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The Lopez de Bertodano Formation is a geological formation in the James Ross archipelago of the Antarctic Peninsula. The strata date from the end of the Late Cretaceous (upper-lower Maastrichtian stage) to the Danian stage of the lower Paleocene, from about 70 to 65.5 million years ago, straddling the Cretaceous-Paleogene boundary.

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  • The Lopez de Bertodano Formation is a geological formation in the James Ross archipelago of the Antarctic Peninsula. The strata date from the end of the Late Cretaceous (upper-lower Maastrichtian stage) to the Danian stage of the lower Paleocene, from about 70 to 65.5 million years ago, straddling the Cretaceous-Paleogene boundary. (en)
  • La formation de Lopez de Bertodano est une formation géologique affleurant sur l'île Seymour, dans l'archipel de James Ross, sur la péninsule Antarctique. Les strates vont de la fin du Crétacé supérieur (étage du Maastrichtien) jusqu'au Danien inférieur (Paléocène), il y a environ entre 70 et 65,5 Ma (millions d'années). (fr)
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  • Lopez de Bertodano Formation (en)
dbp:namedfor
  • López de Bertodano Bay (en)
dbp:otherlithology
  • Sandstone with concretions (en)
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dbp:period
  • Danian (en)
dbp:prilithology
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  • Cape Lamb & Lower Sandwich Bluff Members (en)
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  • Marambio & Seymour Island Groups (en)
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  • The Lopez de Bertodano Formation is a geological formation in the James Ross archipelago of the Antarctic Peninsula. The strata date from the end of the Late Cretaceous (upper-lower Maastrichtian stage) to the Danian stage of the lower Paleocene, from about 70 to 65.5 million years ago, straddling the Cretaceous-Paleogene boundary. (en)
  • La formation de Lopez de Bertodano est une formation géologique affleurant sur l'île Seymour, dans l'archipel de James Ross, sur la péninsule Antarctique. Les strates vont de la fin du Crétacé supérieur (étage du Maastrichtien) jusqu'au Danien inférieur (Paléocène), il y a environ entre 70 et 65,5 Ma (millions d'années). (fr)
rdfs:label
  • Formation de Lopez de Bertodano (fr)
  • Lopez de Bertodano Formation (en)
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