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            <name>Title</name>
            <description>A name given to the resource</description>
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                <text>&lt;h2&gt;&lt;strong&gt;L310&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Breccia&lt;/h2&gt;</text>
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            <name>Subject</name>
            <description>The topic of the resource</description>
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                <text>&lt;h3&gt;Specimen Age&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;Permian&lt;/p&gt;
&lt;h3&gt;Location&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;Brockram, Cumbria&lt;/p&gt;
&lt;/div&gt;
&lt;/div&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-set"&gt;
&lt;div class="element"&gt;
&lt;div class="element-text"&gt;
&lt;h3&gt;Hand Specimen&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;
&lt;p&gt;Very poorly sorted.Angular to sub-angular clasts up to 30 mm long. Randomly orientated.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Clasts mainly pale grey, some white, some red.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Red-brown colour of the fine-grained matrix indicates&lt;span&gt; &lt;/span&gt;&lt;span&gt;iron staining&lt;/span&gt;.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Matrix and some clasts fizz with acid, indicating that they are made of carbonate. This is a limestone.&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;Variety of clasts: sedimentary rock fragments, carbonate and feldspar crystals, fine-grained quartz and carbonate, some bioclasts. Clasts are quite angular.&lt;br /&gt;Matrix of very fine-grained clays containing fragments of quartz and carbonate.&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;Clast-supported. Clasts are angular, so sediments cannot have been transported far. (NB, if this rock were matrix supported the clasts could have been transported a long way without losing their angularity.)&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Probably scree accumulation during desert conditions, from approximately the same horizon as L326.&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;&lt;span&gt;Iron-staining&lt;/span&gt;&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Hematite (Fe&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;3&lt;/sub&gt;) → red (blood-red, cherry-red, brown-red) iron-staining&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Limonite (FeO(OH)•nH&lt;sub&gt;2&lt;/sub&gt;O) → yellow or brown iron-staining&lt;/p&gt;
&lt;p&gt;The red-brown colour of this rock is probably produced by hematite.&lt;/p&gt;
&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;breccia&lt;/div&gt;
&lt;/div&gt;
&lt;/div&gt;</text>
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        <name>clastic</name>
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        <name>scree</name>
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            <name>Title</name>
            <description>A name given to the resource</description>
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                <text>&lt;h2&gt;&lt;strong&gt;L200&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Volcanic Breccia&lt;/h2&gt;</text>
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            <name>Subject</name>
            <description>The topic of the resource</description>
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                <text>&lt;h3&gt;Age&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;Carboniferous&lt;/p&gt;
&lt;h3&gt;Location&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;Melrose, Scotland&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;</text>
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            <name>Description</name>
            <description>An account of the resource</description>
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              <elementText elementTextId="54">
                <text>&lt;div class="element-set"&gt;
&lt;div class="element"&gt;
&lt;div class="element-text"&gt;
&lt;h3&gt;Hand Specimen&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;
&lt;p&gt;Sedimentary textures, very poorly sorted.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Sub-round to angular grains up to 20mm across.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Wide variety of clasts: dark purple, cream, rusty orange, grey, several types of lava.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Some black, shiny igneous crystals.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Brown-grey matrix of&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;/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;Wide range of clasts including&lt;br /&gt;- Basalt&lt;br /&gt;- Slate or phyllite&lt;br /&gt;- Schist&lt;br /&gt;- Chert&lt;br /&gt;- Sandstone&lt;br /&gt;- Carbonate&lt;br /&gt;- Quartz&lt;br /&gt;&lt;br /&gt;Matrix of fine volcanic ash.&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;This is an example of the coarser type of material deposited by explosive volcanic action.&lt;br /&gt;&lt;br /&gt;NB,&lt;br /&gt;This is not a typical volcanic breccia, as one usually sees a greater abundance of igneous clasts; other clasts could be wall-rock. Another name for this rock could be “lithic wacke”.&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;volcanic breccia&lt;br /&gt;lithic wacke&lt;/div&gt;
&lt;/div&gt;
&lt;/div&gt;</text>
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        <name>clastic</name>
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        <name>extrusive</name>
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        <name>lithic</name>
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