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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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            <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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                <text>Bereket Haileab</text>
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            <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>BH250-100d</text>
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          <name>Subject</name>
          <description>The topic of the resource</description>
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              <text>Morton Gneiss Saprolite</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>From the rock collection of Bereket Haileab. Sample 100d. 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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          <name>Relation</name>
          <description>A related resource</description>
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              <text>&lt;iframe width="100%" height="480" src="https://drive.google.com/file/d/1ZUxIutARyFAutj7cLfjUADwYjZaJAL1r/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/1IYc9HMlN-M20cAl7T_nB8-5JwByv5w1f/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/1Ox7z5csyTdSPbYh-dTLiww7-lYF1gjfc/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/1fEzKQ0uju82UkN65RL4p6Rsc4C8VVFcE/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/1fJQOkrmVOFABWVQXad-IMgHJ7t9wNJVh/preview" allow="autoplay"&gt;&lt;/iframe&gt;</text>
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          <name>Description</name>
          <description>An account of the resource</description>
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              <text>The Morton Saprolite near Redwood Falls, Minnesota, formed through deep chemical weathering of the Precambrian Morton Gneiss, one of the oldest rock units on Earth. As the gneiss weathers, it produces a distinctive mineral assemblage including quartz, kaolinite, sericite (white mica), gibbsite, goethite, and hematite. Despite extensive mineralogical alteration, the saprolite preserves the original fabric and banding of the gneiss — a hallmark feature of saprolitic weathering. The weathered material is typically reddish to yellowish-brown, reflecting the abundance of iron oxides.&#13;
&#13;
This saprolite has been the subject of multiple geochemistry student research projects, particularly focusing on its mineralogy, weathering processes, and geochemical evolution. Documentation and findings from these student studies are available through resources linked on this website.&#13;
&#13;
This rock/saprolite is the least weathered Morton Geniss.&#13;
&#13;
Several student projects have explored this subject; please refer to the papers, abstracts, and posters available on the Geochemistry of Natural Waters website.&#13;
&#13;
For more discussion on the Morton Saprolite see BH250-100&#13;
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      <name>Clay Mineral</name>
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      <name>Clay Mineral Formation</name>
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      <name>Deep Chemical Weathering</name>
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      <name>Element Mobility</name>
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      <name>Feldspar weathering</name>
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      <name>Goethite</name>
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      <name>Hydrolysis</name>
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      <name>Immobile Element Concentration</name>
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      <name>Kaolinite</name>
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    <tag tagId="1470">
      <name>Leaching</name>
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      <name>metamorphic</name>
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    <tag tagId="577">
      <name>Minnesota</name>
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    <tag tagId="1465">
      <name>Minnesota River Valley</name>
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    <tag tagId="898">
      <name>Morton Gneiss</name>
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    <tag tagId="906">
      <name>Paleosaprolite</name>
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    <tag tagId="1472">
      <name>Potassium Loss</name>
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    <tag tagId="899">
      <name>Precambrian</name>
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    <tag tagId="1474">
      <name>Rare Earth Element (REE) Enrichment</name>
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      <name>Redwood Falls</name>
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      <name>Redwood Falls Minnesota</name>
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    <tag tagId="1467">
      <name>Regolith</name>
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    <tag tagId="1468">
      <name>Residual Soil</name>
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      <name>saprolite</name>
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    <tag tagId="908">
      <name>Saprolitic Weathering</name>
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    <tag tagId="903">
      <name>Sericite</name>
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    <tag tagId="1479">
      <name>Sericite Separation</name>
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    <tag tagId="1471">
      <name>Silica Depletion</name>
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    <tag tagId="1464">
      <name>Southwestern Minnesota</name>
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    <tag tagId="1466">
      <name>Weathered Gneiss</name>
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    <tag tagId="1478">
      <name>White mica</name>
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