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		<title>View of Pacific Coast Highway, California</title>
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		<dc:creator><![CDATA[Willi Van Boven]]></dc:creator>
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		<dc:creator><![CDATA[Willi Van Boven]]></dc:creator>
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		<dc:creator><![CDATA[Willi Van Boven]]></dc:creator>
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		<dc:creator><![CDATA[Willi Van Boven]]></dc:creator>
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		<title>Eshaness shores in Shetland</title>
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		<dc:creator><![CDATA[Willi Van Boven]]></dc:creator>
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					<description><![CDATA[Eshaness can boast one of the highest energy coastlines in the world. Blasted by the full force of the North Atlantic it displays a stunning array of stacks, blowholes and geos (narrow inlets). However, the Eshaness peninsula also tells a fascinating story of a long extinct volcano and a very different past environment.]]></description>
										<content:encoded><![CDATA[<p>During the Devonian period, 350 &#8211; 400 million years ago Shetland lay near the Equator at the heart of large supercontinent and experienced a tropical climate, which varied from wet and humid to dry and arid. The Eshaness volcano lay at the north end of a broad valley containing a massive freshwater lake called Lake Orcadie. The spectacular cliffs you see today cut right through the flank of what was the Eshaness volcano. It has been described as &#8216;the best section through the flank of a volcano in the British Isles&#8217; The cliffs reveal layer upon layer of lava and &#8216;pyroclastic&#8217; rock, (volcanic ash that was blasted through the air from the volcanic crater). As eruption followed eruption, these layers built up rapidly. They formed a very steep and unstable cone around a central vent, from which the lava and ash continued to spew. Although the cone at Eshaness eroded away long a fascinating array of volcanic features remain. These have been brought to life by Geopark Shetland in the self-guide trail &#8216;Shetland&#8217;s Volcano&#8217;.</p>
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		<dc:creator><![CDATA[Willi Van Boven]]></dc:creator>
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		<dc:creator><![CDATA[Willi Van Boven]]></dc:creator>
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					<description><![CDATA[Eshaness can boast one of the highest energy coastlines in the world. Blasted by the full force of the North Atlantic it displays a stunning array of stacks, blowholes and geos (narrow inlets). However, the Eshaness peninsula also tells a fascinating story of a long extinct volcano and a very different past environment.]]></description>
										<content:encoded><![CDATA[<p>During the Devonian period, 350 &#8211; 400 million years ago Shetland lay near the Equator at the heart of large supercontinent and experienced a tropical climate, which varied from wet and humid to dry and arid. The Eshaness volcano lay at the north end of a broad valley containing a massive freshwater lake called Lake Orcadie. The spectacular cliffs you see today cut right through the flank of what was the Eshaness volcano. It has been described as &#8216;the best section through the flank of a volcano in the British Isles&#8217; The cliffs reveal layer upon layer of lava and &#8216;pyroclastic&#8217; rock, (volcanic ash that was blasted through the air from the volcanic crater). As eruption followed eruption, these layers built up rapidly. They formed a very steep and unstable cone around a central vent, from which the lava and ash continued to spew. Although the cone at Eshaness eroded away long a fascinating array of volcanic features remain. These have been brought to life by Geopark Shetland in the self-guide trail &#8216;Shetland&#8217;s Volcano&#8217;.</p>
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