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        <name>Dublin Core</name>
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          <element elementId="50">
            <name>Title</name>
            <description>A name given to the resource</description>
            <elementTextContainer>
              <elementText elementTextId="3233">
                <text>Igneous Rocks</text>
              </elementText>
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          <element elementId="49">
            <name>Subject</name>
            <description>The topic of the resource</description>
            <elementTextContainer>
              <elementText elementTextId="3234">
                <text>This collection covers both volcanic and intrusive rocks, including rhyolites, granites, diorites, andesites, basalts, gabbros, diabases, pumices, obsidians, syenites, phonolites, peridotites, carbonatites, dacites, trachyte, dunites, xenoliths, ignimbrites, and pegmatites.</text>
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          <element elementId="39">
            <name>Creator</name>
            <description>An entity primarily responsible for making the resource</description>
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              <elementText elementTextId="3235">
                <text>Bereket Haileab</text>
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          <element elementId="48">
            <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>
              </elementText>
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          <element elementId="42">
            <name>Format</name>
            <description>The file format, physical medium, or dimensions of the resource</description>
            <elementTextContainer>
              <elementText elementTextId="3258">
                <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>Hand sample</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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        <element elementId="50">
          <name>Title</name>
          <description>A name given to the resource</description>
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              <text>BH250-231a</text>
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        <element elementId="49">
          <name>Subject</name>
          <description>The topic of the resource</description>
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              <text>Ankaramite</text>
            </elementText>
          </elementTextContainer>
        </element>
        <element elementId="38">
          <name>Coverage</name>
          <description>The spatial or temporal topic of the resource, the spatial applicability of the resource, or the jurisdiction under which the resource is relevant</description>
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            <elementText elementTextId="2322">
              <text>Location: Hawaii, USA</text>
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        <element elementId="40">
          <name>Date</name>
          <description>A point or period of time associated with an event in the lifecycle of the resource</description>
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              <text>2022</text>
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          <name>Source</name>
          <description>A related resource from which the described resource is derived</description>
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            <elementText elementTextId="2325">
              <text>From the rock collection of Bereket Haileab. Sample 231a. Housed at Carleton College in Minnesota.</text>
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        </element>
        <element elementId="51">
          <name>Type</name>
          <description>The nature or genre of the resource</description>
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              <text>Hand sample and thin section</text>
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          </elementTextContainer>
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        <element elementId="41">
          <name>Description</name>
          <description>An account of the resource</description>
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              <text>&lt;p data-start="68" data-end="162"&gt;Major Minerals: diopside, olivine, plagioclase&lt;br data-start="118" data-end="121" /&gt;Minor Minerals: titanaugite, oxides&lt;/p&gt;&#13;
&lt;p data-start="164" data-end="543"&gt;Optics: Euhedral olivine, pyroxenes, and plagioclase feldspars are present. Many of the olivine and pyroxene grains are cut perpendicular to their optical axes and display beautiful interference figures. Some olivines exhibit undulose extinction, indicating deformation in the molten magma. Well-developed Carlsbad twinning is observed in olivine, pyroxenes, and plagioclase.&lt;/p&gt;&#13;
&lt;p data-start="545" data-end="758"&gt;Texture: Porphyritic with phenocrysts in a fine-grained groundmass; agglomerated crystal clusters and vesicular features are present. In hand sample, some phenocrysts measure up to 1.5 centimeters in diameter.&lt;/p&gt;&#13;
&lt;p data-start="760" data-end="1056"&gt;Hand Sample: This rock is mapped as an ankaramite, a rare, mafic to ultramafic, dark-colored volcanic rock that is notably rich in large mafic phenocrysts, particularly olivine and clinopyroxene (diopside). It is named after Ankaramy, a locality in Madagascar where it was first described.&lt;/p&gt;&#13;
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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=9a2aa4f8d3834eefa7c1d1b01249e3b0" 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=9a2aa4f8d3834eefa7c1d1b01249e3b0"&gt;here&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;iframe width="100%" height="480" src="https://drive.google.com/file/d/1KF0I5SICCeKCTSgnh_hgv7o3DJU0hmZu/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/1Wcm67qrnDTynNu4YLKs1xLuLqNoAFbId/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/1VPiFhzP-qC59XxMJ2FwXTgVYkB0tPMyg/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/1b7Cr6nZYZfU9rv-jzvl9OzhWvNVkJ1Y-/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/1_-uq3qPEYj2QrGDGsQ5kQQxVgN9r3IBN/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/1S_qOPk375oT9uyv6vDxB0RWSAVjTT6wF/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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      <name>Agglomerated crystals</name>
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    <tag tagId="672">
      <name>Andalusite extinction</name>
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    <tag tagId="668">
      <name>Ankaramite</name>
    </tag>
    <tag tagId="38">
      <name>basanite</name>
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    <tag tagId="382">
      <name>Carlsbad twinning</name>
    </tag>
    <tag tagId="251">
      <name>Diopside</name>
    </tag>
    <tag tagId="671">
      <name>Diopside twining</name>
    </tag>
    <tag tagId="237">
      <name>Euhedral pyroxene</name>
    </tag>
    <tag tagId="674">
      <name>Glomeroporphyritic</name>
    </tag>
    <tag tagId="669">
      <name>Hawaii volcanic rocks</name>
    </tag>
    <tag tagId="5">
      <name>igneous</name>
    </tag>
    <tag tagId="7">
      <name>mafic</name>
    </tag>
    <tag tagId="353">
      <name>mafic volcanic rock</name>
    </tag>
    <tag tagId="474">
      <name>Olivine phenocrysts</name>
    </tag>
    <tag tagId="670">
      <name>Plagioclase twinning</name>
    </tag>
    <tag tagId="190">
      <name>porphyritic texture</name>
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    <tag tagId="227">
      <name>Titanaugite</name>
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    <tag tagId="188">
      <name>vesicular basalt</name>
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      <name>volcanic</name>
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    <tag tagId="675">
      <name>Volcanic phenocrysts</name>
    </tag>
    <tag tagId="673">
      <name>Wavy extinction</name>
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