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  <title><![CDATA[1A Collections]]></title>
  <subtitle><![CDATA[Rocks, minerals and fossils collections for Part 1A students]]></subtitle>
  <author>
    <name><![CDATA[Department of Earth Sciences]]></name>
  </author>
  <updated>2024-04-09T21:24:29+01:00</updated>
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  <entry>
    <id>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/198</id>
    <title><![CDATA[<h2>Foliation</h2>]]></title>
    <updated>2019-07-04T09:53:06+01:00</updated>
    <link rel="alternate" type="text/html" href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/198"/>
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        <h3>Title</h3>
                    <div class="element-text"><h2>Foliation</h2></div>
            </div><!-- end element -->
        <div id="dublin-core-subject" class="element">
        <h3>Subject</h3>
                    <div class="element-text"><span>This refers to any pervasive planar feature in a rock. It is produced by the arrangement of the constituent grains into sheet-like structures, usually in compositionally distinct layers. Foliations can be primary (e.g. bedding, fissility, flow banding) or secondary (e.g. cleavage).</span></div>
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  </entry>
  <entry>
    <id>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/199</id>
    <title><![CDATA[<h2>Form</h2>]]></title>
    <summary><![CDATA[<em>See<span> </span><a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/206">habit</a>.</em>]]></summary>
    <updated>2019-07-04T09:53:07+01:00</updated>
    <link rel="alternate" type="text/html" href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/199"/>
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            <div id="dublin-core-title" class="element">
        <h3>Title</h3>
                    <div class="element-text"><h2>Form</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/206">habit</a>.</em></div>
            </div><!-- end element -->
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  </entry>
  <entry>
    <id>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/61</id>
    <title><![CDATA[<h2>Galena</h2>]]></title>
    <summary><![CDATA[<div class="element">
<h3>Formula</h3>
<div class="element-text">
<p>PbS</p>
</div>
</div>
<div class="element">
<h3>Structure</h3>
<div class="element-text">
<p>Non-silicate</p>
</div>
</div>
<div class="element">
<h3>Crystal System</h3>
<div class="element-text">
<p><em>Crystal system:</em><span> </span>cubic</p>
</div>
</div>
<div class="element">
<h3>Physical Properties</h3>
<div class="element-text">
<p><em>Colour in hand specimen:</em><span> </span>lead grey<br /><em>Streak:</em><span> </span>lead grey<br /><em>Lustre:</em><span> </span>metallic<br /><em>Cleavage:</em><span> </span>one, perfect<br /><em>Hardness:</em><span> </span>2.5</p>
</div>
</div>
<div class="element">
<h3>Optical Properties</h3>
<div class="element-text">
<p><em>Colour in plane polarised light:</em><span> </span>opaque<br /><em>Relief:</em><span> </span>high</p>
</div>
</div>
<div class="element">
<h3>Mineral Specimens</h3>
<div class="element-text">
<p class="NoSpacing"><strong><span>M412 </span></strong><strong><span>Quartz (with galena and pyrite)</span><span> </span></strong><br class="NoSpacing" /><strong>North Wales</strong><strong></strong><span> </span><br class="NoSpacing" />A mass of small hexagonal quartz prisms, with galena, pyrite and zinc blende.<span> </span><br class="NoSpacing" />Transparent, white to light grey<span> </span><br class="NoSpacing" />Galena: purple-black, shiny, platy habit, metallic<span> </span><br />Pyrite: metallic lustre, gold colour, cubic habit, “Fools’ gold”</p>
</div>
</div>
<div class="element">
<h3>Mineral Name</h3>
<div class="element-text">galena</div>
</div>]]></summary>
    <updated>2019-07-04T09:52:21+01:00</updated>
    <link rel="alternate" type="text/html" href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/61"/>
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    <category term="dense"/>
    <category term="grey"/>
    <category term="streak"/>
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            <div id="dublin-core-title" class="element">
        <h3>Title</h3>
                    <div class="element-text"><h2>Galena</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">
<p>PbS</p>
</div>
</div>
<div class="element">
<h3>Structure</h3>
<div class="element-text">
<p>Non-silicate</p>
</div>
</div>
<div class="element">
<h3>Crystal System</h3>
<div class="element-text">
<p><em>Crystal system:</em><span> </span>cubic</p>
</div>
</div>
<div class="element">
<h3>Physical Properties</h3>
<div class="element-text">
<p><em>Colour in hand specimen:</em><span> </span>lead grey<br /><em>Streak:</em><span> </span>lead grey<br /><em>Lustre:</em><span> </span>metallic<br /><em>Cleavage:</em><span> </span>one, perfect<br /><em>Hardness:</em><span> </span>2.5</p>
</div>
</div>
<div class="element">
<h3>Optical Properties</h3>
<div class="element-text">
<p><em>Colour in plane polarised light:</em><span> </span>opaque<br /><em>Relief:</em><span> </span>high</p>
</div>
</div>
<div class="element">
<h3>Mineral Specimens</h3>
<div class="element-text">
<p class="NoSpacing"><strong><span>M412 </span></strong><strong><span>Quartz (with galena and pyrite)</span><span> </span></strong><br class="NoSpacing" /><strong>North Wales</strong><strong></strong><span> </span><br class="NoSpacing" />A mass of small hexagonal quartz prisms, with galena, pyrite and zinc blende.<span> </span><br class="NoSpacing" />Transparent, white to light grey<span> </span><br class="NoSpacing" />Galena: purple-black, shiny, platy habit, metallic<span> </span><br />Pyrite: metallic lustre, gold colour, cubic habit, “Fools’ gold”</p>
</div>
</div>
<div class="element">
<h3>Mineral Name</h3>
<div class="element-text">galena</div>
</div></div>
            </div><!-- end element -->
    </div><!-- end element-set -->
]]></content>
  </entry>
  <entry>
    <id>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/45</id>
    <title><![CDATA[<h2>Garnet</h2>]]></title>
    <summary><![CDATA[<div class="element">
<h3>Formula</h3>
<div class="element-text">(Mg,Fe,Ca)<sub>3</sub>Al<sub>2</sub>Si<sub>3</sub>O<sub>12</sub></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>cubic</p>
</div>
</div>
<div class="element">
<h3>Physical Properties</h3>
<div class="element-text">
<p><em>Colour in hand specimen:</em><span> </span>typically red<br /><em>Cleavage:</em><span> </span>none<br /><em>Hardness:</em><span> </span>6-7.5</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, pale pink<span> </span><br /><em>Pleochroism:</em><span> </span>none<br /><em>Relief:</em><span> </span>high<br />Isotropic</p>
</div>
</div>
<div class="element">
<h3>Mineral Specimens</h3>
<div class="element-text">
<p><span><strong>M130 Garnet schist</strong></span><br /><strong>Portsoy, Banffshire</strong><br />Euhedral porphyroblasts of dark-red garnet, with quartz, mica and other minerals in a medium-grade metamorphic rock.</p>
</div>
</div>
<div class="element">
<h3>Rock Specimens</h3>
<div class="element-text">
<p><a href="/p1acollections/exhibits/show/metamorphic-rocks/l504">L504 Garnet schist</a></p>
</div>
</div>
<div class="element">
<h3>Advanced Notes</h3>
<div class="element-text">
<p>The garnet group encompasses a wide range of compositions, and consequently a range of optical and physical properties. The properties detailed above are typical of pyrope (Mg<sub>3</sub>Al<sub>2</sub>Si<sub>3</sub>O<sub>12</sub>), almandine (Fe<sup>2+</sup><sub>3</sub>Al<sub>2</sub>Si<sub>3</sub>O<sub>12</sub>) and grossular (Ca<sub>3</sub>Al<sub>2</sub>Si<sub>3</sub>O<sub>12</sub>).</p>
</div>
</div>
<div class="element">
<h3>Mineral Name</h3>
<div class="element-text">garnet</div>
</div>]]></summary>
    <updated>2019-07-04T09:52:16+01:00</updated>
    <link rel="alternate" type="text/html" href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/45"/>
    <link rel="enclosure" href="https://wserv3.esc.cam.ac.uk/p1acollections/files/original/74710dbf85be2a6e9e238ba537ef6ad4.jpg" type="image/jpeg" length="2391444"/>
    <category term="metamorphism"/>
    <category term="metapelite"/>
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            <div id="dublin-core-title" class="element">
        <h3>Title</h3>
                    <div class="element-text"><h2>Garnet</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">(Mg,Fe,Ca)<sub>3</sub>Al<sub>2</sub>Si<sub>3</sub>O<sub>12</sub></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>cubic</p>
</div>
</div>
<div class="element">
<h3>Physical Properties</h3>
<div class="element-text">
<p><em>Colour in hand specimen:</em><span> </span>typically red<br /><em>Cleavage:</em><span> </span>none<br /><em>Hardness:</em><span> </span>6-7.5</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, pale pink<span> </span><br /><em>Pleochroism:</em><span> </span>none<br /><em>Relief:</em><span> </span>high<br />Isotropic</p>
</div>
</div>
<div class="element">
<h3>Mineral Specimens</h3>
<div class="element-text">
<p><span><strong>M130 Garnet schist</strong></span><br /><strong>Portsoy, Banffshire</strong><br />Euhedral porphyroblasts of dark-red garnet, with quartz, mica and other minerals in a medium-grade metamorphic rock.</p>
</div>
</div>
<div class="element">
<h3>Rock Specimens</h3>
<div class="element-text">
<p><a href="/p1acollections/exhibits/show/metamorphic-rocks/l504">L504 Garnet schist</a></p>
</div>
</div>
<div class="element">
<h3>Advanced Notes</h3>
<div class="element-text">
<p>The garnet group encompasses a wide range of compositions, and consequently a range of optical and physical properties. The properties detailed above are typical of pyrope (Mg<sub>3</sub>Al<sub>2</sub>Si<sub>3</sub>O<sub>12</sub>), almandine (Fe<sup>2+</sup><sub>3</sub>Al<sub>2</sub>Si<sub>3</sub>O<sub>12</sub>) and grossular (Ca<sub>3</sub>Al<sub>2</sub>Si<sub>3</sub>O<sub>12</sub>).</p>
</div>
</div>
<div class="element">
<h3>Mineral Name</h3>
<div class="element-text">garnet</div>
</div></div>
            </div><!-- end element -->
    </div><!-- end element-set -->
]]></content>
  </entry>
  <entry>
    <id>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/116</id>
    <title><![CDATA[<h2>Gastropod</h2>]]></title>
    <summary><![CDATA[<h2>Taxonomy</h2>
<p>Phylum: Mollusca</p>
<p>Class: Gastropoda</p>
<h2>Diagnostic Features</h2>
<p>Coiled shell - planispiral or helical - consists of body whorl and spire</p>
<p>Mostly aragonitic shell</p>
<p>Shell consists of one large chamber (no septa)</p>
<p>Aperture</p>
<p>Siphonal notch</p>
<h2>Way of life</h2>
<p>Marine, non-marine, land-dwelling</p>
<p>Carnivorous, scavenging, deposit feeding and more</p>
<h2>Advanced notes</h2>
<p>Because of their conservative shell shape it is difficult to use gastropods as environmental or stratigraphic indicators.</p>
<h2>Specimens</h2>
<p><a href="/p1acollections/exhibits/show/gastropods" target="_blank" rel="noreferrer noopener">Browse gastropods</a></p>
<h2>External links</h2>
<p><a href="https://www.youtube.com/watch?v=2ilSDcZAXNM" target="_blank" rel="noreferrer noopener">Telling planispiral fossils apart</a></p>]]></summary>
    <updated>2019-07-04T09:52:41+01:00</updated>
    <link rel="alternate" type="text/html" href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/116"/>
    <link rel="enclosure" href="https://wserv3.esc.cam.ac.uk/p1acollections/files/original/c6b9427325c8a625a1fb715e2ba9b761.png" type="image/png" length="104741"/>
    <link rel="enclosure" href="https://wserv3.esc.cam.ac.uk/p1acollections/files/original/852990c0fa5efed6ff5d4c9668161751.png" type="image/png" length="105196"/>
    <category term="coil"/>
    <content type="html"><![CDATA[<div class="element-set">
            <div id="dublin-core-title" class="element">
        <h3>Title</h3>
                    <div class="element-text"><h2>Gastropod</h2></div>
            </div><!-- end element -->
        <div id="dublin-core-description" class="element">
        <h3>Description</h3>
                    <div class="element-text"><h2>Taxonomy</h2>
<p>Phylum: Mollusca</p>
<p>Class: Gastropoda</p>
<h2>Diagnostic Features</h2>
<p>Coiled shell - planispiral or helical - consists of body whorl and spire</p>
<p>Mostly aragonitic shell</p>
<p>Shell consists of one large chamber (no septa)</p>
<p>Aperture</p>
<p>Siphonal notch</p>
<h2>Way of life</h2>
<p>Marine, non-marine, land-dwelling</p>
<p>Carnivorous, scavenging, deposit feeding and more</p>
<h2>Advanced notes</h2>
<p>Because of their conservative shell shape it is difficult to use gastropods as environmental or stratigraphic indicators.</p>
<h2>Specimens</h2>
<p><a href="/p1acollections/exhibits/show/gastropods" target="_blank" rel="noreferrer noopener">Browse gastropods</a></p>
<h2>External links</h2>
<p><a href="https://www.youtube.com/watch?v=2ilSDcZAXNM" target="_blank" rel="noreferrer noopener">Telling planispiral fossils apart</a></p></div>
            </div><!-- end element -->
    </div><!-- end element-set -->
]]></content>
  </entry>
  <entry>
    <id>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/200</id>
    <title><![CDATA[<h2>Glass</h2>]]></title>
    <summary><![CDATA[<em>Have a look at the<strong> rhyolite glass (<a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/7">L113</a>)</strong><span> </span>in the 1A Reference Series.</em>]]></summary>
    <updated>2019-07-04T09:53:07+01:00</updated>
    <link rel="alternate" type="text/html" href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/200"/>
    <content type="html"><![CDATA[<div class="element-set">
            <div id="dublin-core-title" class="element">
        <h3>Title</h3>
                    <div class="element-text"><h2>Glass</h2></div>
            </div><!-- end element -->
        <div id="dublin-core-subject" class="element">
        <h3>Subject</h3>
                    <div class="element-text"><span>When magma is quenched (cooled exceedingly rapidly) even very small crystals are unable to grow. Instead, a volcanic glass is formed. It is amorphous (having no crystalline structure), and is consequently isotropic.</span></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> rhyolite glass (<a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/7">L113</a>)</strong><span> </span>in the 1A Reference Series.</em></div>
            </div><!-- end element -->
    </div><!-- end element-set -->
]]></content>
  </entry>
  <entry>
    <id>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/201</id>
    <title><![CDATA[<h2>Glomerocryst</h2>]]></title>
    <updated>2019-07-04T09:53:07+01:00</updated>
    <link rel="alternate" type="text/html" href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/201"/>
    <content type="html"><![CDATA[<div class="element-set">
            <div id="dublin-core-title" class="element">
        <h3>Title</h3>
                    <div class="element-text"><h2>Glomerocryst</h2></div>
            </div><!-- end element -->
        <div id="dublin-core-subject" class="element">
        <h3>Subject</h3>
                    <div class="element-text"><span>A glomerocryst is a clump of phenocrysts. A rock in which clumping of phenocrysts is abundant and pervasive is said to have a glomeroporphyritic texture.</span></div>
            </div><!-- end element -->
    </div><!-- end element-set -->
]]></content>
  </entry>
  <entry>
    <id>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/202</id>
    <title><![CDATA[<h2>Glomeroporphyritic</h2>]]></title>
    <updated>2019-07-04T09:53:07+01:00</updated>
    <link rel="alternate" type="text/html" href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/202"/>
    <content type="html"><![CDATA[<div class="element-set">
            <div id="dublin-core-title" class="element">
        <h3>Title</h3>
                    <div class="element-text"><h2>Glomeroporphyritic</h2></div>
            </div><!-- end element -->
        <div id="dublin-core-subject" class="element">
        <h3>Subject</h3>
                    <div class="element-text"><span>This is an igneous texture in which phenocrysts clump together, within a fine-grained groundmass.</span></div>
            </div><!-- end element -->
    </div><!-- end element-set -->
]]></content>
  </entry>
  <entry>
    <id>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/203</id>
    <title><![CDATA[<h2>Granular (or phaneritic)</h2>]]></title>
    <summary><![CDATA[<em>Have a look at the <strong>hornblende biotite granite (<a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/4">L102</a>) </strong>in the 1A Reference Series.</em>]]></summary>
    <updated>2019-07-04T09:53:07+01:00</updated>
    <link rel="alternate" type="text/html" href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/203"/>
    <content type="html"><![CDATA[<div class="element-set">
            <div id="dublin-core-title" class="element">
        <h3>Title</h3>
                    <div class="element-text"><h2>Granular (or phaneritic)</h2></div>
            </div><!-- end element -->
        <div id="dublin-core-subject" class="element">
        <h3>Subject</h3>
                    <div class="element-text">This texture refers to an igneous or metamorphic rock which consists entirely of interlocking, roughly equant grains, large enough to be seen with naked eye.</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>hornblende biotite granite (<a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/4">L102</a>) </strong>in the 1A Reference Series.</em></div>
            </div><!-- end element -->
    </div><!-- end element-set -->
]]></content>
  </entry>
  <entry>
    <id>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/204</id>
    <title><![CDATA[<h2>Graphic texture</h2>]]></title>
    <updated>2019-07-04T09:53:08+01:00</updated>
    <link rel="alternate" type="text/html" href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/204"/>
    <link rel="enclosure" href="https://wserv3.esc.cam.ac.uk/p1acollections/files/original/b90e25b863bee88dd35e7098a3f2d7e4.png" type="image/png" length="37207"/>
    <content type="html"><![CDATA[<div class="element-set">
            <div id="dublin-core-title" class="element">
        <h3>Title</h3>
                    <div class="element-text"><h2>Graphic texture</h2></div>
            </div><!-- end element -->
        <div id="dublin-core-subject" class="element">
        <h3>Subject</h3>
                    <div class="element-text"><span>The regular intergrowth of two minerals (usually quartz and feldspar), which crystallised simultaneously. It is called “graphic” because the intergrowths resemble writing.</span></div>
            </div><!-- end element -->
    </div><!-- end element-set -->
]]></content>
  </entry>
</feed>
