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The Rattlesnake Hills greenstone belt represents a fragment of a partially exposed synformal Archean greenstone belt within the Wyoming craton that was intruded by Cenozoic alkalic volcanics. The supracrustal belt has been subjected to multiphase deformation during the Archean and later brittle deformation during the Laramide orogeny. Ductile deformation during the Archean produced foliation, and at least three episodes of folding.

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  • The Rattlesnake Hills greenstone belt represents a fragment of a partially exposed synformal Archean greenstone belt within the Wyoming craton that was intruded by Cenozoic alkalic volcanics. The supracrustal belt has been subjected to multiphase deformation during the Archean and later brittle deformation during the Laramide orogeny. Ductile deformation during the Archean produced foliation, and at least three episodes of folding. (en)
  • La cintura di rocce verdi delle Rattlesnake Hills rappresenta un frammento del sinclinale parzialmente esposto della cintura di rocce verdi risalenti all'Archeano posta all'interno del cratone del Wyoming, che è stata intruso da vulcanismo alcalino del Cenozoico. La cintura sopracrostale ha subìto deformazioni multifase durante l'Archeano, seguite da una successiva deformazione fragile durante l'orogenesi laramide. La deformazione duttile durante l'Archeano ha dato luogo a foliazione e ad almeno tre episodi di formazione di pieghe. (it)
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  • The Rattlesnake Hills greenstone belt represents a fragment of a partially exposed synformal Archean greenstone belt within the Wyoming craton that was intruded by Cenozoic alkalic volcanics. The supracrustal belt has been subjected to multiphase deformation during the Archean and later brittle deformation during the Laramide orogeny. Ductile deformation during the Archean produced foliation, and at least three episodes of folding. (en)
  • La cintura di rocce verdi delle Rattlesnake Hills rappresenta un frammento del sinclinale parzialmente esposto della cintura di rocce verdi risalenti all'Archeano posta all'interno del cratone del Wyoming, che è stata intruso da vulcanismo alcalino del Cenozoico. La cintura sopracrostale ha subìto deformazioni multifase durante l'Archeano, seguite da una successiva deformazione fragile durante l'orogenesi laramide. La deformazione duttile durante l'Archeano ha dato luogo a foliazione e ad almeno tre episodi di formazione di pieghe. (it)
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  • Cintura di rocce verdi delle Rattlesnake Hills (it)
  • Rattlesnake Hills greenstone belt (en)
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