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      <src>https://bereket-haileab.geology.sites.carleton.edu/files/original/e84de6fdb51bb116a1bec759fe50e30d.jpg</src>
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            <name>Title</name>
            <description>A name given to the resource</description>
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                <text>Metamorphic Rocks</text>
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          <element elementId="49">
            <name>Subject</name>
            <description>The topic of the resource</description>
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              <elementText elementTextId="3237">
                <text>This collection includes slates, phyllites, schists, gneisses, eclogites, marbles, quartzites, skarns, granulites, and mylonites.</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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            <name>Format</name>
            <description>The file format, physical medium, or dimensions of the resource</description>
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              <elementText elementTextId="3256">
                <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>BH250-177</text>
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          <name>Subject</name>
          <description>The topic of the resource</description>
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              <text>Black Vishnu Schist</text>
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          <name>Description</name>
          <description>An account of the resource</description>
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              <text>Major Minerals: hornblende, quartz&#13;
&#13;
 The Vishnu Schist is one of the oldest rock units in the Grand Canyon, forming part of the Vishnu Basement Rocks exposed in the Inner Gorge. The term "Black Vishnu Schist" refers specifically to the darker, more mafic-rich variants of the Vishnu Schist. These rocks are Paleoproterozoic in age (~1.75 billion years) and are derived from metamorphism of volcanic protoliths as can be seen from the mineral assemblage. Metamorphism reached the amphibolite facies, producing a rock that is strongly foliated and lineated, with well-developed schistosity.&#13;
&#13;
The Black Vishnu Schist is in direct contact with the overlying Paleozoic sedimentary rocks (Tapeats Sandstone) across the famous Great Unconformity, providing a striking example of this profound geologic boundary in North America. I have taken several photos of this nonconformity, which are available on this website.&#13;
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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: Lower Section, Grand Canyon, Arizona, USA&#13;
Nearby Geographic Feature: Grand Canyon</text>
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          <name>Date</name>
          <description>A point or period of time associated with an event in the lifecycle of the resource</description>
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              <text>August 2015</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 BH250-177. 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=d078b4a34e154008986da45784b784d4" 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=d078b4a34e154008986da45784b784d4"&gt;here&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;iframe width="100%" height="480" src="https://drive.google.com/file/d/1C3aLBDHbPP3YlfwA65as4faP5dl00RYO/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/1I5hFchXiRPTjkLhEUVdBUeb7s3HxenkF/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/1afVJb4dOITyPmhL7wdrnZ337v3m6ZrbF/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/1WRZE5GBxs4WDLbemhj2IJLlcz-hdQv4r/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/1bFPt09K2kzSyBmoVEBH8rt_rS2RbXrIr/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/1OS_URfW7RLY0l-zAeGB9tU8hCXII0lyO/preview" allow="autoplay"&gt;&lt;/iframe&gt; &lt;iframe width="100%" height="480" src="https://drive.google.com/file/d/1EkuGC53BI_3rQg3K-Zzh4avKf2NH8yIv/preview" allow="autoplay"&gt;&lt;/iframe&gt; &lt;iframe width="100%" height="480" src="https://drive.google.com/file/d/1UiTzzvx4a8HIdmjbX0rS59E11qZGoZrZ/preview" allow="autoplay"&gt;&lt;/iframe&gt; &lt;iframe width="100%" height="480" src="https://drive.google.com/file/d/1RTZt8ZnRQxugdysmRIZ9FWigvaO3wrVA/preview" allow="autoplay"&gt;&lt;/iframe&gt; &lt;iframe width="100%" height="480" src="https://drive.google.com/file/d/18tFXsoHS2eM_SC7RX4gbjKrxDcziRGw8/preview" allow="autoplay"&gt;&lt;/iframe&gt; &lt;iframe width="100%" height="480" src="https://drive.google.com/file/d/1xEFT-cf85Bh2RW_7hm54kNb13DBmtG-C/preview" allow="autoplay"&gt;&lt;/iframe&gt; &lt;iframe width="100%" height="480" src="https://drive.google.com/file/d/1Swbh35NqMThtf6u654zIL1E242Y2rFBa/preview" allow="autoplay"&gt;&lt;/iframe&gt; &lt;iframe width="100%" height="480" src="https://drive.google.com/file/d/1aB3oxoscLqLUZRI9GVMTjRYPMpQW824p/preview" allow="autoplay"&gt;&lt;/iframe&gt; &lt;iframe width="100%" height="480" src="https://drive.google.com/file/d/179Ts4dPPn3IqaLCQIwcDe_NRbtlSLPtQ/preview" allow="autoplay"&gt;&lt;/iframe&gt;</text>
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              <text>Bereket Haileab</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</text>
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      <name>Amphibolite Facies</name>
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      <name>Black Vishnu Schist</name>
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    <tag tagId="612">
      <name>Foliation</name>
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    <tag tagId="982">
      <name>Great Unconformity</name>
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    <tag tagId="536">
      <name>Hornblende</name>
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    <tag tagId="981">
      <name>Hornblende Quartz Schist</name>
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    <tag tagId="980">
      <name>Mafic Metamorphism</name>
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    <tag tagId="1">
      <name>metamorphic</name>
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      <name>nonconformity</name>
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      <name>schist</name>
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      <name>Schistosity</name>
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      <name>Tapeats Sandstone</name>
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      <name>Vishnu Schist</name>
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      <name>Volcanic Protoliths</name>
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