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    <name>Site</name>
    <description>Represents a site.</description>
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        <name>Show Point</name>
        <description/>
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            <text>true</text>
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        <name>Prim Media</name>
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        <element elementId="50">
          <name>Title</name>
          <description>A name given to the resource</description>
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              <text>The Blue Stane</text>
            </elementText>
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        </element>
        <element elementId="48">
          <name>Source</name>
          <description>A related resource from which the described resource is derived</description>
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              <text>mathematicalycurious</text>
            </elementText>
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        <element elementId="43">
          <name>Identifier</name>
          <description>An unambiguous reference to the resource within a given context</description>
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              <text>291</text>
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          <name>Type</name>
          <description>The nature or genre of the resource</description>
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              <text>Site</text>
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        <element elementId="79">
          <name>Spatial Coverage</name>
          <description>Spatial characteristics of the resource.</description>
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              <text>current,56.34006274390947,-2.801288366317749;</text>
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          <name>Description</name>
          <description>An account of the resource</description>
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              <text>The Blue Stane is a relic of Pre-Christian Pictish St. Andrews when it had some now forgotten ritual significance. It is reputed to have been the coronation stone of Kenneth MacAlpine, who united the Kingdom of the Scots and the Picts in 843 A.D. &#13;
&#13;
The Stane is shown on the John Geddy map of St. Andrews (1580), at which time it stood on the south side of what is now Double Dykes Road. It later stood at the City Road crossroads and was moved here in Victorian times. It may have also once stood by the West Port.&#13;
&#13;
Geologically, the Stane is made of Dolerite (or Whinstone), an iron and magnesium-rich igneous rock found on Drumcarrow Craig. It was probably plucked by glaciers which covered Fife during the last ice age and was then dropped nearby as a glacial erratic when the ice retreated about 14000 years ago. </text>
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          <name>Date</name>
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              <text>1580</text>
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        <element elementId="37">
          <name>Contributor</name>
          <description>An entity responsible for making contributions to the resource</description>
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              <text>sjv1@st-andrews.ac.uk</text>
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        <element elementId="49">
          <name>Subject</name>
          <description>The topic of the resource</description>
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              <text>Natural History,Photography</text>
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      <name>Europeana</name>
      <description>Specific elements of the Europeana Semantic Elements.</description>
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          <name>Europeana Type</name>
          <description>The Europeana material type of the resource.</description>
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              <text>TEXT</text>
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