Spence Shale

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The Spence Shale is the middle member of the Langston Formation in southeastern Idaho and northeastern Utah. It is exposed in the Bear River Range, the Wasatch Range and the Wellsville Mountains. It is known for its abundant Cambrian trilobites and the preservation of Burgess Shale-type fossils. The type locality is in southeastern Idaho, near the town of Liberty. It was first described by Charles Doolittle Walcott in 1908. rdf:langString
Les schistes de Spence sont une unité stratigraphique du Cambrien moyen présente dans des massifs de la province géologique du Grand Bassin, au sud-est de l'Idaho et au nord de l'Utah, aux États-Unis. Cette unité stratigraphique, qui fait partie de la formation de Langston, constitue un Konservat-Lagerstätte dont le mode de préservation de fossiles est de (en) (BST). Les schistes de Spence, parfois appelés Spence Tongue, sont connus pour leur richesse en fossiles de trilobites, de hyolithes et d'animaux à corps mou. rdf:langString
rdf:langString Schistes de Spence
rdf:langString Spence Shale
rdf:langString Spence Shale
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rdf:langString Hyolitha, Spence Shale
rdf:langString Les schistes de Spence sont une unité stratigraphique du Cambrien moyen présente dans des massifs de la province géologique du Grand Bassin, au sud-est de l'Idaho et au nord de l'Utah, aux États-Unis. Cette unité stratigraphique, qui fait partie de la formation de Langston, constitue un Konservat-Lagerstätte dont le mode de préservation de fossiles est de (en) (BST). Les schistes de Spence, parfois appelés Spence Tongue, sont connus pour leur richesse en fossiles de trilobites, de hyolithes et d'animaux à corps mou. Les schistes de Spence ont été décrits et nommés en 1908 par le paléontologue Charles Doolittle Walcott d'après le Spence Gulch, site type localisé dans la chaîne de montagne de Bear River, en Idaho.
rdf:langString The Spence Shale is the middle member of the Langston Formation in southeastern Idaho and northeastern Utah. It is exposed in the Bear River Range, the Wasatch Range and the Wellsville Mountains. It is known for its abundant Cambrian trilobites and the preservation of Burgess Shale-type fossils. The type locality is in southeastern Idaho, near the town of Liberty. It was first described by Charles Doolittle Walcott in 1908.
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