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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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                <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>
            <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>
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                <text>Housed in Anderson Hall, Carleton College.</text>
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            <name>Format</name>
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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>Title</name>
          <description>A name given to the resource</description>
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              <text>BH250-250</text>
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          <description>The topic of the resource</description>
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              <text>Basalt</text>
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              <text>East Pacific Rise, recovered by HOV Alvin at 2500 m depth</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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          <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 250. Housed at Carleton College in Minnesota.</text>
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          <name>Publisher</name>
          <description>An entity responsible for making the resource available</description>
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              <text>Bereket Haileab</text>
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              <text>Mid-oceanic ridge basalt (MORB) from East Pacific Rise, showing glassy, basalt and a chilled margin.&#13;
&#13;
Petrologic and Mantle Significance:&#13;
This mid-ocean ridge basalt (MORB) from the East Pacific Rise represents the dominant volcanic rock type forming the oceanic crust at divergent plate boundaries. It originated from partial melting of the upper mantle at depths of ~60–80 km. The presence of glass and a chilled margin reflects rapid quenching during submarine eruption, preserving the melt composition with minimal alteration.&#13;
&#13;
Geochemically, MORB is typically depleted in incompatible elements and exhibits relatively uniform isotopic ratios (e.g., low ⁸⁷Sr/⁸⁶Sr and high ¹⁴³Nd/¹⁴⁴Nd), indicating a well-mixed, depleted mantle source that has experienced prior melt extraction. Once analyzed for its chemistry and thin sections are made, this sample will serve as a valuable geochemical reference for understanding mantle composition, magma generation processes, and global mantle heterogeneity.&#13;
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              <text>Bereket Haileab, Carleton College Geology Department&#13;
Adam Soule '97</text>
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          <description>A related resource</description>
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              <text>&lt;iframe width="100%" height="480" src="https://drive.google.com/file/d/1HfKRYZDJ-neJAuKyLPHDDN0my1OQnPdx/preview" allow="autoplay"&gt;&lt;/iframe&gt;&lt;iframe width="100%" height="480" src="https://drive.google.com/file/d/19f70K0nJ0U2007yA4DfRg2u0qNOaYoXz/preview" allow="autoplay"&gt;&lt;/iframe&gt;&lt;iframe width="100%" height="480" src="https://drive.google.com/file/d/1JqDsPYom35vJgcxBmxyG8vERFSOorom-/preview" allow="autoplay"&gt;&lt;/iframe&gt;&lt;iframe width="100%" height="480" src="https://drive.google.com/file/d/1BfXwdQ7qlhX4-D149unPCLQ6OGps9Lwl/preview" allow="autoplay"&gt;&lt;/iframe&gt;&lt;iframe width="100%" height="480" src="https://drive.google.com/file/d/175deXA_R80TbsZht3wPxO6tZWq19o7xb/preview" allow="autoplay"&gt;&lt;/iframe&gt;</text>
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      <name>basalt</name>
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      <name>Mid-Oceanic Ridge Basalt</name>
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