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The Palisades Sill is a Triassic, 200 Ma diabase intrusion. It extends through portions of New York and New Jersey. It is most noteworthy for The Palisades, the cliffs that rise steeply above the western bank of the Hudson River. The ideal location and accessibility of the sill, as well as its unique features, have generated much attention from nature enthusiasts, rock climbers, and geologists alike.

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  • Palisades Sill (en)
  • Palisades Sill (nl)
  • Soleira de Palisades (pt)
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  • The Palisades Sill is a Triassic, 200 Ma diabase intrusion. It extends through portions of New York and New Jersey. It is most noteworthy for The Palisades, the cliffs that rise steeply above the western bank of the Hudson River. The ideal location and accessibility of the sill, as well as its unique features, have generated much attention from nature enthusiasts, rock climbers, and geologists alike. (en)
  • De Palisades Sill is een uit het Trias stammende 200 Ma diabaas-intrusie (een sill). De diabaas dagzoomt in delen van New York en New Jersey. Palisades Sill is vooral noemenswaardig voor de , de kliffen die steil boven de westelijke oever van de Hudson uitsteken. De makkelijke toegankelijkheid van de sill maken het gebied populair bij veel natuurliefhebbers en geologen. (nl)
  • A Soleira de Palisades é uma intrusão ígnea que se localiza em Nova Jersey, no nordeste dos Estados Unidos da América. Formada há aproximadamente 190 milhões de anos, tem cerca de 330 metros de espessura com intrusões em arenito erodido do Triássico. A única intrusão humana na área é a Ponte George Washington. (pt)
foaf:depiction
  • http://commons.wikimedia.org/wiki/Special:FilePath/Palisades_Sill_from_Palisades_Parkway.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Palisades_Sill_near_Englewood_Cliffs.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Newark_Basin_Cross_Section.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Columnar_Jointing_in_the_Palisades_Sill.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Palisades_Sill_Location_Map.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Palisades_Sill_Olivine_Zone.jpg
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  • The Palisades Sill is a Triassic, 200 Ma diabase intrusion. It extends through portions of New York and New Jersey. It is most noteworthy for The Palisades, the cliffs that rise steeply above the western bank of the Hudson River. The ideal location and accessibility of the sill, as well as its unique features, have generated much attention from nature enthusiasts, rock climbers, and geologists alike. (en)
  • De Palisades Sill is een uit het Trias stammende 200 Ma diabaas-intrusie (een sill). De diabaas dagzoomt in delen van New York en New Jersey. Palisades Sill is vooral noemenswaardig voor de , de kliffen die steil boven de westelijke oever van de Hudson uitsteken. De makkelijke toegankelijkheid van de sill maken het gebied populair bij veel natuurliefhebbers en geologen. (nl)
  • A Soleira de Palisades é uma intrusão ígnea que se localiza em Nova Jersey, no nordeste dos Estados Unidos da América. Formada há aproximadamente 190 milhões de anos, tem cerca de 330 metros de espessura com intrusões em arenito erodido do Triássico. A única intrusão humana na área é a Ponte George Washington. (pt)
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