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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)
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)
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
See Www.Kilda.Org.Uk
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
Most Of The Elevations Of Serra Do Mar Were Formed About 60 Million Years Ago. (Wiki)
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)
Records The Exact Boundary Between 2 Periods (Cretacious-Paleocene)
