''Abydosaurus'' (a nearly complete skull, lower jaws and first four neck vertebrae of the specimen DINO 16488 found here at the base of the Mussentuchit Member of the Cedar Mountain Formation is the holotype for the description) and various long-neck, long-tail sauropods. It was declared a National Monument on October 4, 1915.〔
==Geology==
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.
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 Uintas during the Laramide orogeny . The relentless forces of erosion exposed the layers at the surface to be found by paleontologists.

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