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Trilobite fossils are relatively common in the region west of Delta (part of the House Range's Wheeler Shale). Several local companies maintain fossil dig areas where they allow visitors to dig their own fossils for a small fee. Near Delta is a mountain called Topaz Mountain, which derives its name from the topaz that is
During the four years that spanned from 1972 to 1976, rocks and fossils were stocked at the BYU football stadium until a specific building was constructed in 1976 for the BYU Earth Science Museum, [5] known in the present day as the BYU Museum of Paleontology. Under the direction of the BYU Earth Science Museum, the quarry has been excavated ...
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. [1] During the Precambrian, the area of northeastern Utah now occupied by the Uinta Mountains was a shallow sea which was home to simple ...
Fossil of the Middle Ordovician graptolite Didymograptus †Didymograptus †Didymograptus nitidus – or unidentified comparable form †Dimeropygiella †Diplorrhina †Donaldina †Dresbachia †Echinaria †Ectosteorhachis – or unidentified related form †Ehmaniella †Eldonia †Eleutherocentrus †Elrathia †Elrathina †Emeraldella ...
This list of the Paleozoic life of Utah contains the various prehistoric life-forms whose fossilized remains have been reported from within the US state of Utah and are between 538.8 and 252.17 million years of age.
The geology of Utah, in the western United States, includes rocks formed at the edge of the proto-North American continent during the Precambrian.A shallow marine sedimentary environment covered the region for much of the Paleozoic and Mesozoic, followed by dryland conditions, volcanism, and the formation of the basin and range terrain in the Cenozoic.
The Weeks Formation is a geologic formation in Utah.It preserves fossils dating back to the Cambrian period and more specifically the Guzhangian stage.Its upper part has yielded a diverse fauna dominated by trilobites and brachiopods, but also comprising various soft-bodied organisms, such as Falcatamacaris. [1]
The Chinle Formation is an Upper Triassic continental geological formation of fluvial, lacustrine, and palustrine to eolian deposits spread across the U.S. states of Nevada, Utah, northern Arizona, western New Mexico, and western Colorado. In New Mexico, it is often raised to the status of a geological group, the Chinle Group.