Connected Sites
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The Causeway Coast Has An Unparalleled Display Of Geological Formations Representing Volcanic Activity During The Early Tertiary Period Some 50-60 Million Years Ago. (Ab Ev)
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Chemical Analysis And Geological Evidence Suggests That The Pinnacles Were Created Some 60 Million Years Ago In The Tertiary Period, Emerging From The Cone Of A River And Further Transformed By Earthquakes (Ab Ev)
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Created As Part Of The British Tertiary Volcanic Province During The Volcanic Activity Of The Palaeocene And Early Eocene (C63-52ma) Which Accompanied The Early Stages Of The Opening Of The N Atlantic.
See Www.Kilda.Org.Uk
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At About 90ma Madagascar Parted From India And Seychelles. The Isolation Of The Seychelles Was Completed At About 65ma When India And Seychelles Drifted Apart
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Most Of The Elevations Of Serra Do Mar Were Formed About 60 Million Years Ago. (Wiki)
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Having Completed Its Separation From All Other Land Masses More Than 60 Million Years Ago, Madagascar's Plant And Animal Life Evolved In Isolation. (Wiki)
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Records The Exact Boundary Between 2 Periods (Cretacious-Paleocene)
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