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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;Resinous [lustre]&lt;/h2&gt;</text>
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                <text>&lt;div&gt;
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&lt;p&gt;Minerals displaying the lustre of resin or of smooth-surfaced plastic are described as resinous. Amber, for example, has resinous lustre.&lt;/p&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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            <name>Title</name>
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                <text>&lt;h2&gt;Replacement&lt;/h2&gt;</text>
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                <text>An igneous texture in which a mineral grain is resorbed and a later crystallising phase grows in its place.</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;Relief&lt;/h2&gt;</text>
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                <text>&lt;p&gt;When viewed under plane polarised light, some mineral grains are more clearly defined than others. They have heavier, darker edges. These minerals have higher relief.&lt;/p&gt;
&lt;p&gt;Relief is determined by the difference in the refractive indices of the grain and mounting medium. The mounting medium typically has a refractive index (R.I., n&lt;sub&gt;i&lt;/sub&gt;) of ~1.54. A mineral with a low refractive index, such as quartz (R.I., n&lt;sub&gt;i&lt;/sub&gt; ~1.5) has low relief because it has a refractive index very similar to that of the mounting medium. A mineral with a high refractive index, such as garnet (R.I., n&lt;sub&gt;i&lt;/sub&gt; ~1.7) has high relief because it has a refractive index much higher than that of the mounting medium.&lt;/p&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;Prismatic&lt;/h2&gt;</text>
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                <text>&lt;span&gt;An elongate “pencil-like” crystal habit. Prismatic crystals are wider than acicular crystals.&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;Porphyroblast&lt;/h2&gt;</text>
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                <text>&lt;p&gt;A porphyroblast is the metamorphic equivalent of a phenocryst. Do not confuse them! It is a large crystal set into a finer-grained fabric, in a metamorphic rock.&lt;/p&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;&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;&lt;/p&gt;
&lt;/div&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;Porphyritic&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;An igneous rock containing phenocrysts in a fine-grained groundmass is said to have a porphyritic texture.&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;/div&gt;
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          <name>Dublin Core</name>
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              <name>Description</name>
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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;Porosity&lt;/h2&gt;</text>
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                <text>&lt;p&gt;The proportion of the material occupied by space, measured in volume percent. A porous material contains fluid-filled spaces, or pores, while a non-porous material does not. NB, make sure you understand the difference between porosity and permeability.&lt;/p&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;&lt;em&gt;Compare with&lt;span&gt; &lt;/span&gt;&lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/234"&gt;permeability&lt;/a&gt;.&lt;/em&gt;&lt;/p&gt;
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&lt;/div&gt;
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          <name>Dublin Core</name>
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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;Polycrystalline&lt;/h2&gt;</text>
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            <description>The topic of the resource</description>
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                <text>&lt;p&gt;A crystalline sample of a single mineral, containing many crystals. Quartzite, for example, is polycrystalline quartz.&lt;/p&gt;</text>
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                <text>&lt;em&gt;Have a look at the &lt;strong&gt;quartzites (&lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/39"&gt;L520&lt;/a&gt;, &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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                <text>&lt;h2&gt;Poikilitic&lt;/h2&gt;</text>
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                <text>An igneous texture in which a small number of large grains enclose many smaller grains of another phase.</text>
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                <text>&lt;em&gt;Have a look at the &lt;strong&gt;gabbro (&lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/10"&gt;L141&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;Plutonic&lt;/h2&gt;</text>
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                <text>Plutonic rocks and textures are those associated with deep magmatic intrusions, where cooling is slow. Crystals are thus able to grow very large, producing coarse-grained textures. This term is restricted to large igneous bodies more than hundreds of metres in diameter.</text>
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