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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;Lineation&lt;/h2&gt;</text>
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&lt;p&gt;This refers to any pervasive linear feature in a rock. It can be produced by the intersection of two foliations (planar rock fabrics) or by the alignment of linear objects such as elongate grains in the rock. Linear fabrics can be primary (e.g. flow lineations) or secondary (e.g. mineral alignment during metamorphism).&lt;/p&gt;
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                <text>&lt;h2&gt;Leucocratic&lt;/h2&gt;</text>
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&lt;p&gt;Leucocratic rocks have a low colour index. That is to say that &amp;lt;30 vol% of the rock is made up of ferromagnesian minerals.&lt;/p&gt;
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                <text>&lt;h2&gt;Length slow&lt;/h2&gt;</text>
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                <text>&lt;span&gt;All anisotropic minerals have fast and slow vibration directions. If the &lt;/span&gt;&lt;strong&gt;slow&lt;/strong&gt;&lt;span&gt;&lt;strong&gt; &lt;/strong&gt;vibration direction is parallel to the direction of &lt;strong&gt;elongation&lt;/strong&gt; of the crystal, it is said to be length &lt;/span&gt;&lt;strong&gt;slow&lt;/strong&gt;&lt;span&gt;.&lt;/span&gt;</text>
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                <text>&lt;em&gt;Compare with&lt;span&gt; &lt;/span&gt;&lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/216"&gt;length fast&lt;/a&gt;.&lt;/em&gt;</text>
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                <text>&lt;h2&gt;Length fast&lt;/h2&gt;</text>
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                <text>&lt;span&gt;All anisotropic minerals have fast and slow vibration directions. If the &lt;/span&gt;&lt;strong&gt;fast&lt;/strong&gt;&lt;span&gt;&lt;strong&gt; &lt;/strong&gt;vibration direction is parallel to the direction of &lt;strong&gt;elongation&lt;/strong&gt; of the crystal, the crystal is length &lt;/span&gt;&lt;strong&gt;fast&lt;/strong&gt;&lt;span&gt;.&lt;/span&gt;</text>
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                <text>&lt;em&gt;Compare with&lt;span&gt; &lt;/span&gt;&lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/217"&gt;length slow&lt;/a&gt;.&lt;/em&gt;</text>
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                <text>&lt;h2&gt;Lath&lt;/h2&gt;</text>
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                <text>A crystal with an elongate, needle-like form is said to be lath-shaped. This term is most commonly applied to elongate crystals of feldspar in igneous rocks.</text>
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                <text>&lt;h2&gt;Kinks&lt;/h2&gt;</text>
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                <text>These are bands of deformation in which the orientation is changed due to slipping on several parallel slip planes. Kinks can occur in a single crystal or in foliated rock.</text>
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                <text>&lt;h2&gt;Isotropic&lt;/h2&gt;</text>
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                <text>&lt;p&gt;The speed of light through any medium is inversely proportional to the refractive index of the medium. The refractive index of a mineral is determined by the arrangement and type of atoms within its structure.&lt;/p&gt;
&lt;p&gt;If the structure of the mineral allows light to travel at the same velocity through the mineral in all orientations, the mineral is isotropic. That is to say, it has the same refractive index in all directions. Under cross-polarised light isotropic minerals always appear black. Garnet is an isotropic mineral&lt;/p&gt;</text>
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                <text>&lt;em&gt;Compare with&lt;span&gt; &lt;/span&gt;&lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/174"&gt;anisotropic&lt;/a&gt;.&lt;/em&gt;</text>
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                <text>&lt;h2&gt;Intrusive&lt;/h2&gt;</text>
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                <text>Rocks which have formed by the intrusion of igneous material below the surface of the Earth are described as intrusive.</text>
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                <text>&lt;em&gt;Compare with&lt;span&gt; &lt;/span&gt;&lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/191"&gt;extrusive&lt;/a&gt;.&lt;/em&gt;</text>
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                <text>An igneous texture in which large &lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/173"&gt;anhedral&lt;/a&gt; grains fill the gaps between earlier crystallising phases.</text>
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          <element elementId="41">
            <name>Description</name>
            <description>An account of the resource</description>
            <elementTextContainer>
              <elementText elementTextId="557">
                <text>&lt;em&gt;Have a look at the &lt;strong&gt;granodiorite (&lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/8"&gt;L120&lt;/a&gt;)&lt;/strong&gt; in the 1A Reference Series.&lt;/em&gt;</text>
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  <item itemId="210" 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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          </elementContainer>
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    </collection>
    <elementSetContainer>
      <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>
        <elementContainer>
          <element elementId="50">
            <name>Title</name>
            <description>A name given to the resource</description>
            <elementTextContainer>
              <elementText elementTextId="552">
                <text>&lt;h2&gt;Inclusion&lt;/h2&gt;</text>
              </elementText>
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          </element>
          <element elementId="49">
            <name>Subject</name>
            <description>The topic of the resource</description>
            <elementTextContainer>
              <elementText elementTextId="553">
                <text>As a crystal grows in a magma, tiny blobs of melt can become trapped in its structure. These are melt inclusions. Small crystals of other minerals can also become trapped. These are mineral inclusions.</text>
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          <element elementId="41">
            <name>Description</name>
            <description>An account of the resource</description>
            <elementTextContainer>
              <elementText elementTextId="554">
                <text>Have a look at the &lt;strong&gt;alkali basalt (&lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/1"&gt;L100&lt;/a&gt;)&lt;/strong&gt;, the &lt;strong&gt;porphyritic rhyolite (&lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/5"&gt;L110&lt;/a&gt;)&lt;/strong&gt; and the &lt;strong&gt;garnet schist (&lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/38"&gt;L504&lt;/a&gt;)&lt;/strong&gt; in the 1A Reference Series.</text>
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