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    <title><![CDATA[1A Collections]]></title>
    <link>https://wserv3.esc.cam.ac.uk/p1acollections/items/browse?page=25&amp;sort_field=Dublin+Core%2CTitle&amp;output=rss2</link>
    <description><![CDATA[]]></description>
    <pubDate>Tue, 09 Apr 2024 21:25:50 +0100</pubDate>
    <managingEditor>p1acollections@esc.cam.ac.uk (1A Collections)</managingEditor>
    <generator>Zend_Feed</generator>
    <docs>http://blogs.law.harvard.edu/tech/rss</docs>
    <item>
      <title><![CDATA[Serpentine]]></title>
      <link>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/54</link>
      <description><![CDATA[<div class="element-set">
            <div id="dublin-core-title" class="element">
        <h3>Title</h3>
                    <div class="element-text"><h2>Serpentine</h2></div>
            </div><!-- end element -->
        <div id="dublin-core-subject" class="element">
        <h3>Subject</h3>
                    <div class="element-text"><span>Serpentine is a common alteration product of olivine, produced by hydration at low temperatures.</span></div>
            </div><!-- end element -->
        <div id="dublin-core-description" class="element">
        <h3>Description</h3>
                    <div class="element-text"><div class="element">
<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>
</div>
</div>
<div class="element">
<h3>Structure</h3>
<div class="element-text">
<p>Sheet silicate</p>
</div>
</div>
<div class="element">
<h3>Crystal System</h3>
<div class="element-text">
<p><em>Crystal system:</em><span> </span>monoclinic or orthorhombic (-)</p>
</div>
</div>
<div class="element">
<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>
</div>
</div>
<div class="element">
<h3>Rock Specimens</h3>
<div class="element-text">
<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>
</div>
</div>
<div class="element">
<h3>Mineral Name</h3>
<div class="element-text">serpentine</div>
</div></div>
            </div><!-- end element -->
    </div><!-- end element-set -->
<div class="item-file image-jpeg"><a class="download-file" href="https://wserv3.esc.cam.ac.uk/p1acollections/files/original/6667ec467cbdbb73c1ac797cbd273fd0.jpg"><img class="thumb" src="https://wserv3.esc.cam.ac.uk/p1acollections/files/square_thumbnails/6667ec467cbdbb73c1ac797cbd273fd0.jpg" alt="serpentine_CS.jpg" title="serpentine_CS.jpg"></a></div>]]></description>
      <pubDate>Mon, 17 Jun 2019 15:35:04 +0100</pubDate>
      <enclosure url="https://wserv3.esc.cam.ac.uk/p1acollections/files/fullsize/6667ec467cbdbb73c1ac797cbd273fd0.jpg" type="image/jpeg" length="134974"/>
    </item>
    <item>
      <title><![CDATA[Simple twinning]]></title>
      <link>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/252</link>
      <description><![CDATA[<div class="element-set">
            <div id="dublin-core-title" class="element">
        <h3>Title</h3>
                    <div class="element-text"><h2>Simple twinning</h2></div>
            </div><!-- end element -->
        <div id="dublin-core-subject" class="element">
        <h3>Subject</h3>
                    <div class="element-text">A single twin plane, producing two twins, within one mineral grain is called a simple twin. The clinopyroxene augite can display simple twinning. Simple twins are occasionally referred to as <a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/179">Carlsbad twins</a>.</div>
            </div><!-- end element -->
    </div><!-- end element-set -->
]]></description>
      <pubDate>Fri, 21 Jun 2019 17:33:02 +0100</pubDate>
    </item>
    <item>
      <title><![CDATA[Solid solution]]></title>
      <link>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/253</link>
      <description><![CDATA[<div class="element-set">
            <div id="dublin-core-title" class="element">
        <h3>Title</h3>
                    <div class="element-text"><h2>Solid solution</h2></div>
            </div><!-- end element -->
        <div id="dublin-core-subject" class="element">
        <h3>Subject</h3>
                    <div class="element-text">Minerals such as quartz have a discrete composition and thus one chemical formula (in this case SiO<sub>2</sub>). Other minerals can have a range of compositions between two or three end-member chemical formulae. Olivine, for example, has an end-member composition called forsterite (FeSiO<sub>4</sub>). By gradually replacing Fe atoms with Mg atoms, a continuous range of compositions can be produced ending at the Mg end-member, fayallite (MgSiO<sub>4</sub>). The range of compositions is called a solid solution.</div>
            </div><!-- end element -->
    </div><!-- end element-set -->
]]></description>
      <pubDate>Fri, 21 Jun 2019 17:35:36 +0100</pubDate>
    </item>
    <item>
      <title><![CDATA[Specific gravity, D]]></title>
      <link>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/254</link>
      <description><![CDATA[<div class="element-set">
            <div id="dublin-core-title" class="element">
        <h3>Title</h3>
                    <div class="element-text"><h2>Specific gravity, D</h2></div>
            </div><!-- end element -->
        <div id="dublin-core-subject" class="element">
        <h3>Subject</h3>
                    <div class="element-text">This is a measure of density. It is the ratio of the density of the substance being described (e.g. a mineral) to the density of water. Olivine has a specific density, D = 3.222, which means that olivine is 3.222 times more dense than water. Since water has a density of 1 g cm<sup>-3</sup>, olivine has a density of 3.22 g cm<sup>-3</sup>.</div>
            </div><!-- end element -->
    </div><!-- end element-set -->
]]></description>
      <pubDate>Fri, 21 Jun 2019 17:37:44 +0100</pubDate>
    </item>
    <item>
      <title><![CDATA[Sphene (titanite)]]></title>
      <link>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/44</link>
      <description><![CDATA[<div class="element-set">
            <div id="dublin-core-title" class="element">
        <h3>Title</h3>
                    <div class="element-text"><h2>Sphene<strong> (titanite)</strong></h2></div>
            </div><!-- end element -->
        <div id="dublin-core-description" class="element">
        <h3>Description</h3>
                    <div class="element-text"><div class="element">
<h3>Formula</h3>
<div class="element-text">CaTi[SiO<sub>4</sub>](O, OH, F)</div>
</div>
<div class="element">
<h3>Structure</h3>
<div class="element-text">
<p>Orthosilicate</p>
</div>
</div>
<div class="element">
<h3>Crystal System</h3>
<div class="element-text">
<p><em>Crystal system:</em><span> </span>monoclinic (+)</p>
</div>
</div>
<div class="element">
<h3>Physical Properties</h3>
<div class="element-text">
<p><em>Colour in hand specimen:</em><span> </span>colourless, yellow, green, brown or black<br /><em>Cleavage:</em><span> </span>one, good<br /><em>Hardness:</em><span> </span>5</p>
</div>
</div>
<div class="element">
<h3>Optical Properties</h3>
<div class="element-text">
<p><em>Colour in plane polarised light:</em><span> </span>colourless, yellow or typically brown<br /><em>Pleochroism:</em><span> </span>moderate if coloured<br /><em>Relief:</em><span> </span>high<br /><em>Birefringence:</em><span> </span>0.100-0.192; &gt;4th order<br /><em>Extinction:</em><span> </span>inclined<br /><em>Twinning:</em><span> </span>simple twins; occasionally lamellar twins</p>
</div>
</div>
<div class="element">
<h3>Rock Specimens</h3>
<div class="element-text">
<p><a href="/p1acollections/exhibits/show/igneous-rocks/l101">L101 Granite</a><span> </span><br /><a href="/p1acollections/exhibits/show/igneous-rocks/l120">L120 Granodiorite</a></p>
</div>
</div>
<div class="element">
<h3>Mineral Name</h3>
<div class="element-text">sphene<br />titanite<br /><h3>Advanced notes</h3>
<div class="element-text">Diamond shaped cross sections are common<br /><br /></div>
</div>
</div></div>
            </div><!-- end element -->
    </div><!-- end element-set -->
<div class="item-file image-jpeg"><a class="download-file" href="https://wserv3.esc.cam.ac.uk/p1acollections/files/original/8d7c5ffdcaf046d54625d611965a68ea.jpg"><img class="thumb" src="https://wserv3.esc.cam.ac.uk/p1acollections/files/square_thumbnails/8d7c5ffdcaf046d54625d611965a68ea.jpg" alt="Sphene_CS.jpg" title="Sphene_CS.jpg"></a></div>]]></description>
      <pubDate>Mon, 17 Jun 2019 13:02:48 +0100</pubDate>
      <enclosure url="https://wserv3.esc.cam.ac.uk/p1acollections/files/fullsize/8d7c5ffdcaf046d54625d611965a68ea.jpg" type="image/jpeg" length="122776"/>
    </item>
    <item>
      <title><![CDATA[Splendent [lustre]]]></title>
      <link>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/255</link>
      <description><![CDATA[<div class="element-set">
            <div id="dublin-core-title" class="element">
        <h3>Title</h3>
                    <div class="element-text"><h2>Splendent [lustre]</h2></div>
            </div><!-- end element -->
        <div id="dublin-core-description" class="element">
        <h3>Description</h3>
                    <div class="element-text"><em>See <strong><a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/224">metallic</a></strong>.</em></div>
            </div><!-- end element -->
    </div><!-- end element-set -->
]]></description>
      <pubDate>Fri, 21 Jun 2019 17:40:03 +0100</pubDate>
    </item>
    <item>
      <title><![CDATA[Subhedral]]></title>
      <link>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/256</link>
      <description><![CDATA[<div class="element-set">
            <div id="dublin-core-title" class="element">
        <h3>Title</h3>
                    <div class="element-text"><h2>Subhedral</h2></div>
            </div><!-- end element -->
        <div id="dublin-core-subject" class="element">
        <h3>Subject</h3>
                    <div class="element-text">A crystal displaying some, but not all of its characteristic crystal faces is called subhedral.</div>
            </div><!-- end element -->
    </div><!-- end element-set -->
]]></description>
      <pubDate>Fri, 21 Jun 2019 17:40:29 +0100</pubDate>
    </item>
    <item>
      <title><![CDATA[Sutured contacts]]></title>
      <link>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/257</link>
      <description><![CDATA[<div class="element-set">
            <div id="dublin-core-title" class="element">
        <h3>Title</h3>
                    <div class="element-text"><h2>Sutured contacts</h2></div>
            </div><!-- end element -->
        <div id="dublin-core-subject" class="element">
        <h3>Subject</h3>
                    <div class="element-text">Usually refers to quartz grains, which have undergone partial recrystallisation, producing irregular, sutured grain boundaries.</div>
            </div><!-- end element -->
        <div id="dublin-core-description" class="element">
        <h3>Description</h3>
                    <div class="element-text"><em>Have a look at the <strong>quartzites (<a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/39">L520</a>, <a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/40">L521</a>)</strong> in the 1A Reference Series.</em></div>
            </div><!-- end element -->
    </div><!-- end element-set -->
]]></description>
      <pubDate>Fri, 21 Jun 2019 17:45:41 +0100</pubDate>
    </item>
    <item>
      <title><![CDATA[Tabular]]></title>
      <link>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/258</link>
      <description><![CDATA[<div class="element-set">
            <div id="dublin-core-title" class="element">
        <h3>Title</h3>
                    <div class="element-text"><h2>Tabular</h2></div>
            </div><!-- end element -->
        <div id="dublin-core-subject" class="element">
        <h3>Subject</h3>
                    <div class="element-text">Flat, planar, non-elongate crystals are described as having a tabular habit. Tabular crystals are thicker than platy crystals.</div>
            </div><!-- end element -->
    </div><!-- end element-set -->
]]></description>
      <pubDate>Fri, 21 Jun 2019 17:47:30 +0100</pubDate>
    </item>
    <item>
      <title><![CDATA[Tartan twinning]]></title>
      <link>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/259</link>
      <description><![CDATA[<div class="element-set">
            <div id="dublin-core-title" class="element">
        <h3>Title</h3>
                    <div class="element-text"><h2>Tartan twinning</h2></div>
            </div><!-- end element -->
        <div id="dublin-core-description" class="element">
        <h3>Description</h3>
                    <div class="element-text"><em>See<span> </span><a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/183">cross-hatched twinning</a>.</em></div>
            </div><!-- end element -->
    </div><!-- end element-set -->
]]></description>
      <pubDate>Fri, 21 Jun 2019 17:48:24 +0100</pubDate>
    </item>
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