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            <name>Title</name>
            <description>A name given to the resource</description>
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                <text>Sedimentary Rocks</text>
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            <name>Subject</name>
            <description>The topic of the resource</description>
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              <elementText elementTextId="3240">
                <text>This collection includes sandstones, limestones, breccias, conglomerates, dolostones, shales, oolites, and BIF.</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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            <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="3254">
                <text>Thin sections, thin section scans, hand samples, hand sample images, photomicrographs.</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>BH250-175e</text>
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          <description>The topic of the resource</description>
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              <text>Bass Limestone</text>
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          <description>An account of the resource</description>
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              <text>Major Mineral: calcite&#13;
Minor Mineral: chert&#13;
&#13;
In thin section, the Bass Limestone contains low-birefringence, low-relief minerals identified as chert (microcrystalline quartz), which formed through diagenetic recrystallization. As the oldest sedimentary unit in the Grand Canyon, the Bass Limestone has experienced low-grade metamorphism, leading to the recrystallization of both calcite and chert.&#13;
&#13;
The calcite grain size in the Bass Limestone is substantially larger than that of younger limestones in the region, such as the Muav Limestone, reflecting the prolonged effects of metamorphism and diagenesis. This contrasts with younger and less-altered limestones like samples BH250-122, 125, 128, 140, 175f, 122wc, and 128c, which retain finer-grained textures.&#13;
&#13;
You will find many calcite grains in Bass Limestone thin sections are cut perpendicular to sub-perpendicular to the c-axis, producing optic axis figures or off-centered uniaxial negative interference figures when viewed under crossed polars.&#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: Mile 132 Stone Creek, 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 2021</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 BH250-175e. 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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          <description>An entity primarily responsible for making the resource</description>
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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>Bass Limestone</name>
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      <name>Chert</name>
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      <name>diagenetic recystallization</name>
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    <tag tagId="962">
      <name>Grand Canyon Supergroup</name>
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    <tag tagId="49">
      <name>limestone</name>
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      <name>microcrystalline quartz</name>
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