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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>
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              <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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                <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>
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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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    <name>Thin section and hand sample</name>
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          <name>Title</name>
          <description>A name given to the resource</description>
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              <text>BH250-41</text>
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        <element elementId="49">
          <name>Subject</name>
          <description>The topic of the resource</description>
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              <text>Dunite</text>
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              <text>Major Mineral: forsterite, olivine&lt;br /&gt;Minor Minerals: serpentine, magnetite&lt;br /&gt;Texture: equigranular olivine&lt;br /&gt;&lt;br /&gt;&#13;
&lt;p&gt;BH250-41 is a dunite from&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;span&gt;Balsam&lt;/span&gt;, composed almost entirely of forsterite-rich&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;span&gt;Olivine&lt;/span&gt;. It is one of the most visually striking rocks, both in hand sample and especially in thin section. Under crossed polars, the olivine grains display vivid second-order interference colors. Well-oriented grains cut perpendicular to the c-axis yield excellent biaxial interference figures, with a 2V angle close to 90°, making the mineral appear nearly optically neutral. In this orientation, the isogyre forms a straight line that rotates smoothly about the optic axis—an ideal demonstration for teaching optical mineralogy.&lt;/p&gt;&#13;
&lt;p data-start="674" data-end="1214"&gt;On the Olivine–Orthopyroxene–Clinopyroxene (Ol–Opx–Cpx) ternary diagram used for ultramafic igneous rock classification, dunite plots near the olivine apex because it contains more than 90% olivine, with only minor pyroxene if present. BH250-41 would therefore plot very close to the Ol corner of the diagram, firmly within the dunite field. This position reflects its highly magnesium-rich, mantle-derived composition and distinguishes it from harzburgite, lherzolite, and pyroxenite fields that contain greater proportions of pyroxenes.&lt;/p&gt;&#13;
&lt;p data-start="1216" data-end="1664"&gt;Optically, olivine exhibits strong birefringence, producing bright second-order rainbow-like interference colors. It is biaxial with a 2V angle of approximately 90°, and in favorable orientations may appear nearly optically neutral. This sample provides excellent teaching examples for selecting grains that produce an optic-axis interference figure and for demonstrating the difference between biaxial and uniaxial behavior under the microscope.&lt;/p&gt;&#13;
&lt;p data-start="1666" data-end="2191"&gt;BH250-41 also shows evidence in some thin sections of later metamorphic or alteration reactions, where primary olivine has begun to break down along fractures or grain margins. Common reactions include hydration to&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;span&gt;Serpentine&lt;/span&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;or talc-bearing assemblages, recording fluid infiltration after crystallization. These secondary textures provide an excellent contrast between pristine mantle olivine and later alteration during tectonic uplift and weathering. A simplified serpentinization reaction is:&lt;/p&gt;&#13;
&lt;span class="base"&gt;&lt;span class="strut"&gt;&lt;/span&gt;&lt;span class="mord"&gt;3(&lt;/span&gt;&lt;span class="mspace"&gt;&lt;/span&gt;&lt;span class="mord"&gt;&lt;span class="mord text"&gt;MgFe)&lt;/span&gt;&lt;span class="msupsub"&gt;&lt;span class="vlist-t vlist-t2"&gt;&lt;span class="vlist-r"&gt;&lt;span class="vlist"&gt;&lt;span&gt;&lt;span class="sizing reset-size6 size3 mtight"&gt;&lt;span class="mord mtight"&gt;2&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;span class="vlist-s"&gt;​&lt;/span&gt;&lt;/span&gt;&lt;span class="vlist-r"&gt;&lt;span class="vlist"&gt;&lt;span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;span class="mord"&gt;&lt;span class="mord text"&gt;SiO&lt;/span&gt;&lt;span class="msupsub"&gt;&lt;span class="vlist-t vlist-t2"&gt;&lt;span class="vlist-r"&gt;&lt;span class="vlist"&gt;&lt;span&gt;&lt;span class="pstrut"&gt;&lt;/span&gt;&lt;span class="sizing reset-size6 size3 mtight"&gt;&lt;span class="mord 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mtight"&gt;2&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;span class="vlist-s"&gt;​&lt;/span&gt;&lt;/span&gt;&lt;span class="vlist-r"&gt;&lt;span class="vlist"&gt;&lt;span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;span class="mord text"&gt;&lt;span class="mord"&gt;O &lt;/span&gt;&lt;/span&gt;&lt;span class="mspace"&gt;&lt;/span&gt;&lt;span class="mbin"&gt;+ 2&lt;/span&gt;&lt;span class="mspace"&gt;&lt;/span&gt;&lt;/span&gt;&lt;span class="base"&gt;&lt;span class="strut"&gt;&lt;/span&gt;&lt;span class="mord"&gt;&lt;span class="mord text"&gt;O&lt;/span&gt;&lt;span class="msupsub"&gt;&lt;span class="vlist-t vlist-t2"&gt;&lt;span class="vlist-r"&gt;&lt;span class="vlist"&gt;&lt;span&gt;&lt;span class="pstrut"&gt;&lt;/span&gt;&lt;span class="sizing reset-size6 size3 mtight"&gt;&lt;span class="mord mtight"&gt;2 &lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;span class="vlist-s"&gt;​&lt;/span&gt;&lt;/span&gt;&lt;span class="vlist-r"&gt;&lt;span class="vlist"&gt;&lt;span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;span class="mspace"&gt;&lt;/span&gt;&lt;span class="mrel"&gt;→ &lt;/span&gt;&lt;span class="mspace"&gt;&lt;/span&gt;&lt;/span&gt;&lt;span class="base"&gt;&lt;span class="strut"&gt;&lt;/span&gt;&lt;span class="mord"&gt;2&lt;/span&gt;&lt;span class="mspace"&gt;&lt;/span&gt;&lt;span class="mord"&gt;&lt;span class="mord text"&gt;Mg&lt;/span&gt;&lt;span class="msupsub"&gt;&lt;span class="vlist-t vlist-t2"&gt;&lt;span class="vlist-r"&gt;&lt;span class="vlist"&gt;&lt;span&gt;&lt;span class="pstrut"&gt;&lt;/span&gt;&lt;span class="sizing reset-size6 size3 mtight"&gt;&lt;span class="mord mtight"&gt;3&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;span class="vlist-s"&gt;​&lt;/span&gt;&lt;/span&gt;&lt;span class="vlist-r"&gt;&lt;span class="vlist"&gt;&lt;span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;span class="mord"&gt;&lt;span class="mord text"&gt;Si&lt;/span&gt;&lt;span class="msupsub"&gt;&lt;span class="vlist-t vlist-t2"&gt;&lt;span class="vlist-r"&gt;&lt;span class="vlist"&gt;&lt;span&gt;&lt;span class="pstrut"&gt;&lt;/span&gt;&lt;span class="sizing reset-size6 size3 mtight"&gt;&lt;span class="mord mtight"&gt;2&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;span class="vlist-s"&gt;​&lt;/span&gt;&lt;/span&gt;&lt;span class="vlist-r"&gt;&lt;span class="vlist"&gt;&lt;span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;span class="mord"&gt;&lt;span class="mord text"&gt;O&lt;/span&gt;&lt;span class="msupsub"&gt;&lt;span class="vlist-t vlist-t2"&gt;&lt;span class="vlist-r"&gt;&lt;span class="vlist"&gt;&lt;span&gt;&lt;span class="pstrut"&gt;&lt;/span&gt;&lt;span class="sizing reset-size6 size3 mtight"&gt;&lt;span class="mord mtight"&gt;5&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;span class="vlist-s"&gt;​&lt;/span&gt;&lt;/span&gt;&lt;span class="vlist-r"&gt;&lt;span class="vlist"&gt;&lt;span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;span class="mopen"&gt;(&lt;/span&gt;&lt;span class="mord text"&gt;&lt;span class="mord"&gt;OH&lt;/span&gt;&lt;/span&gt;&lt;span class="mclose"&gt;)&lt;span class="msupsub"&gt;&lt;span class="vlist-t vlist-t2"&gt;&lt;span class="vlist-r"&gt;&lt;span class="vlist"&gt;&lt;span&gt;&lt;span class="pstrut"&gt;&lt;/span&gt;&lt;span class="sizing reset-size6 size3 mtight"&gt;&lt;span class="mord mtight"&gt;4&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;span class="vlist-s"&gt;​&lt;/span&gt;&lt;/span&gt;&lt;span class="vlist-r"&gt;&lt;span class="vlist"&gt;&lt;span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;span class="mspace"&gt;&amp;nbsp;&lt;/span&gt;&lt;span class="mopen"&gt;(&lt;/span&gt;&lt;span class="mord text"&gt;&lt;span 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          <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 BH250-41. Housed at Carleton College in Minnesota.</text>
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              <text>Thin section and hand sample</text>
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          <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=426a8f55a4dd483ca317808ef82f20b1" 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=426a8f55a4dd483ca317808ef82f20b1"&gt;here&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;iframe width="100%" height="480" src="https://drive.google.com/file/d/1jl-5KZUFAbm3UuhI4czX0CYXcsifXOx_/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/1XNRniVB7aQWWoA32Awlp84vfqnY4pQjf/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/1JxfcXWHXAREtxcQbCNqg2jwhizTYm1gS/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-kPFzgN1RKuRHHMx5zRVGLUSgrgEkpZ9/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/1TMNilt8f60JiiP_3EX-Dv4xx1iqjWLqZ/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/1bjNP6Carp4RV_n0Oa4LwSaLjgoXAJyHQ/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/1SSMdVlf18yv7Ym6pMgNjbcEWnzivo9ls/preview" allow="autoplay"&gt;&lt;iframe width="100%" height="480" src="https://drive.google.com/file/d/16puBbmOxWiVoP3uob8vl77dopCZMb-TN/preview" allow="autoplay"&gt;&lt;/iframe&gt;&lt;/iframe&gt;&lt;br /&gt;&lt;br /&gt;&lt;iframe width="100%" height="480" src="https://drive.google.com/file/d/1hAKVyzvfRGUrVR48Gz_x8tlaJhnA22e2/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/19de2VzZluIHRhS1XeGj1o698koJ1a54B/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/1HGpg9JcT-Yw95b5cSDeZKxw6cpXmymYI/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/11TP06iGOAdc7PzLO_fcPOsIGu86wDL1k/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/1pRgBMlIT55SDEiEBJsTN_J3uxKULfKOZ/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/18RkeyPoKqbBhrd9xUctkuQyMvWJgiyCe/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/1ecsjbkhjcqomvTr9iMPHCABFNW65KHR6/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/1TFMweiUFlfx_CZdr5konqpY3688xrU0R/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/1NKZYYB89d5aDJXEw2IHZCQiprJyzeJCz/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/1FRACWu5QIyv1cTH6sRVVwMcj3W2S-k7k/preview" allow="autoplay"&gt;&lt;/iframe&gt;&lt;iframe width="100%" height="480" src="https://drive.google.com/file/d/1RvzxN4kC6bCy5rj0GR7W0Y0vy1fXgaAl/preview" allow="autoplay"&gt;&lt;/iframe&gt;&lt;iframe width="100%" height="480" src="https://drive.google.com/file/d/1kHxXUzDP6nQgZd82XaIicz3EUJ_KH_Z6/preview" allow="autoplay"&gt;&lt;/iframe&gt;&lt;iframe width="100%" height="480" src="https://drive.google.com/file/d/16puBbmOxWiVoP3uob8vl77dopCZMb-TN/preview" allow="autoplay"&gt;&lt;/iframe&gt;</text>
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              <text>Bereket Haileab</text>
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              <text>Balsam, North Carolina, USA</text>
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      <name>2V ~90°</name>
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      <name>2V angle</name>
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    <tag tagId="145">
      <name>2V measurements</name>
    </tag>
    <tag tagId="135">
      <name>Balsam</name>
    </tag>
    <tag tagId="1553">
      <name>Balsam NC</name>
    </tag>
    <tag tagId="138">
      <name>biaxial</name>
    </tag>
    <tag tagId="885">
      <name>Biaxial Mineral</name>
    </tag>
    <tag tagId="139">
      <name>biaxial neutral</name>
    </tag>
    <tag tagId="129">
      <name>cumulate</name>
    </tag>
    <tag tagId="579">
      <name>cumulate rock</name>
    </tag>
    <tag tagId="19">
      <name>dunite</name>
    </tag>
    <tag tagId="131">
      <name>equigranular</name>
    </tag>
    <tag tagId="118">
      <name>euhedral</name>
    </tag>
    <tag tagId="1922">
      <name>Fo-rich olivine</name>
    </tag>
    <tag tagId="122">
      <name>forsterite</name>
    </tag>
    <tag tagId="130">
      <name>granular texture</name>
    </tag>
    <tag tagId="142">
      <name>high relief</name>
    </tag>
    <tag tagId="5">
      <name>igneous</name>
    </tag>
    <tag tagId="1932">
      <name>igneous rock classification</name>
    </tag>
    <tag tagId="1554">
      <name>Interference Colors</name>
    </tag>
    <tag tagId="144">
      <name>interference figure</name>
    </tag>
    <tag tagId="1298">
      <name>Isogyre</name>
    </tag>
    <tag tagId="213">
      <name>Magnetite</name>
    </tag>
    <tag tagId="127">
      <name>mantle derived</name>
    </tag>
    <tag tagId="1919">
      <name>mantle rock</name>
    </tag>
    <tag tagId="128">
      <name>mantle xenolith</name>
    </tag>
    <tag tagId="365">
      <name>mantle-derived magma</name>
    </tag>
    <tag tagId="132">
      <name>Mg rich olivine</name>
    </tag>
    <tag tagId="136">
      <name>North Carolina</name>
    </tag>
    <tag tagId="1931">
      <name>Ol-Opx-Cpx classification</name>
    </tag>
    <tag tagId="183">
      <name>olivine</name>
    </tag>
    <tag tagId="134">
      <name>olivine peridotite</name>
    </tag>
    <tag tagId="1930">
      <name>olivine-rich rock</name>
    </tag>
    <tag tagId="143">
      <name>optic axis figure</name>
    </tag>
    <tag tagId="1933">
      <name>optically neutral orientation</name>
    </tag>
    <tag tagId="58">
      <name>peridotite</name>
    </tag>
    <tag tagId="133">
      <name>peridotite suite</name>
    </tag>
    <tag tagId="9">
      <name>plutonic</name>
    </tag>
    <tag tagId="252">
      <name>Serpentine</name>
    </tag>
    <tag tagId="233">
      <name>Serpentinization</name>
    </tag>
    <tag tagId="1934">
      <name>talc alteration</name>
    </tag>
    <tag tagId="126">
      <name>ultrabasic</name>
    </tag>
    <tag tagId="18">
      <name>ultramafic</name>
    </tag>
    <tag tagId="244">
      <name>Ultramafic rock</name>
    </tag>
    <tag tagId="1920">
      <name>upper mantle</name>
    </tag>
    <tag tagId="137">
      <name>USA</name>
    </tag>
  </tagContainer>
</item>
