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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>
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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>
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          <name>Title</name>
          <description>A name given to the resource</description>
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              <text>BH250-49</text>
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          <name>Subject</name>
          <description>The topic of the resource</description>
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              <text>Sacred Heart Granite</text>
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          <description>An account of the resource</description>
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              <text>Major Minerals: microcline, orthoclase, quartz &lt;br /&gt;Minor Minerals: albite, biotite, muscovite, chlorite (pennite), sphene (titanite), zicon, monazite, oxides&lt;br /&gt;&lt;br /&gt;Mineralogy Comments: thin sections contain myrmekite&lt;br /&gt;Alteration: orthoclase and plagicalse are altered to sercite (white mica), biotite to chlorie alteration&lt;br /&gt;&lt;br /&gt;BH250-49 is from the Sacred Heart Granite near Belview, Minnesota—one of our regular stops on field trips to the Minnesota River Valley. The Sacred Heart Granite is a Neoarchean pluton that intruded the older Morton and Montevideo gneiss complexes around 2.604 Ga (2,604 million years ago). Recenlty Emma Watson a Carleton College student from the Class of 2023, worked on this rock and obtained revised age determinations for the pluton.&lt;br /&gt;&lt;br /&gt;The intrusion represents the final phase of high-grade metamorphic and deformational events that produced the Morton Gneiss and surrounding metamorphic rocks, closely tied to the last stages of Neoarchean convergent tectonics in the region.&lt;br /&gt;&lt;br /&gt;BH250-49 is a medium-grained, massive, and typically pink to gray granite, generally fresh and only weakly deformed relative to the surrounding gneisses. Its modal composition is approximately 40% K-feldspar, 30% oligoclase (a plagioclase feldspar), and 25% quartz, with subordinate amounts of biotite.&lt;br /&gt;&lt;br /&gt;&lt;br /&gt;&lt;iframe width="1800" height="100" src="https://docs.google.com/spreadsheets/d/e/2PACX-1vS4nyqCmZQGn3t6vX4g4nhDPwHMBaKrigt1LaY2pykWbBGXB1wNb6FYArx625I-JTtD7lyg4uz1OS1r/pubhtml?gid=861277415&amp;amp;single=true&amp;amp;widget=true&amp;amp;headers=false"&gt;&lt;/iframe&gt;</text>
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          <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: near Sacred Heart, Minnesota, USA&#13;
GPS Coordinates: 44°39'28.95"N, 95°20'17.19"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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              <text>From the rock collection of Bereket Haileab. Sample BH250-49. Housed at Carleton College in Minnesota.</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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          <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=d15b9b9ff56343b2a7f7fb383389579b" 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=d15b9b9ff56343b2a7f7fb383389579b"&gt;here&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;iframe width="100%" height="480" src="https://drive.google.com/file/d/1xV9z6lt_GaXvxOhVhKLsrLJeM9sx8kAb/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/1HHxB1Kf8w7AokVk0q0W42MHQ03v8epLM/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/1mAUsGHUCPcwVMSEBJgLyMn1lWp6ClTci/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/1X8sdx-v5spXwu-54zOyaw_OF-6UNuDa5/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/1IPz1fSoJK5xSSrQ8TScgUXqCPKRg_4vA/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/1AvEcO2Cdp0WldKFv2jgSfpmQTlvSvPRx/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/1jGCyph761elgX5LxhvELx4P4WnDL6rIw/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/1t5iZPoGpphPPSGJimdT--HhXYjBniCLP/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/18QucXLxZTH654KBYCHdYaOsnnypx9feI/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/13oTDzDW3JzV2wQILfKezfl3xmXdT8uyc/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/1SVQXdxCPpj_XGtXtJQ55jvebjl6lhHST/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/1IEkAGJuoz1YFkyooQRLoGW-nqcLI7p-y/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/1JvLMkCCNR9CjUGT1KUnqPykLOivYi8Df/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/1jzx2d2aQQBDTQSsIjX3prjiFyls7y1sA/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/134zJZG_GvAyRdwaQNQJpTi3A7LTVAP3b/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/1xh_SJO6zmhdn8xG1akxfBjUVXO79pgTd/preview" allow="autoplay"&gt;&lt;/iframe&gt;&lt;br /&gt;TAS diagram of sample BH250-49.</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>#Granite</name>
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      <name>albite</name>
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      <name>Belview MN</name>
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      <name>Biotite</name>
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      <name>Biotite to chlorite alteration</name>
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      <name>Chlorite (pennite)</name>
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      <name>Feldspar alteration</name>
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      <name>felsic</name>
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      <name>felsic igneous rock</name>
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      <name>granite</name>
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      <name>igneous</name>
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      <name>microcline</name>
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      <name>Minnesota</name>
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      <name>Minnesota River Valley</name>
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      <name>monazite</name>
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      <name>Morton Gneiss</name>
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