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The Cloverly Formation is a geological formation of Early and Late Cretaceous age (Valanginian to Cenomanian stage) that is present in parts of Montana, Wyoming, Colorado and Utah in the western United States. It was named for a post office on the eastern side of the Bighorn Basin in Wyoming by N.H. Darton in 1904. The sedimentary rocks of formation were deposited in floodplain environments and contain vertebrate fossils, including a diverse assemblage of dinosaur remains. In 1973, the Cloverly Formation Site was designated as a National Natural Landmark by the National Park Service.

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  • Cloverly Formation (en)
  • Formació de Cloverly (ca)
  • Souvrství Cloverly (cs)
  • Formación Cloverly (es)
  • Formation de Cloverly (fr)
rdfs:comment
  • Souvrství Cloverly je geologické souvrství, jehož sedimenty se rozkládají na území západoamerických států Montana, Wyoming, Colorado a Utah. Své jméno odvozuje od poštovní stanice, která se na přelomu 19. a 20. století nacházela na východní straně Bighornské pánve. Jméno pro souvrství zvolil N. H. Darton v roce 1904. (cs)
  • La formació de Cloverly data del Cretaci inferior i està localitzada a Montana i Wyoming, a l'oest dels Estats Units. (ca)
  • The Cloverly Formation is a geological formation of Early and Late Cretaceous age (Valanginian to Cenomanian stage) that is present in parts of Montana, Wyoming, Colorado and Utah in the western United States. It was named for a post office on the eastern side of the Bighorn Basin in Wyoming by N.H. Darton in 1904. The sedimentary rocks of formation were deposited in floodplain environments and contain vertebrate fossils, including a diverse assemblage of dinosaur remains. In 1973, the Cloverly Formation Site was designated as a National Natural Landmark by the National Park Service. (en)
  • La formation de Cloverly est une formation géologique datant du Crétacé inférieur (Aptien et Albien) située dans les États du Montana et du Wyoming aux États-Unis. (fr)
  • La Formación Cloverly , es una formación geológica datada alrededor de 112 a 99,6 millones de años atrás en el Albiense durante el Cretácico inferior, en el bajo de Bighorn, en el límite entre los estados de Montana y Wyoming, en Estados Unidos, incluyendo el estrato anteriormente llamado Formación Dakota. Tiene un grueso medio de aproximadamente 90 metros y parte superior de la Fm. Cloverly es marcada por facies marinas transgresiva, depositada por un mar interior que penetro en dirección Sur Se la divide en tres miemnbros (es)
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  • Cloverly Formation (en)
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  • http://commons.wikimedia.org/wiki/Special:FilePath/Acrocantosaurus4.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Aquilops_NT_small.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Cloverly_Fm.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Ceratodus.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Deinonychus_ewilloughby.png
  • http://commons.wikimedia.org/wiki/Special:FilePath/GobiconodonDB15.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Microvenator.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Sauroposeidon_proteles.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Sauropelta_jconway.png
  • http://commons.wikimedia.org/wiki/Special:FilePath/Zephyrosaurus_in_Copenhagen.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Tenontosaurus_BW.jpg
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