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      <description>An inanimate, three-dimensional object or substance. Note that digital representations of, or surrogates for, these objects should use Moving Image, Still Image, Text or one of the other types.</description>
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                <text>&lt;h2&gt;Chlorite&lt;/h2&gt;</text>
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            <name>Subject</name>
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                <text>&lt;span&gt;Chlorite is a common high-temperature alteration product of ferromagnesian minerals (such as biotite) in igneous rocks. It is stable in the upper part of the crust and is a major constituent of the metamorphic rocks known as greenschists.&lt;/span&gt;</text>
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                <text>&lt;div class="element-set"&gt;
&lt;div class="element"&gt;
&lt;div class="element-text"&gt;
&lt;h3 class="NoSpacing"&gt;Formula&lt;/h3&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element-set"&gt;
&lt;div class="element"&gt;
&lt;div class="element-text"&gt;(Mg,Fe&lt;sup&gt;2+&lt;/sup&gt;,Fe&lt;sup&gt;3+&lt;/sup&gt;,Mn,Al)&lt;sub&gt;12&lt;/sub&gt;[(Si,Al)&lt;sub&gt;8&lt;/sub&gt;O&lt;sub&gt;20&lt;/sub&gt;](OH)&lt;sub&gt;16&lt;/sub&gt;&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Structure&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;Sheet silicate&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Crystal System&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;&lt;em&gt;Crystal system:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;monoclinic (+) (-)&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Physical Properties&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p class="NoSpacing"&gt;&lt;em&gt;&lt;span&gt;Colour in hand specimen:&lt;/span&gt;&lt;/em&gt;&lt;span&gt; green&lt;/span&gt;&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;&lt;em&gt;&lt;span&gt;Cleavage:&lt;/span&gt;&lt;/em&gt;&lt;span&gt; one, good&lt;/span&gt;&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;&lt;em&gt;&lt;span&gt;Hardness:&lt;/span&gt;&lt;/em&gt;&lt;span&gt; 2-3&lt;/span&gt;&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Optical Properties&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p class="NoSpacing"&gt;&lt;em&gt;Colour in plane polarised light:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;colourless or green&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;&lt;em&gt;Pleochroism:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;weak to moderate&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;&lt;em&gt;Relief:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;low&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;&lt;em&gt;Birefringence:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;anomalous (blue or brown colours that do not appear in the Michel-Levy chart)&lt;span&gt; &lt;/span&gt;&lt;br /&gt;&lt;em&gt;Extinction:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;straight&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Rock Specimens&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;&lt;a href="/p1acollections/exhibits/show/igneous-rocks/l100"&gt;L100 Alkali granite&lt;/a&gt;&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;&lt;a href="/p1acollections/exhibits/show/igneous-rocks/l101"&gt;L101 Granite&lt;/a&gt;&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;&lt;a href="/p1acollections/exhibits/show/igneous-rocks/l120"&gt;L120 Granodiorite&lt;/a&gt;&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;&lt;a href="/p1acollections/exhibits/show/igneous-rocks/l130"&gt;L130 Andesite, porphyritic (porphyrite)&lt;/a&gt;&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;&lt;a href="/p1acollections/exhibits/show/igneous-rocks/l161"&gt;L161 Basalt, amygdaloidal&lt;/a&gt;&lt;span&gt; &lt;/span&gt;&lt;br /&gt;&lt;a href="/p1acollections/exhibits/show/volcaniclastic-rocks/l201"&gt;L201 Tuff&lt;/a&gt;&lt;span&gt; &lt;/span&gt;&lt;br /&gt;&lt;a href="/p1acollections/exhibits/show/metamorphic-rocks/l504"&gt;L504 Garnet schist&lt;/a&gt;&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Mineral Name&lt;/h3&gt;
&lt;div class="element-text"&gt;chlorite&lt;/div&gt;
&lt;/div&gt;
&lt;/div&gt;</text>
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        <name>alteration</name>
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        <name>metamorphism</name>
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            <name>Title</name>
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                <text>&lt;h2&gt;Garnet&lt;/h2&gt;</text>
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            <description>An account of the resource</description>
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                <text>&lt;div class="element"&gt;
&lt;h3&gt;Formula&lt;/h3&gt;
&lt;div class="element-text"&gt;(Mg,Fe,Ca)&lt;sub&gt;3&lt;/sub&gt;Al&lt;sub&gt;2&lt;/sub&gt;Si&lt;sub&gt;3&lt;/sub&gt;O&lt;sub&gt;12&lt;/sub&gt;&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Structure&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;Orthosilicate&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Crystal System&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;&lt;em&gt;Crystal system:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;cubic&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Physical Properties&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;&lt;em&gt;Colour in hand specimen:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;typically red&lt;br /&gt;&lt;em&gt;Cleavage:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;none&lt;br /&gt;&lt;em&gt;Hardness:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;6-7.5&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Optical Properties&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;&lt;em&gt;Colour in plane polarised light:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;colourless, pale pink&lt;span&gt; &lt;/span&gt;&lt;br /&gt;&lt;em&gt;Pleochroism:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;none&lt;br /&gt;&lt;em&gt;Relief:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;high&lt;br /&gt;Isotropic&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Mineral Specimens&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;&lt;span&gt;&lt;strong&gt;M130 Garnet schist&lt;/strong&gt;&lt;/span&gt;&lt;br /&gt;&lt;strong&gt;Portsoy, Banffshire&lt;/strong&gt;&lt;br /&gt;Euhedral porphyroblasts of dark-red garnet, with quartz, mica and other minerals in a medium-grade metamorphic rock.&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Rock Specimens&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;&lt;a href="/p1acollections/exhibits/show/metamorphic-rocks/l504"&gt;L504 Garnet schist&lt;/a&gt;&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Advanced Notes&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;The garnet group encompasses a wide range of compositions, and consequently a range of optical and physical properties. The properties detailed above are typical of pyrope (Mg&lt;sub&gt;3&lt;/sub&gt;Al&lt;sub&gt;2&lt;/sub&gt;Si&lt;sub&gt;3&lt;/sub&gt;O&lt;sub&gt;12&lt;/sub&gt;), almandine (Fe&lt;sup&gt;2+&lt;/sup&gt;&lt;sub&gt;3&lt;/sub&gt;Al&lt;sub&gt;2&lt;/sub&gt;Si&lt;sub&gt;3&lt;/sub&gt;O&lt;sub&gt;12&lt;/sub&gt;) and grossular (Ca&lt;sub&gt;3&lt;/sub&gt;Al&lt;sub&gt;2&lt;/sub&gt;Si&lt;sub&gt;3&lt;/sub&gt;O&lt;sub&gt;12&lt;/sub&gt;).&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Mineral Name&lt;/h3&gt;
&lt;div class="element-text"&gt;garnet&lt;/div&gt;
&lt;/div&gt;</text>
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        <name>metamorphism</name>
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        <name>metapelite</name>
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                <text>&lt;h2&gt;&lt;strong&gt;L201&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Tuff&lt;/h2&gt;</text>
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            <name>Description</name>
            <description>An account of the resource</description>
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                <text>&lt;div class="element"&gt;
&lt;h3&gt;Hand Specimen&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;Fine-grained, blue-green, sedimentary texture.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Slaty&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/180"&gt;cleavage&lt;/a&gt;.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Some patches of lighter and finer-grained material.&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Thin-section&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;Slaty cleavage due to the alignment of chlorite and muscovite.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Cross-cut by the blobs of the fine-grained material. These are orange-brown in thin-section. Could be water-lain ash, ripped-up to form clasts.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Very fine-grained, brown matrix, probably&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/266"&gt;volcanic&lt;/a&gt;&lt;span&gt; &lt;/span&gt;ash.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Carbonate, quartz and opaque clasts slightly larger than the matrix.&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Rock History&lt;/h3&gt;
&lt;div class="element-text"&gt;Fine-grained volcanic ash deposited by an explosive volcanic eruption has undergone low grade metamorphism to produce a slaty cleavage.&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;&lt;/div&gt;
&lt;div class="element"&gt;&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Rock Name&lt;/h3&gt;
&lt;div class="element-text"&gt;tuff&lt;/div&gt;
&lt;/div&gt;</text>
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        <name>cleavage</name>
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        <name>slaty</name>
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