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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;Fissility&lt;/h2&gt;</text>
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                <text>&lt;span&gt;This refers to the tendency of some sedimentary rocks to break along their bedding planes. Shales are fissile. Fissility is distinct from cleavage because cleavage is not aligned with the bedding planes.&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;Flow banding&lt;/h2&gt;</text>
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                <text>This occurs when an inhomogeneous magma flows, thereby drawing out the inhomogeneities into bands of different compositions. When this happens on a very fine scale it is called flow lamination.</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;Foliation&lt;/h2&gt;</text>
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                <text>&lt;span&gt;This refers to any pervasive planar feature in a rock. It is produced by the arrangement of the constituent grains into sheet-like structures, usually in compositionally distinct layers. Foliations can be primary (e.g. bedding, fissility, flow banding) or secondary (e.g. cleavage).&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;Form&lt;/h2&gt;</text>
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                <text>&lt;em&gt;See&lt;span&gt; &lt;/span&gt;&lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/206"&gt;habit&lt;/a&gt;.&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;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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          <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;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;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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                <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;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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                <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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      </elementSet>
    </elementSetContainer>
  </item>
</itemContainer>
