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            <name>Title</name>
            <description>A name given to the resource</description>
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                <text>Metamorphic Rocks</text>
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            <name>Subject</name>
            <description>The topic of the resource</description>
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                <text>This collection includes slates, phyllites, schists, gneisses, eclogites, marbles, quartzites, skarns, granulites, and mylonites.</text>
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            <name>Creator</name>
            <description>An entity primarily responsible for making the resource</description>
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                <text>Bereket Haileab</text>
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            <name>Source</name>
            <description>A related resource from which the described resource is derived</description>
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                <text>Housed in Anderson Hall, Carleton College.</text>
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            <name>Format</name>
            <description>The file format, physical medium, or dimensions of the resource</description>
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                <text>Thin sections, thin section scans, hand samples, hand sample images, photomicrographs, chemical analyses (major elements, trace elements and REE analyses for selected samples).</text>
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    <name>Thin section</name>
    <description/>
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      <name>Dublin Core</name>
      <description>The Dublin Core metadata element set is common to all Omeka records, including items, files, and collections. For more information see, http://dublincore.org/documents/dces/.</description>
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          <name>Title</name>
          <description>A name given to the resource</description>
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              <text>BH250-79</text>
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          <name>Subject</name>
          <description>The topic of the resource</description>
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              <text>Marble</text>
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          <name>Description</name>
          <description>An account of the resource</description>
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              <text>Major Mineral: dolomite&#13;
Mineralogy Comments: dolomite has anomalous biaxial figures&#13;
&#13;
Compared to BH250-78, this marble originated from a very clean carbonate protolith, lacking siliceous or other non-carbonate materials. The carbonate minerals display well-developed twin lamellae, which can be used to distinguish between calcite and dolomite by locating the c-axis through relief changes and observing whether the c-axis forms an acute or obtuse angle with the twin lamellae. Additionally, many carbonate crystals are oriented favorably for obtaining clear interference figures under polarized light.</text>
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          <name>Source</name>
          <description>A related resource from which the described resource is derived</description>
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              <text>From the rock collection of Bereket Haileab. Sample 79. Housed at Carleton College in Minnesota.</text>
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          <name>Type</name>
          <description>The nature or genre of the resource</description>
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              <text>Thin section</text>
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          <name>Relation</name>
          <description>A related resource</description>
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              <text>&lt;iframe width="100%" height="600" style="border: 0;" src="https://carleton.maps.arcgis.com/apps/instant/media/index.html?appid=b1295b95cd6b4d8e9f6b8ff6d7f4b6ec" frameborder="0" allowfullscreen="allowfullscreen"&gt;iFrames are not supported on this page.&lt;/iframe&gt;&lt;br /&gt;View on ArcGIS Online &lt;a href="https://carleton.maps.arcgis.com/home/item.html?id=b1295b95cd6b4d8e9f6b8ff6d7f4b6ec"&gt;here&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;iframe width="100%" height="480" src="https://drive.google.com/file/d/1MiYSzUYPKaIimpDH9lQsLh1cnn0IAwbE/preview" allow="autoplay"&gt;&lt;/iframe&gt;&lt;br /&gt;&lt;br /&gt;&lt;iframe width="100%" height="480" src="https://drive.google.com/file/d/1wzdp6GT90z3YetUSYl4SkGuF1rBkzo2I/preview" allow="autoplay"&gt;&lt;/iframe&gt;&lt;br /&gt;&lt;br /&gt;&lt;iframe width="100%" height="480" src="https://drive.google.com/file/d/1pK8cHz7AqB9dVhmnnxwhXFQdgWiTq7CI/preview" allow="autoplay"&gt;&lt;/iframe&gt;</text>
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          <name>Creator</name>
          <description>An entity primarily responsible for making the resource</description>
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              <text>Bereket Haileab</text>
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    <tag tagId="1496">
      <name>C-axis orientation</name>
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      <name>Calcite</name>
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    <tag tagId="29">
      <name>carbonate</name>
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      <name>Carbonate Minerals</name>
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    <tag tagId="1495">
      <name>Clean carbonate protolith</name>
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    <tag tagId="884">
      <name>Dolomite</name>
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    <tag tagId="995">
      <name>Interference figures</name>
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    <tag tagId="32">
      <name>marble</name>
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    <tag tagId="1">
      <name>metamorphic</name>
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    <tag tagId="864">
      <name>relief</name>
    </tag>
    <tag tagId="893">
      <name>Twin Lamellae</name>
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