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Geology and the Evolution of Landscape in the Kerry Geopark

Geology and the Evolution of Landscape in the Kerry Geopark

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<strong>Geology</strong> <strong>and</strong> <strong>the</strong> <strong>Evolution</strong> <strong>of</strong> L<strong>and</strong>scape <strong>in</strong><br />

<strong>the</strong> <strong>Kerry</strong> <strong>Geopark</strong><br />

• <strong>Geology</strong> <strong>of</strong> <strong>the</strong> <strong>Geopark</strong> is dom<strong>in</strong>ated by<br />

Terrestrial Rocks <strong>of</strong> <strong>the</strong> Devonian (400 m.y.a)<br />

age. (Circa 5200 metres thickness).<br />

• Overwhelm<strong>in</strong>gly terrestrial / desert s<strong>and</strong>stones<br />

<strong>and</strong> lesser f<strong>in</strong>e gra<strong>in</strong>ed rocks.<br />

• A period <strong>of</strong> emergence <strong>of</strong> l<strong>and</strong> – based<br />

vertebrates, e.g. Tetrapods<br />

• Succeed<strong>in</strong>g Carboniferous rocks now largely<br />

eroded away but preserved to <strong>the</strong> East.

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