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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;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;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;Leucocratic&lt;/h2&gt;</text>
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                <text>&lt;div&gt;
&lt;div class="element-set"&gt;
&lt;div class="element"&gt;
&lt;div class="element-text"&gt;
&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;
&lt;/div&gt;
&lt;/div&gt;
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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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                <text>&lt;div&gt;
&lt;div class="element-set"&gt;
&lt;div class="element"&gt;
&lt;div class="element-text"&gt;
&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;
&lt;/div&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;/div&gt;</text>
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                <text>&lt;h2&gt;Lustre&lt;/h2&gt;</text>
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                <text>A combination of the intensity and quality of the light reflected from the surface of a mineral. A number of terms are used to describe the range of lustres displayed by minerals, including adamantine, dull, metallic, pearly, resinous and vitreous.</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;Macrocryst&lt;/h2&gt;</text>
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                <text>A relatively large crystal, usually occurring within an igneous rock. Unlike the term phenocryst, it does not imply a petrogenetic link between the crystal and the surrounding magma.</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/236"&gt;phenocryst&lt;/a&gt;.&lt;/em&gt;</text>
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                <text>&lt;h2&gt;Melanocratic&lt;/h2&gt;</text>
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                <text>Melanocratic rocks have a high colour index. That is to say that 60-90 vol% of the rock is made up of ferromagnesian minerals.</text>
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                <text>&lt;h2&gt;Mesocratic&lt;/h2&gt;</text>
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            <name>Subject</name>
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                <text>Mesocratic rocks have a moderate colour index. That is to say that 30-60 vol% of the rock is made up of ferromagnesian minerals.</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;Metallic [lustre]&lt;/h2&gt;</text>
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                <text>Minerals displaying a metal-like lustre are described as metallic. These minerals have surfaces which are perfectly reflective. Pyrite, for example, has metallic lustre.</text>
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                <text>&lt;em&gt;Have a look at &lt;strong&gt;pyrite (&lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/60"&gt;M520&lt;/a&gt;)&lt;/strong&gt; in the 1A Reference Series.&lt;/em&gt;</text>
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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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              <description>A name given to the resource</description>
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                  <text>Glossary</text>
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                <text>&lt;h2&gt;Micaceous&lt;/h2&gt;</text>
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            <name>Subject</name>
            <description>The topic of the resource</description>
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                <text>A rock containing a significant proportion of micas is described as micaceous. The micas are a group of sheet silicate minerals, which include biotite and muscovite.</text>
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                <text>&lt;em&gt;Have a look at &lt;strong&gt;&lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/51"&gt;muscovite mica&lt;/a&gt; (M301, M302) &lt;/strong&gt;and &lt;strong&gt;&lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/52"&gt;biotite mica&lt;/a&gt; (M303, M304)&lt;/strong&gt; in the 1A Reference Series.&lt;/em&gt;</text>
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