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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;Microcline twinning&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/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;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;
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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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            <name>Title</name>
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                <text>&lt;h2&gt;Mohs scale&lt;/h2&gt;</text>
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            <name>Subject</name>
            <description>The topic of the resource</description>
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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;Ooid&lt;/h2&gt;</text>
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                <text>Sub-spherical sedimentary grains comprising a nucleus surrounded by concentric layers of carbonate precipitate. Ooids form abiogenically. They are sometimes referred to as ooliths.</text>
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                <text>&lt;em&gt;Have a look at the &lt;strong&gt;oolitic ironstone (&lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/34"&gt;L361&lt;/a&gt;) &lt;/strong&gt;and the&lt;strong&gt; oolitic limestone (&lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/32"&gt;L353&lt;/a&gt;)&lt;/strong&gt; in the 1A Reference Series.&lt;/em&gt;</text>
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  <item itemId="231" public="1" featured="0">
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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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              <name>Title</name>
              <description>A name given to the resource</description>
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                  <text>Glossary</text>
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            <name>Title</name>
            <description>A name given to the resource</description>
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                <text>&lt;h2&gt;Orthosilicate&lt;/h2&gt;</text>
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                <text>&lt;span&gt;Silicate minerals in which the SiO4 tetrahedra do not share oxygen atoms with one another are called orthosilicates, or island silicates. These minerals do not contain bridging oxygen atoms.&lt;/span&gt;</text>
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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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              <name>Title</name>
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            <name>Title</name>
            <description>A name given to the resource</description>
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                <text>&lt;h2&gt;Overgrowth&lt;/h2&gt;</text>
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                <text>The crystallisation of one mineral on the surface of another, producing a rim or part of a rim.</text>
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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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        <name>Dublin Core</name>
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            <name>Title</name>
            <description>A name given to the resource</description>
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                <text>&lt;h2&gt;Pearly [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>&lt;span&gt;Unsurprisingly the quality and intensity of light reflected from minerals displaying “pearly” lustre is reminiscent of pearls. This effect is produced by the reflection of light from many thin, coplanar, transparent sheets within the mineral. Muscovite, for example, has pearly lustre.&lt;/span&gt;</text>
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            <name>Description</name>
            <description>An account of the resource</description>
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              <elementText elementTextId="613">
                <text>&lt;em&gt;Have a look at the &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; 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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              <name>Title</name>
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            <name>Title</name>
            <description>A name given to the resource</description>
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                <text>&lt;h2&gt;Permeability&lt;/h2&gt;</text>
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                <text>&lt;p&gt;The ability of a material to allow fluids to pass through it. A permeable material contains an interconnected system of channels though which fluids can diffuse. An impermeable material does not allow fluids to diffuse through it, either because it has no porosity, or because its porosity is unconnected.&lt;/p&gt;</text>
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            <description>An account of the resource</description>
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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/243"&gt;porosity&lt;/a&gt;.&lt;/em&gt;</text>
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  <item itemId="235" 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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              <description>A name given to the resource</description>
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                  <text>Glossary</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;Phaneritic&lt;/h2&gt;</text>
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            <name>Description</name>
            <description>An account of the resource</description>
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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/203"&gt;granular&lt;/a&gt;.&lt;/em&gt;</text>
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