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          <element elementId="50">
            <name>Title</name>
            <description>A name given to the resource</description>
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              <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>
              </elementText>
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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>
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              <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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  <itemType itemTypeId="20">
    <name>Thin section and 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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            <elementText elementTextId="2006">
              <text>BH250-204</text>
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        <element elementId="49">
          <name>Subject</name>
          <description>The topic of the resource</description>
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              <text>Gabbro, Stillwater Complex </text>
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          <name>Description</name>
          <description>An account of the resource</description>
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              <text>Major Minerals: Enstatite (orthopyroxene), anorthite (plagioclase)&#13;
Minor Minerals: Augite (clinopyroxene), titanaugite (clinopyroxene), sulfide (visible in handsample), serpentine&#13;
&#13;
Texture: coarse grained, intrusive rock with ophitic texture.&#13;
&#13;
Optics: Well-formed (euhedral) pyroxene crystals are present, with interstitial plagioclase feldspars ranging from euhedral to subhedral, reflecting the sequence of crystallization an excellent example for interpreting phase relationships using a no-solid solution binary phase diagram. Exsolution lamellae are observed within orthopyroxene, hosting inclusions of clinopyroxene.&#13;
&#13;
Alteration:&#13;
There is strong evidence of hydrothermal fluid interaction, marked by vein formation and significant alteration of pyroxenes to serpentine. Additionally, late-stage crystallization of sulfides such as pyrite is evident.</text>
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          <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="2009">
              <text>Location: Montana, USA&#13;
GPS Coordinates: 45°23'21.17"N, 109°52'43.86"W</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="2011">
              <text>From the rock collection of Bereket Haileab. Sample BH250-204. 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>Thin section and hand sample</text>
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          <name>Relation</name>
          <description>A related resource</description>
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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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        <element elementId="37">
          <name>Contributor</name>
          <description>An entity responsible for making contributions to the resource</description>
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              <text>Bereket Haileab</text>
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      <name>Anorthite</name>
    </tag>
    <tag tagId="225">
      <name>Augite</name>
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    <tag tagId="226">
      <name>Clinopyroxene</name>
    </tag>
    <tag tagId="242">
      <name>Clinopyroxene inclusions</name>
    </tag>
    <tag tagId="235">
      <name>Coarse-grained</name>
    </tag>
    <tag tagId="220">
      <name>Enstatite</name>
    </tag>
    <tag tagId="237">
      <name>Euhedral pyroxene</name>
    </tag>
    <tag tagId="240">
      <name>Exsolution lamellae</name>
    </tag>
    <tag tagId="10">
      <name>gabbro</name>
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    <tag tagId="231">
      <name>Hydrothermal alteration</name>
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    <tag tagId="5">
      <name>igneous</name>
    </tag>
    <tag tagId="219">
      <name>Igneous petrology</name>
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    <tag tagId="239">
      <name>Interstitial plagioclase</name>
    </tag>
    <tag tagId="236">
      <name>Intrusive texture</name>
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    <tag tagId="217">
      <name>Layered mafic intrusion</name>
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    <tag tagId="7">
      <name>mafic</name>
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    <tag tagId="218">
      <name>Mafic intrusive</name>
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    <tag tagId="224">
      <name>Minor Minerals</name>
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    <tag tagId="216">
      <name>Montana geology</name>
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    <tag tagId="183">
      <name>olivine</name>
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      <name>Orthopyroxene</name>
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    <tag tagId="241">
      <name>Orthopyroxene host</name>
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    <tag tagId="223">
      <name>Plagioclase feldspar</name>
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    <tag tagId="9">
      <name>plutonic</name>
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      <name>Pyrite</name>
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    <tag tagId="232">
      <name>Pyroxene alteration</name>
    </tag>
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      <name>Serpentine (alteration)</name>
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      <name>Serpentinization</name>
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      <name>Stillwater Complex</name>
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      <name>Subhedral plagioclase</name>
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      <name>Sulfide minerals</name>
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      <name>Sulfide veins</name>
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    <tag tagId="227">
      <name>Titanaugite</name>
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