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The Potsdam Sandstone, more formally known as the Potsdam Group, is a geologic unit of mid-to-late Cambrian age found in Northern New York and northern Vermont and Quebec and Ontario. A well-cemented sandstone of nearly pure quartz, in the 19th century it was widely used in construction and in refractory linings for iron furnaces.

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  • Grès de Potsdam (fr)
  • Potsdam Sandstone (en)
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  • Le grès de Potsdam, formellement groupe de Potsdam, est une formation géologique datant du milieu à la fin du Cambrien située au nord des états américains de New York et du Vermont) ainsi qu'au sud du Québec. Ce grès, découvert au XIXe siècle, est formé par cimentation de grains de quartz. Il est utilisé dans la construction, les réfractaires et les garnitures de fours pour la fusion des métaux. (fr)
  • The Potsdam Sandstone, more formally known as the Potsdam Group, is a geologic unit of mid-to-late Cambrian age found in Northern New York and northern Vermont and Quebec and Ontario. A well-cemented sandstone of nearly pure quartz, in the 19th century it was widely used in construction and in refractory linings for iron furnaces. (en)
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  • Potsdam Sandstone (en)
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  • http://commons.wikimedia.org/wiki/Special:FilePath/PotsdamSandstone_Diplocraterion.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/PotsdamSandstone_xbeds.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Potsdam_Protichnites.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/SnellHall(2009).jpg
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