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                <text>Chronostratigraphic Chart</text>
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                <text>Michel-Levy Chart</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;Zonation&lt;/h2&gt;</text>
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                <text>As a crystal grows slowly in a magma chamber the magma from which it is crystallising may evolve, changing its composition. Thus later crystallising regions or “zones” of the crystal will have a slightly different composition from earlier crystallising regions. The crystal thus displays zonation.&lt;br /&gt;Zonation is seen under cross-polarised light by variations in the birefringence colours of the different zones.</text>
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                <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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                  <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;Volcanic&lt;/h2&gt;</text>
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                <text>Volcanic rocks and textures are those associated with magmatic eruptions at the surface of the Earth. These eruptions can occur into air, water or ice. In each case cooling is very rapid, causing fine-grained textures to develop.</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;Vitreous [lustre]&lt;/h2&gt;</text>
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                <text>Minerals displaying a glass-like lustre are described as vitreous. These minerals are transparent or translucent and have relatively low refractive indices. Quartz and calcite, for example, have vitreous lustre.</text>
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            <name>Description</name>
            <description>An account of the resource</description>
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                <text>Have a look at &lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/57"&gt;quartz&lt;/a&gt; (M410, M411, M412) and &lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/64"&gt;calcite&lt;/a&gt; (M540, M541, M542) in the 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;Vesicular&lt;/h2&gt;</text>
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                <text>Igneous rocks with a vesicular texture contain air bubbles, called vesicles. These can be round or distorted. In thin-section, vesicles are filled with the mounting medium and consequently appear clear and colourless with low relief under plain polarised light. They are isotropic. Vesicles which are infilled with precipitated minerals, such as calcite or quartz are called amygdales.</text>
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                <text>Have a look at the rhyolitic glass (&lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/7"&gt;L113&lt;/a&gt;) and the porphyritic andesite (&lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/9"&gt;L130&lt;/a&gt;) in the 1A Reference Series.</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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            <name>Title</name>
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                <text>&lt;h2&gt;Undulose extinction&lt;/h2&gt;</text>
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                <text>If some areas of a mineral grain have different extinction positions from other areas of the same grain, the grain is said to display undulose extinction. Importantly, there is no sharp division between areas with different extinction positions; otherwise the phenomenon could be due to twinning. Undulose extinction is frequently observed in strained quartz, where the crystal lattice has been distorted by being squeezed.</text>
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                <text>&lt;em&gt;Have a look at the &lt;strong&gt;ferruginous sandstone (&lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/26"&gt;L327&lt;/a&gt;) &lt;/strong&gt;and the&lt;strong&gt; quartzite (&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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                  <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>&lt;h2&gt;Twinning&lt;/h2&gt;</text>
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          <element elementId="49">
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                <text>Within a single mineral grain the crystal lattice may be oriented differently on either side of a plane, or twin plane. Thus the grain will go into extinction at different positions on either side of the twin plane. This is twinning.</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;Turbidite&lt;/h2&gt;</text>
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                <text>Sedimentary rock structure characterised by a fining-up sequence. They are produced by turbidity flows.</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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            <name>Title</name>
            <description>A name given to the resource</description>
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                <text>&lt;h2&gt;Tectosilicate&lt;/h2&gt;</text>
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            <description>The topic of the resource</description>
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                <text>&lt;p&gt;Framework silicate.&lt;/p&gt;</text>
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