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<item xmlns="http://omeka.org/schemas/omeka-xml/v5" itemId="8" public="1" featured="0" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://omeka.org/schemas/omeka-xml/v5 http://omeka.org/schemas/omeka-xml/v5/omeka-xml-5-0.xsd" uri="https://bereket-haileab.geology.sites.carleton.edu/items/show/8?output=omeka-xml" accessDate="2026-10-22T12:59:51+00:00">
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      <src>https://bereket-haileab.geology.sites.carleton.edu/files/original/c24e79b749a001892d830bd1dd5d80f2.jpeg</src>
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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="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>
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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>
              </elementText>
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  <itemType itemTypeId="18">
    <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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        <element elementId="50">
          <name>Title</name>
          <description>A name given to the resource</description>
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              <text>BH250-8</text>
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        <element elementId="49">
          <name>Subject</name>
          <description>The topic of the resource</description>
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            <elementText elementTextId="65">
              <text>Tuff</text>
            </elementText>
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        <element elementId="41">
          <name>Description</name>
          <description>An account of the resource</description>
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            <elementText elementTextId="66">
              <text>Major Mineral: hornblende &lt;br /&gt;Minor Mineral: clinopyroxene altering to chlorite, sanidine, titanite, sericite, calcite, apatite&lt;br /&gt;Click &lt;a href="https://www.digitalscope.org/ViewerUI/?SlideId=6ebde66b-c6cc-4d73-9f0d-d3b95ab923e9"&gt;here&lt;/a&gt; for a high resolution scan&lt;br /&gt;&lt;br /&gt;&#13;
&lt;p&gt;BH250-8 is a strikingly beautiful tuff with rich mineralogical features. It contains basaltic hornblende—some crystals showing zoning—as well as both orthopyroxene (OPX) and clinopyroxene (CPX), with some CPX grains displaying anomalous interference colors. Scattered quartz grains are also present. Plagioclase feldspars exhibit alteration to sericite, while portions of the pyroxene have altered to chlorite. Accessory minerals include sphene (titanite) and exceptionally large, well-formed apatite grains—some cut parallel and others perpendicular to the c-axis, clearly revealing basal cleavage. Secondary calcite occurs along veins and voids, and the groundmass contains devitrified and recrystallized volcanic glass. This is a particularly beautiful and mineralogically diverse sample.&lt;br /&gt;&lt;br /&gt;There are several apatite crystals cut parallel to the C-axis that can be used to determine, length fast, length slow optical property as seeing in the video.&lt;/p&gt;</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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            <elementText elementTextId="68">
              <text>From the rock collection of Bereket Haileab. Sample 8. Housed at Carleton College in Minnesota.</text>
            </elementText>
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        <element elementId="51">
          <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=a0a0bd40ee6449d08239c495b3b69bb1" 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/apps/instant/media/index.html?appid=a0a0bd40ee6449d08239c495b3b69bb1"&gt;here&lt;/a&gt;&lt;a href="https://carleton.maps.arcgis.com/home/item.html?id=056af387bc7d45bfa762ccd20d45d96b"&gt;&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;iframe width="100%" height="480" src="https://drive.google.com/file/d/1l1qnS723ph71--VAF8_tRN7Le8kF1tuk/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/1RLGeQ-VcaA7zH_smwNBkhCsStR0373xF/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/16yGJO2oSAeTCLLqrpCFhaXAqKyT2QPiY/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/1AvJn02wCKcxl5B1SH2pDX0CbCUhdn8jo/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/14ys7YVosrwZHm8btnye6V3icL0Yat75H/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/1KFSPbximkQlk4u5dP6npU1vcpwNzmSMz/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/1WShR3AY9pJWG9emTk9UJJ9wxRjBoBiUX/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/1GIwdoePJw8pxnya8ASrhnBiqGe8H-TgX/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/16QhBGImpt3pfYPi4NncYW_s2_fKJGZC7/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_MRN8sEFPw-pKXoHYRjRxiI3CV0nQuDy/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/1d4vuWNWZ0y9bJ-b8P4odEB8JdYlOekWI/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/1jKnVwGcI6KjmDOWoVWQZoJBEEKxN9U7H/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/1mk0r0kcv46_RnyQn4f73Y3RdJIokn-TD/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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  </elementSetContainer>
  <tagContainer>
    <tag tagId="1538">
      <name>Alteration (sericite</name>
    </tag>
    <tag tagId="286">
      <name>Anomalous interference colors</name>
    </tag>
    <tag tagId="271">
      <name>Apatite</name>
    </tag>
    <tag tagId="8">
      <name>basalt</name>
    </tag>
    <tag tagId="1534">
      <name>Basaltic hornblende</name>
    </tag>
    <tag tagId="1539">
      <name>chlorite)</name>
    </tag>
    <tag tagId="1536">
      <name>Clinopyroxene (CPX)</name>
    </tag>
    <tag tagId="815">
      <name>Devitrified Glass</name>
    </tag>
    <tag tagId="536">
      <name>Hornblende</name>
    </tag>
    <tag tagId="5">
      <name>igneous</name>
    </tag>
    <tag tagId="1541">
      <name>length fast</name>
    </tag>
    <tag tagId="1542">
      <name>length slow</name>
    </tag>
    <tag tagId="7">
      <name>mafic</name>
    </tag>
    <tag tagId="1537">
      <name>Orthopyroxene (OPX)</name>
    </tag>
    <tag tagId="1540">
      <name>Recrystallization</name>
    </tag>
    <tag tagId="618">
      <name>Titanite (Sphene)</name>
    </tag>
    <tag tagId="1036">
      <name>Titanoaugite</name>
    </tag>
    <tag tagId="24">
      <name>tuff</name>
    </tag>
    <tag tagId="6">
      <name>volcanic</name>
    </tag>
    <tag tagId="23">
      <name>volcaniclastic</name>
    </tag>
    <tag tagId="1409">
      <name>welded tuff</name>
    </tag>
    <tag tagId="1535">
      <name>Zoned minerals</name>
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