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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;Hypermelanic&lt;/h2&gt;</text>
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                <text>&lt;span&gt;Hypermelanic rocks have a very high colour index. That is to say that &amp;gt;90 vol% of the rock is made up of ferromagnesian minerals.&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;Hypabyssal&lt;/h2&gt;</text>
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                <text>Hypabyssal rocks and textures are those associated with very shallow magmatic intrusions, where cooling is moderately rapid. This term is restricted to relatively small intrusive bodies centimetres to tens of metres in diameter.</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;Hardness&lt;/h2&gt;</text>
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            <description>The topic of the resource</description>
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                <text>Hardness is measured on the Mohs scale. A hard mineral is rigid, resistant to pressure and is not easily scratched. Determining the hardness (or relative hardness) of a mineral in hand specimen can aid your identification of the mineral.</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;Habit (or form)&lt;/h2&gt;</text>
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                <text>The three dimensional shape of a crystal. The crystal structure of a mineral influences the characteristic habit(s) which it displays. For example, biotite mica tends to display a platy or tabular habit because its crystal lattice is made up of sheets.</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;Groundmass&lt;/h2&gt;</text>
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                <text>Rapidly cooled magmas are largely made-up of many tiny crystals. These make up the groundmass.</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;Graphic texture&lt;/h2&gt;</text>
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            <description>The topic of the resource</description>
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                <text>&lt;span&gt;The regular intergrowth of two minerals (usually quartz and feldspar), which crystallised simultaneously. It is called “graphic” because the intergrowths resemble writing.&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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            <description>A name given to the resource</description>
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                <text>&lt;h2&gt;Granular (or phaneritic)&lt;/h2&gt;</text>
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                <text>This texture refers to an igneous or metamorphic rock which consists entirely of interlocking, roughly equant grains, large enough to be seen with naked eye.</text>
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                <text>&lt;em&gt;Have a look at the &lt;strong&gt;hornblende biotite granite (&lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/4"&gt;L102&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;Glomeroporphyritic&lt;/h2&gt;</text>
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                <text>&lt;span&gt;This is an igneous texture in which phenocrysts clump together, within a fine-grained groundmass.&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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            <name>Title</name>
            <description>A name given to the resource</description>
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                <text>&lt;h2&gt;Glomerocryst&lt;/h2&gt;</text>
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                <text>&lt;span&gt;A glomerocryst is a clump of phenocrysts. A rock in which clumping of phenocrysts is abundant and pervasive is said to have a glomeroporphyritic texture.&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;Glass&lt;/h2&gt;</text>
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                <text>&lt;span&gt;When magma is quenched (cooled exceedingly rapidly) even very small crystals are unable to grow. Instead, a volcanic glass is formed. It is amorphous (having no crystalline structure), and is consequently isotropic.&lt;/span&gt;</text>
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                <text>&lt;em&gt;Have a look at the&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;&lt;span&gt; &lt;/span&gt;in the 1A Reference Series.&lt;/em&gt;</text>
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