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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;Mohs scale&lt;/h2&gt;</text>
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                <text>Mineral hardness is described using the Mohs scale. The scale runs from very soft at 0 up to very hard at 10. The positions of minerals are determined by their relative hardness. For example, quartz can scratch calcite, but calcite cannot scratch quartz. Thus quartz is harder than calcite.</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;Microperthite texture&lt;/h2&gt;</text>
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                <text>Parallel lamellae or trains of blebs of one mineral, all in the same optical orientation, are enclosed in a single “host” crystal of another mineral. This texture is generally attributed to solid-state exsolution of the daughter phase from the host.</text>
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                <text>&lt;em&gt;Have a look at the &lt;strong&gt;alkali granite (&lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/1"&gt;L100&lt;/a&gt;)&lt;/strong&gt; and 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;Microcrystalline&lt;/h2&gt;</text>
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                <text>Rocks with a crystalline structure in which the individual crystals cannot be identified by the naked eye, but are large enough to be identified using standard optical microscopy are described as microcrystalline.</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/184"&gt;cryptocrystalline&lt;/a&gt;.&lt;/em&gt;&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;/div&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;Microcline twinning&lt;/h2&gt;</text>
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            <name>Description</name>
            <description>An account of the resource</description>
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              <elementText elementTextId="594">
                <text>&lt;em&gt;See&lt;span&gt; &lt;/span&gt;&lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/183"&gt;cross-hatched twins&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;Micaceous&lt;/h2&gt;</text>
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                <text>A rock containing a significant proportion of micas is described as micaceous. The micas are a group of sheet silicate minerals, which include biotite and muscovite.</text>
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              <elementText elementTextId="592">
                <text>&lt;em&gt;Have a look at &lt;strong&gt;&lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/51"&gt;muscovite mica&lt;/a&gt; (M301, M302) &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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          <name>Dublin Core</name>
          <description>The Dublin Core metadata element set is common to all Omeka records, including items, files, and collections. For more information see, http://dublincore.org/documents/dces/.</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>
              <description>A name given to the resource</description>
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            <name>Title</name>
            <description>A name given to the resource</description>
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                <text>&lt;h2&gt;Metallic [lustre]&lt;/h2&gt;</text>
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                <text>Minerals displaying a metal-like lustre are described as metallic. These minerals have surfaces which are perfectly reflective. Pyrite, for example, has metallic lustre.</text>
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                <text>&lt;em&gt;Have a look at &lt;strong&gt;pyrite (&lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/60"&gt;M520&lt;/a&gt;)&lt;/strong&gt; in the 1A Reference Series.&lt;/em&gt;</text>
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  <item itemId="223" public="1" featured="0">
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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;Mesocratic&lt;/h2&gt;</text>
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                <text>Mesocratic rocks have a moderate colour index. That is to say that 30-60 vol% of the rock is made up of ferromagnesian minerals.</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;Melanocratic&lt;/h2&gt;</text>
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            <name>Subject</name>
            <description>The topic of the resource</description>
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                <text>Melanocratic rocks have a high colour index. That is to say that 60-90 vol% of the rock is made up of ferromagnesian minerals.</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;Macrocryst&lt;/h2&gt;</text>
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                <text>A relatively large crystal, usually occurring within an igneous rock. Unlike the term phenocryst, it does not imply a petrogenetic link between the crystal and the surrounding magma.</text>
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                <text>&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;</text>
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        <name>Dublin Core</name>
        <description>The Dublin Core metadata element set is common to all Omeka records, including items, files, and collections. For more information see, http://dublincore.org/documents/dces/.</description>
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          <element elementId="50">
            <name>Title</name>
            <description>A name given to the resource</description>
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                <text>&lt;h2&gt;Lustre&lt;/h2&gt;</text>
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          <element elementId="49">
            <name>Subject</name>
            <description>The topic of the resource</description>
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                <text>A combination of the intensity and quality of the light reflected from the surface of a mineral. A number of terms are used to describe the range of lustres displayed by minerals, including adamantine, dull, metallic, pearly, resinous and vitreous.</text>
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