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1 A geologic map of Utah, illustrates the strata conventionally colored differently according to geological age. Notice the San Rafael Swell, the dominant geologic and geographic feature in the eastcentral part of the State. The Cleveland-Lloyd Dinosaur Quarry (C-LDQ) is located on the northern end or nose of the Swell.P1048 James H. Madsen Photograph CollectionP1048n002
2 This view of the Cleveland-Lloyd Dinosaur Quarry (C-LDQ) in Emery County, Utah is typical of the primitive landscape and isolated areas, where many of Utah's dinosaurs are found and collected.P1048 James H. Madsen Photograph CollectionP1048n003
3 These colorful, Morrison Formation exposures are similar to the rock outcrops where dinosaur bones are found in many localities across the Colorado Plateau of Utah, New Mexico, and Colorado.P1048 James H. Madsen Photograph CollectionP1048n004
4 The Visitor Center at the C-LDQ, which became a United States Natural Landmark in 1968, has some interesting graphics that interpret and detail the operation and history of the Quarry. Included in the exhibits are some prepared, original dinosaur bones, and a mounted free- standing skeleton of a medium-sized Allosaur, which consists of less than 50% of the original, fossil bones. The skull of the Allosaur can be seen through the window in the front of the building.P1048 James H. Madsen Photograph CollectionP1048n006
5 Interior of the C-LDQ Visitor's Center showing a dinosaur skeleton.P1048 James H. Madsen Photograph CollectionP1048n006a
6 This is a view of the main interpretive exhibit, an Allosaurus, inside the Visitor Center at the Cleveland-Lloyd Dinosaur Quarry. The Center is open on a limited basis during the summer months and not at all for the rest of the year. The Quarry, Visitor Center, and picnic areas are supervised and maintained by the United States, Department of the Interior, Bureau of Land Management with the support and excavation at various times of the College of Eastern Utah, Prehistoric Museum, the Earth Science Museum at Brigham Young University, and the Utah Museum of Natural History.P1048 James H. Madsen Photograph CollectionP1048n007
7 This oil painting by Utah artist, Gale Hammond, is his interpretation of dinosaur life at the Cleveland-Lloyd Quarry 147.5 million years ago. A large Allosaur looks on, while a second predator attacks a Camptosaur. Notice the vegetation and a ponderous sauropod dinosaur wading the shallow lake in the background. Few dinosaur Paleontologists now agree that sauropods spent much time swimming or wading, thereby risking getting mired in the mud of or adjacent to shallow bodies of water.P1048 James H. Madsen Photograph CollectionP1048n008
8 Painting interpretation of dinosaur life.P1048 James H. Madsen Photograph CollectionP1048n009a
9 A good lesson to learn early on, when digging dinosaurs, is that even in a desert there is occasional rain; and when it rains, it is advisable to have a drain in the lowest part of the quarry excavation lest it turn into a wading pool, as seen here.P1048 James H. Madsen Photograph CollectionP1048n014
10 View from above, looking south(?).P1048 James H. Madsen Photograph CollectionP1048nGS01
11 Northerly view of quarry from Visitor Center.P1048 James H. Madsen Photograph CollectionP1048nGS02
12 Close-up view of limestone cap, lying over the fossiliferous unit, which is approximately 1 meter in thickness.P1048 James H. Madsen Photograph CollectionP1048nGS05
13 Another view of the limestone cap showing the undulating surface of the underlying fossiliferous, bentonitic shale.P1048 James H. Madsen Photograph CollectionP1048nGS06
14 The left background may be very close to the original Princeton Quarry outline.P1048 James H. Madsen Photograph CollectionP1048nGS07
15 Prospect near the southern end of the Quarry in the vicinity of the Princeton Quarry(?).P1048 James H. Madsen Photograph CollectionP1048nGS08
16 Large rib in blocky shale, Quarry number 2214.P1048 James H. Madsen Photograph CollectionP1048nGS09
17 A concretionary limestone unit with a number of bones enclosed.P1048 James H. Madsen Photograph CollectionP1048nGS10
18 Neural spine, sauropod (?), enclosed in the softer shale unit.P1048 James H. Madsen Photograph CollectionP1048nGS11
19 Horizon showing soft, bentonitic shale unit underlying more massive unit.P1048 James H. Madsen Photograph CollectionP1048nGS12
20 Blocky shale horizon near the base of the fossiliferous unit. Usually has sparse fossils at least.P1048 James H. Madsen Photograph CollectionP1048nGS13
21 Interesting shots of flat-lying, blockey shale near the base of the fossiliferous unit.P1048 James H. Madsen Photograph CollectionP1048nGS14
22 Interesting shots of flat-lying, blockey shale near the base of the fossiliferous unit.P1048 James H. Madsen Photograph CollectionP1048nGS15
23 Interesting shots of flat-lying, blockey shale near the base of the fossiliferous unit.P1048 James H. Madsen Photograph CollectionP1048nGS16
24 Quarry worker, indicating that he cannot find any fossils. Pot-holing is not a good quarrying procedure.P1048 James H. Madsen Photograph CollectionP1048nGS17
25 Caudal vertebra, Camarasaurus.P1048 James H. Madsen Photograph CollectionP1048nIN_A01
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