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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;Adamantine [lustre]&lt;/h2&gt;</text>
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                <text>&lt;span&gt;Minerals displaying a diamond-like lustre are described as adamantine. These minerals are transparent or translucent and have very high refractive indices, producing the high degree of lustre. Zeolites, for example, have adamantine lustre.&lt;/span&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;Aeolian&lt;/h2&gt;</text>
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                <text>&lt;span&gt;Relating to or arising from the action of the wind; aeolian sediments are wind-blown. Also spelt eolian.&lt;/span&gt;</text>
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            <description>An account of the resource</description>
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                <text>Have a look at the ferruginous arenite sandstone (&lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/25"&gt;L326&lt;/a&gt;) in the 1A Reference Series.</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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            <description>A name given to the resource</description>
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                <text>&lt;h2&gt;Albite twinning&lt;/h2&gt;</text>
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                <text>&lt;span&gt;Named after albite (Na-plagioclase) twinning on the (010) crystallographic plane.&lt;br /&gt;See &lt;/span&gt;&lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/169"&gt;lamellar twinning&lt;/a&gt;&lt;span&gt;.&lt;/span&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;Lamellar twinning&lt;/h2&gt;</text>
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                <text>&lt;span&gt;Many parallel twins can be produced within one mineral grain by multiple parallel twin planes. This is known as lamellar twinning. It is a diagnostic characteristic of plagioclase feldspar, and is sometimes referred to as &lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/168"&gt;albite twinning&lt;/a&gt;.&lt;/span&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;Alteration&lt;/h2&gt;</text>
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                <text>&lt;span&gt;Rocks undergo mineralogical change at low pressures, produced by reactions with circulating fluids. The replacement of the original minerals in the rock tends to take place primarily along cracks and around the edges of grains, though whole mineral grains can be replaced. The decomposition of olivine to serpentine is a common example of alteration.&lt;br /&gt;&lt;/span&gt;</text>
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                <text>&lt;em&gt;Common alteration minerals include clays for plagioclase, &lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/54"&gt;serpentine&lt;/a&gt; for olivine, and &lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/53"&gt;chlorite&lt;/a&gt; for ferromagnesian minerals such as biotite.&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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              <name>Title</name>
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            <description>A name given to the resource</description>
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                <text>&lt;h2&gt;Amorphous&lt;/h2&gt;</text>
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            <name>Subject</name>
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                <text>&lt;span&gt;Amorphous materials are non-crystalline solids. That is to say that they do not display long-range order in their structures. Glass is amorphous.&lt;/span&gt;</text>
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            <description>An account of the resource</description>
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                <text>&lt;em&gt;Have a look at the&lt;span&gt;&lt;strong&gt; rhyolite glass (&lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/7"&gt;L113&lt;/a&gt;)&lt;/strong&gt; i&lt;/span&gt;n the 1A Reference Series.&lt;/em&gt;</text>
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  <item itemId="172" public="1" featured="0">
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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;Amygdale&lt;/h2&gt;</text>
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                <text>&lt;span&gt;A vesicle (necessarily in an igneous rock), which has been filled in by a mineral crystallising from late-stage fluids. Amygdales are commonly produced by the crystallisation of &lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/57"&gt;quartz&lt;/a&gt;, &lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/64"&gt;calcite&lt;/a&gt; or zeolite.&lt;/span&gt;</text>
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            <description>An account of the resource</description>
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                <text>&lt;em&gt;Have a look at the &lt;strong&gt;amygdaloidal basalt (&lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/11"&gt;L161&lt;/a&gt;) &lt;/strong&gt;in the 1A Reference Series.&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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            <description>A name given to the resource</description>
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                <text>&lt;h2&gt;Anhedral&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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                <text>&lt;span&gt;A crystal displaying none of its characteristic crystal faces is called anhedral.&lt;/span&gt;</text>
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          <element elementId="41">
            <name>Description</name>
            <description>An account of the resource</description>
            <elementTextContainer>
              <elementText elementTextId="468">
                <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; for anhedral quartz, biotite and plagioclase.&lt;/em&gt;</text>
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  <item itemId="174" public="1" featured="0">
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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;Anisotropic&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;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 different velocities depending on the direction in which the light is passing through it, the mineral is anisotropic. That is to say, it has different refractive indices in different orientations.&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;/div&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/213"&gt;isotropic&lt;/a&gt;.&lt;/em&gt;</text>
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              <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>Glossary</text>
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                <text>&lt;h2&gt;Aphanitic (or aphyric)&lt;/h2&gt;</text>
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                <text>&lt;span&gt;Igneous rocks made up of grains too small to be seen with the naked eye have an aphanitic texture. These rocks do not contain phenocrysts. They are non-porphyritic.&lt;/span&gt;</text>
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