Connected Sites
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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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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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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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records the exact boundary between 2 periods (Cretacious-Paleocene)
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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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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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Most of the elevations of Serra do Mar were formed about 60 million years ago. (wiki)
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