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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;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>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>Pleochroism</text>
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                <text>Some minerals are pleochroic. When rotated under plane polarised light they change colour. Biotite and the amphibole hornblende are pleochroic.</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/50"&gt;hornblende amphibole&lt;/a&gt; (M201, M211) &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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