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    <pubDate>Tue, 09 Apr 2024 21:16:22 +0100</pubDate>
    <managingEditor>p1acollections@esc.cam.ac.uk (1A Collections)</managingEditor>
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      <title><![CDATA[Serpentine]]></title>
      <link>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/54</link>
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        <h3>Title</h3>
                    <div class="element-text"><h2>Serpentine</h2></div>
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        <h3>Subject</h3>
                    <div class="element-text"><span>Serpentine is a common alteration product of olivine, produced by hydration at low temperatures.</span></div>
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        <h3>Description</h3>
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<h3>Formula</h3>
<div class="element-text">
<p>Mg<sub>3</sub>[Si<sub>2</sub>O<sub>5</sub>](OH)<sub>4</sub></p>
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<h3>Structure</h3>
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<p>Sheet silicate</p>
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<h3>Crystal System</h3>
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<p><em>Crystal system:</em><span> </span>monoclinic or orthorhombic (-)</p>
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<h3>Optical Properties</h3>
<div class="element-text">
<p class="NoSpacing"><span>Serpentine is commonly very fine-grained. It can be recognised by its textural association with olivine and by its low birefringence and habit.</span></p>
<p class="NoSpacing"><em><span>Colour in plane polarised light:</span></em><span> green</span><span> </span><br class="NoSpacing" /><em><span>Relief:</span></em><span> low</span><span> </span><br class="NoSpacing" /><em><span>Birefringence:</span></em><span> 1<sup>st</sup> order</span></p>
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<h3>Rock Specimens</h3>
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<p><a href="/p1acollections/exhibits/show/igneous-rocks/l141">L141 Gabbro</a><span> </span><br /><a href="/p1acollections/exhibits/show/igneous-rocks/l162">L162 Basalt, porphyritic</a><span> </span><br /><a href="/p1acollections/exhibits/show/igneous-rocks/l172">L172 Ultramafic cumulate</a></p>
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<h3>Mineral Name</h3>
<div class="element-text">serpentine</div>
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      <pubDate>Mon, 17 Jun 2019 15:35:04 +0100</pubDate>
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