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            <name>Title</name>
            <description>A name given to the resource</description>
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                <text>Igneous Rocks</text>
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            <name>Subject</name>
            <description>The topic of the resource</description>
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                <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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            <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 and hand sample</name>
    <description/>
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          <name>Title</name>
          <description>A name given to the resource</description>
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              <text>BH250-131e</text>
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          <name>Subject</name>
          <description>The topic of the resource</description>
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              <text>Phonolite, Orendite, Orendite Wyominite, Lamproite</text>
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          <name>Description</name>
          <description>An account of the resource</description>
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              <text>Major Minerals: phlogopite, leucite &lt;br /&gt;Minor Minerals: apatite, diopside, orthoclase&lt;br /&gt;&lt;br /&gt;&#13;
&lt;p&gt;Leucite Hills, Wyoming is a geologically fascinating area situated within the Rock Springs Uplift of southwestern Wyoming. It is renowned for its rare, leucite-rich volcanic rocks. These rocks are composed predominantly of ultrapotassic volcanic lithologies, including leucitite a rock characterized by fine-grained to porphyritic textures and abundant leucite (KAlSi₂O₆). The samples from Leucite Hills were collected by Cameron Webb, Josh Zoellmer, and Anderson Cole class of 2014! Thank you, guys!&lt;/p&gt;&#13;
&lt;p&gt;Petrology and mineralogy:&lt;br /&gt;Leucite is the dominant feldspathoid mineral, commonly forming euhedral phenocrysts as well as fine grains within the groundmass.&lt;/p&gt;&#13;
&lt;p&gt;Phlogopite, a Ti-rich variety of mica, is widespread in some samples and appears as both groundmass flakes and phenocrysts.&lt;/p&gt;&#13;
&lt;p&gt;Nepheline occurs occasionally as an accessory feldspathoid mineral.&lt;/p&gt;&#13;
&lt;p&gt;&amp;nbsp;&lt;/p&gt;&#13;
&lt;p&gt;Geochemistry:&lt;br /&gt;The rocks are ultrapotassic, with K₂O contents often exceeding 10 wt% (see tables in chemical analysis) and plot in the phonolite field on the TAS diagram. They are rich in alkali oxides (Na₂O + K₂O) and display elevated concentrations of Large Ion Lithophile Elements (LILE) such as K, Rb, and Ba as seen in the spider diagram/Rare Earth Plot.&lt;/p&gt;&#13;
&lt;p&gt;Mica Types:&lt;br /&gt;The primary micas found in Leucite Hills volcanic rocks are, phlogopite, including Ti-rich varieties, which are compositionally distinct. These micas occur as well-formed phenocrysts (up to several millimeters in size) and are mineralogically and chemically significant indicators of mantle metasomatism and magmatic conditions.&lt;/p&gt;&#13;
&lt;br /&gt;&lt;iframe width="1800" height="100" src="https://docs.google.com/spreadsheets/d/e/2PACX-1vS4nyqCmZQGn3t6vX4g4nhDPwHMBaKrigt1LaY2pykWbBGXB1wNb6FYArx625I-JTtD7lyg4uz1OS1r/pubhtml?gid=2074065796&amp;amp;single=true&amp;amp;widget=true&amp;amp;headers=false"&gt;&lt;/iframe&gt;</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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              <text>Location: Leucite Hills, Wyoming, USA&#13;
Nearby Geographic Feature: Zirkel Mesa&#13;
GPS Coordinates: 41.7999068, -108.9228398</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 BH250-131e. Housed at Carleton College in Minnesota.</text>
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          <name>Contributor</name>
          <description>An entity responsible for making contributions to the resource</description>
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              <text>Bereket Haileab&#13;
Cameron Webb '14, Josh Zoellmer '14, and Anderson Cole '14</text>
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          <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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              <text>&lt;iframe width="100%" height="600" style="border: 0;" src="https://carleton.maps.arcgis.com/apps/instant/media/index.html?appid=e2bcc949a9b8447e83c8e832addee949" 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=e2bcc949a9b8447e83c8e832addee949"&gt;here&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;iframe width="100%" height="480" src="https://drive.google.com/file/d/1eZ0IcJuvYK_WAxlexXnXLgQjVTp0IF0D/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/1FJlD7T3yVXeJ2BTduUbl5PXIAITha7Vn/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/1N890rgeLdNhbIEWkLAPBigk0psjM4ie1/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/1y4Co33xBoWpXThSf5sif6aDCNmOuFXWS/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/1pj-qt4ijsXLPxmU9rRQ6ezzytt_UVMNO/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/1iNq5HYHhrReFMoGyTFOjzTS8fm-SPIwX/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/1Q26A0X0eXTZUTeDIK_Scap170Z5txjR4/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/1nnLF7ZHCbWYO3p-QmZ1PFlS4K6nITMJl/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/11WV2VTXe5FpzdgZx7hBav1eJskxBqr0X/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/1vNbLBQnJ2nfXPOFcxyS41-2YtUh0fcNN/preview" allow="autoplay"&gt;&lt;/iframe&gt;&lt;br /&gt;&lt;br /&gt;&lt;br /&gt;&lt;br /&gt;&lt;br /&gt;&lt;iframe width="100%" height="480" src="https://drive.google.com/file/d/1EG9UmZ03I6aYKQSIRm16jQUlOzz7zSZO/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/1gIQU3TaREAcJYlNvICoRmEry5l80MbcI/preview" allow="autoplay"&gt;&lt;/iframe&gt;&lt;br /&gt;TAS diagram of BH250-131e &lt;iframe width="100%" height="480" src="https://drive.google.com/file/d/1khKirwYAk86PCIJj6-Aq-pwCmWzDPDVv/preview" allow="autoplay"&gt;&lt;/iframe&gt;</text>
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          <description>An entity primarily responsible for making the resource</description>
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              <text>Bereket Haileab</text>
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      <name>Feldspathoid minerals</name>
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      <name>Feldspathoid volcanic rocks</name>
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    <tag tagId="1187">
      <name>High K₂O content</name>
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    <tag tagId="5">
      <name>igneous</name>
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      <name>intermediate</name>
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      <name>leucite</name>
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      <name>Leucite Hills</name>
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      <name>Leucitite</name>
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      <name>Orendite</name>
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      <name>Phlogopite</name>
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      <name>phonolite</name>
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      <name>Ti-rich phlogopite</name>
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      <name>Ultrapotassic composition</name>
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      <name>Ultrapotassic volcanic rocks</name>
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      <name>volcanic</name>
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    <tag tagId="1190">
      <name>Wyoming volcanics</name>
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      <name>Wyominite</name>
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      <name>Zirkel Mesa</name>
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