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                <text>&lt;h2&gt;Serpentine&lt;/h2&gt;</text>
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                <text>&lt;span&gt;Serpentine is a common alteration product of olivine, produced by hydration at low temperatures.&lt;/span&gt;</text>
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                <text>&lt;div class="element"&gt;
&lt;h3&gt;Formula&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;Mg&lt;sub&gt;3&lt;/sub&gt;[Si&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt;](OH)&lt;sub&gt;4&lt;/sub&gt;&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Structure&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;Sheet silicate&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Crystal System&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;&lt;em&gt;Crystal system:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;monoclinic or orthorhombic (-)&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Optical Properties&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p class="NoSpacing"&gt;&lt;span&gt;Serpentine is commonly very fine-grained. It can be recognised by its textural association with olivine and by its low birefringence and habit.&lt;/span&gt;&lt;/p&gt;
&lt;p class="NoSpacing"&gt;&lt;em&gt;&lt;span&gt;Colour in plane polarised light:&lt;/span&gt;&lt;/em&gt;&lt;span&gt; green&lt;/span&gt;&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;&lt;em&gt;&lt;span&gt;Relief:&lt;/span&gt;&lt;/em&gt;&lt;span&gt; low&lt;/span&gt;&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;&lt;em&gt;&lt;span&gt;Birefringence:&lt;/span&gt;&lt;/em&gt;&lt;span&gt; 1&lt;sup&gt;st&lt;/sup&gt; order&lt;/span&gt;&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Rock Specimens&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;&lt;a href="/p1acollections/exhibits/show/igneous-rocks/l141"&gt;L141 Gabbro&lt;/a&gt;&lt;span&gt; &lt;/span&gt;&lt;br /&gt;&lt;a href="/p1acollections/exhibits/show/igneous-rocks/l162"&gt;L162 Basalt, porphyritic&lt;/a&gt;&lt;span&gt; &lt;/span&gt;&lt;br /&gt;&lt;a href="/p1acollections/exhibits/show/igneous-rocks/l172"&gt;L172 Ultramafic cumulate&lt;/a&gt;&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Mineral Name&lt;/h3&gt;
&lt;div class="element-text"&gt;serpentine&lt;/div&gt;
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        <name>alteration</name>
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        <name>hydration</name>
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        <name>olivine</name>
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              <name>Description</name>
              <description>An account of the resource</description>
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                  <text>This glossary describes a number of geological terms with which the 1A students should become familiar.&lt;span&gt; It is by no means an exhaustive list, but is aimed to help you understand the material within the first year course.&lt;/span&gt;</text>
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                <text>&lt;h2&gt;Simple twinning&lt;/h2&gt;</text>
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                <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 &lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/179"&gt;Carlsbad twins&lt;/a&gt;.</text>
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                  <text>This glossary describes a number of geological terms with which the 1A students should become familiar.&lt;span&gt; It is by no means an exhaustive list, but is aimed to help you understand the material within the first year course.&lt;/span&gt;</text>
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                <text>&lt;h2&gt;Solid solution&lt;/h2&gt;</text>
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                <text>Minerals such as quartz have a discrete composition and thus one chemical formula (in this case SiO&lt;sub&gt;2&lt;/sub&gt;). 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&lt;sub&gt;4&lt;/sub&gt;). By gradually replacing Fe atoms with Mg atoms, a continuous range of compositions can be produced ending at the Mg end-member, fayallite (MgSiO&lt;sub&gt;4&lt;/sub&gt;). The range of compositions is called a solid solution.</text>
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                <text>&lt;h2&gt;Specific gravity, D&lt;/h2&gt;</text>
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                <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&lt;sup&gt;-3&lt;/sup&gt;, olivine has a density of 3.22 g cm&lt;sup&gt;-3&lt;/sup&gt;.</text>
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                <text>&lt;h2&gt;Sphene&lt;strong&gt; (titanite)&lt;/strong&gt;&lt;/h2&gt;</text>
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                <text>&lt;div class="element"&gt;
&lt;h3&gt;Formula&lt;/h3&gt;
&lt;div class="element-text"&gt;CaTi[SiO&lt;sub&gt;4&lt;/sub&gt;](O, OH, F)&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Structure&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;Orthosilicate&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Crystal System&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;&lt;em&gt;Crystal system:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;monoclinic (+)&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Physical Properties&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;&lt;em&gt;Colour in hand specimen:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;colourless, yellow, green, brown or black&lt;br /&gt;&lt;em&gt;Cleavage:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;one, good&lt;br /&gt;&lt;em&gt;Hardness:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;5&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Optical Properties&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;&lt;em&gt;Colour in plane polarised light:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;colourless, yellow or typically brown&lt;br /&gt;&lt;em&gt;Pleochroism:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;moderate if coloured&lt;br /&gt;&lt;em&gt;Relief:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;high&lt;br /&gt;&lt;em&gt;Birefringence:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;0.100-0.192; &amp;gt;4th order&lt;br /&gt;&lt;em&gt;Extinction:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;inclined&lt;br /&gt;&lt;em&gt;Twinning:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;simple twins; occasionally lamellar twins&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Rock Specimens&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;&lt;a href="/p1acollections/exhibits/show/igneous-rocks/l101"&gt;L101 Granite&lt;/a&gt;&lt;span&gt; &lt;/span&gt;&lt;br /&gt;&lt;a href="/p1acollections/exhibits/show/igneous-rocks/l120"&gt;L120 Granodiorite&lt;/a&gt;&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Mineral Name&lt;/h3&gt;
&lt;div class="element-text"&gt;sphene&lt;br /&gt;titanite&lt;br /&gt;&lt;h3&gt;Advanced notes&lt;/h3&gt;
&lt;div class="element-text"&gt;Diamond shaped cross sections are common&lt;br /&gt;&lt;br /&gt;&lt;/div&gt;
&lt;/div&gt;
&lt;/div&gt;</text>
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                <text>&lt;h2&gt;Splendent [lustre]&lt;/h2&gt;</text>
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                <text>&lt;em&gt;See &lt;strong&gt;&lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/224"&gt;metallic&lt;/a&gt;&lt;/strong&gt;.&lt;/em&gt;</text>
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                  <text>This glossary describes a number of geological terms with which the 1A students should become familiar.&lt;span&gt; It is by no means an exhaustive list, but is aimed to help you understand the material within the first year course.&lt;/span&gt;</text>
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                <text>&lt;h2&gt;Subhedral&lt;/h2&gt;</text>
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                <text>A crystal displaying some, but not all of its characteristic crystal faces is called subhedral.</text>
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                  <text>This glossary describes a number of geological terms with which the 1A students should become familiar.&lt;span&gt; It is by no means an exhaustive list, but is aimed to help you understand the material within the first year course.&lt;/span&gt;</text>
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                <text>&lt;h2&gt;Sutured contacts&lt;/h2&gt;</text>
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                <text>Usually refers to quartz grains, which have undergone partial recrystallisation, producing irregular, sutured grain boundaries.</text>
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          <element elementId="41">
            <name>Description</name>
            <description>An account of the resource</description>
            <elementTextContainer>
              <elementText elementTextId="671">
                <text>&lt;em&gt;Have a look at the &lt;strong&gt;quartzites (&lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/39"&gt;L520&lt;/a&gt;, &lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/40"&gt;L521&lt;/a&gt;)&lt;/strong&gt; in the 1A Reference Series.&lt;/em&gt;</text>
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  </item>
  <item itemId="258" public="1" featured="0">
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          <name>Dublin Core</name>
          <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>
          <elementContainer>
            <element elementId="41">
              <name>Description</name>
              <description>An account of the resource</description>
              <elementTextContainer>
                <elementText elementTextId="13">
                  <text>This glossary describes a number of geological terms with which the 1A students should become familiar.&lt;span&gt; It is by no means an exhaustive list, but is aimed to help you understand the material within the first year course.&lt;/span&gt;</text>
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            <element elementId="50">
              <name>Title</name>
              <description>A name given to the resource</description>
              <elementTextContainer>
                <elementText elementTextId="14">
                  <text>Glossary</text>
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    <elementSetContainer>
      <elementSet elementSetId="1">
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          <element elementId="50">
            <name>Title</name>
            <description>A name given to the resource</description>
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                <text>&lt;h2&gt;Tabular&lt;/h2&gt;</text>
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          <element elementId="49">
            <name>Subject</name>
            <description>The topic of the resource</description>
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              <elementText elementTextId="673">
                <text>Flat, planar, non-elongate crystals are described as having a tabular habit. Tabular crystals are thicker than platy crystals.</text>
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  <item itemId="259" public="1" featured="0">
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          <name>Dublin Core</name>
          <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>
          <elementContainer>
            <element elementId="41">
              <name>Description</name>
              <description>An account of the resource</description>
              <elementTextContainer>
                <elementText elementTextId="13">
                  <text>This glossary describes a number of geological terms with which the 1A students should become familiar.&lt;span&gt; It is by no means an exhaustive list, but is aimed to help you understand the material within the first year course.&lt;/span&gt;</text>
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              <name>Title</name>
              <description>A name given to the resource</description>
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                  <text>Glossary</text>
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      <elementSet elementSetId="1">
        <name>Dublin Core</name>
        <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>&lt;h2&gt;Tartan twinning&lt;/h2&gt;</text>
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          <element elementId="41">
            <name>Description</name>
            <description>An account of the resource</description>
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                <text>&lt;em&gt;See&lt;span&gt; &lt;/span&gt;&lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/183"&gt;cross-hatched twinning&lt;/a&gt;.&lt;/em&gt;</text>
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