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<item xmlns="http://omeka.org/schemas/omeka-xml/v5" itemId="362" public="1" featured="0" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://omeka.org/schemas/omeka-xml/v5 http://omeka.org/schemas/omeka-xml/v5/omeka-xml-5-0.xsd" uri="https://bereket-haileab.geology.sites.carleton.edu/items/show/362?output=omeka-xml" accessDate="2026-10-22T16:52:38+00:00">
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      <src>https://bereket-haileab.geology.sites.carleton.edu/files/original/cac9c6bd0644e3c54ef57cc1612761bd.jpg</src>
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        <description>The Dublin Core metadata element set is common to all Omeka records, including items, files, and collections. For more information see, http://dublincore.org/documents/dces/.</description>
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          <element elementId="50">
            <name>Title</name>
            <description>A name given to the resource</description>
            <elementTextContainer>
              <elementText elementTextId="3236">
                <text>Metamorphic Rocks</text>
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          <element elementId="49">
            <name>Subject</name>
            <description>The topic of the resource</description>
            <elementTextContainer>
              <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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          <element elementId="42">
            <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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      <description>The Dublin Core metadata element set is common to all Omeka records, including items, files, and collections. For more information see, http://dublincore.org/documents/dces/.</description>
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        <element elementId="50">
          <name>Title</name>
          <description>A name given to the resource</description>
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              <text>BH250-242b</text>
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        <element elementId="49">
          <name>Subject</name>
          <description>The topic of the resource</description>
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              <text>Marble</text>
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        <element elementId="38">
          <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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            <elementText elementTextId="3776">
              <text>Death Valley, California, USA&#13;
Mosaic Canyon California&#13;
GPS coordinates:  36°34'7.45"N, 117° 8'28.24"W</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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            <elementText elementTextId="3778">
              <text>From the rock collection of Bereket Haileab. Sample 242b. Housed at Carleton College in Minnesota.</text>
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        <element elementId="51">
          <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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        <element elementId="46">
          <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/1D5uKi9-NNr0bYsJ2Aa6BOuhZJLXeAV5L/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/1dMaYimLZdUUGlJfFV3JuUlcAzgqTV9MR/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/1jqewSmp1mcIVXwyFrUV-XGrIrog-HOtw/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/1E-1H31S4dZWjUF3jf-x-TSDdoIvlmU0j/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/1jENs2jAyvYXVTaOh5oX1QuFc96v4ILC-/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/1vvLz77wp4F05H2SThKDCkLpmDTbp26mG/preview" allow="autoplay"&gt;&lt;/iframe&gt;&lt;iframe width="100%" height="480" src="https://drive.google.com/file/d/1EygQ-QRjkPgFtujLb4Ga7VNUWe6yW-Z1/preview" allow="autoplay"&gt;&lt;/iframe&gt;&lt;iframe width="100%" height="480" src="https://drive.google.com/file/d/17Z7GSGNy6t5nxe0NMvVU4MNIbCFMdgBQ/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 marble from Mosaic Canyon in Death Valley comes from a classic carbonate sequence exposed along the western part of the valley, composed mainly of Paleozoic limestone and dolostone deposited in shallow marine environments along the passive margin of western North America. In Mosaic Canyon, much of this marble is derived from units such as the Noonday Dolomite and overlying limestones, later metamorphosed under low- to moderate-grade conditions to produce a recrystallized, interlocking calcite texture. The rock commonly preserves subtle banding, stylolites, and pressure-solution features, and locally records minor deformation. The canyon’s distinctive smooth, polished, and fluted walls are the result of sediment-laden flash floods that have sculpted the marble surfaces. Overall, the marble records a history of marine deposition, metamorphism, and tectonic exhumation, followed by ongoing surface erosion (Mike Smith, Class of 1999, personal communication).</text>
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      <name>Basin and Range Province</name>
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    <tag tagId="1651">
      <name>Carbonate rock</name>
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    <tag tagId="1809">
      <name>Death Valley</name>
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    <tag tagId="779">
      <name>Dolostone protolith</name>
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    <tag tagId="1808">
      <name>limestone protolith</name>
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    <tag tagId="32">
      <name>marble</name>
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    <tag tagId="1">
      <name>metamorphic</name>
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    <tag tagId="549">
      <name>metamorphic rock</name>
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    <tag tagId="1811">
      <name>Mosaic Canyon</name>
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    <tag tagId="997">
      <name>Noonday Dolomite</name>
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    <tag tagId="1807">
      <name>recrystallized calcite</name>
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    <tag tagId="1810">
      <name>stylolites</name>
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