Geology and the Evolution of Landscape in the Kerry Geopark
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 />
• The Pre – Atlantic Rift<strong>in</strong>g is <strong>the</strong> source <strong>of</strong><br />
<strong>the</strong> second major tectonic gra<strong>in</strong>;<br />
• A subsidiary NW – SE gra<strong>in</strong> may be part<br />
<strong>of</strong> <strong>the</strong> orig<strong>in</strong>al Armorican stress regime;<br />
• The geology is tw<strong>in</strong>ned on <strong>the</strong> o<strong>the</strong>r side<br />
<strong>of</strong> <strong>the</strong> Atlantic – Devonian s<strong>and</strong>stones <strong>and</strong><br />
shales (Gas source <strong>in</strong> <strong>the</strong> USA);<br />
• These structures def<strong>in</strong>e <strong>the</strong> <strong>Geopark</strong><br />
l<strong>and</strong>scape.