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                <text>&lt;h2&gt;&lt;strong&gt;L350&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Limestone, argillaceous&lt;/h2&gt;</text>
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            <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;Jurassic&lt;/p&gt;
&lt;h3&gt;Location&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;Purbeck&lt;br /&gt;Near Salisbury&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;</text>
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&lt;h3&gt;Hand Specimen&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;Pale yellow-grey mudstone containing the fossil remains of a&lt;span&gt; &lt;/span&gt;&lt;span&gt;small arthropod with a segmented exoskeleton.&lt;/span&gt;&lt;span&gt; &lt;/span&gt;&lt;br /&gt;The rock is banded and shows some surface discolouration due to weathering.&lt;br /&gt;Rock fizzes with acid, so contains carbonate.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;This is a soft, though well consolidated limestone (the surface has been scratched).&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;Moving across the slide, perpendicular to the laminations, there are alternations (gradual transitions) between calcareous mudstone and&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/176"&gt;argillaceous&lt;/a&gt;&lt;span&gt; &lt;/span&gt;limestone. One band is rich in angular quartz grains (0.1 to 0.2 mm), and contains carbonate shell fragments.&lt;/p&gt;
&lt;p&gt;Calcite mudstone – fine-grained mosaic of calcite, small proportion of transparent brown impurity and a few small grains of quartz.&lt;/p&gt;
&lt;p&gt;Argillaceous limestone – even finer grained calcite mosaic, more abundant brown material (probably organic) than in the calcite mudstone.&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;Low energy, aqueous environment.&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;The fossil remains are those of Archaeoniscus, a small crustacean (which belongs to the arthropods), of supposed freshwater origin. With this extra knowledge it may be inferred that the rock was deposited in fresh water.&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;argillaceous limestone&lt;/div&gt;
&lt;/div&gt;</text>
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                <text>&lt;h2&gt;&lt;strong&gt;L327&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Sandstone, ferruginous&lt;/h2&gt;</text>
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                <text>&lt;h3&gt;Age&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;Cretaceous&lt;/p&gt;
&lt;h3&gt;Location&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;Carston, Lower Greensand&lt;br /&gt;Hunstanton&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;</text>
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                <text>&lt;div class="element"&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Hand Specimen&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;Mainly medium sand (to coarse sand in the case of L327a).&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Yellow-brown&lt;span&gt; &lt;/span&gt;&lt;span&gt;iron stained&lt;/span&gt;&lt;span&gt; &lt;/span&gt;quartz, cemented by the same yellow brown oxide. A few larger quartz grains up to 5 mm long. Grains are angular to sub-rounded, and poorly sorted.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Fizzing with acid, indicating that there is a carbonate cement.&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;Angular to sub-angular grains of quartz, displaying&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/263"&gt;undulose extinction&lt;/a&gt;.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Most have thin brown rims of iron oxide.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;A few grains of feldspar.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Minor carbonate cement (sparite).&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;
&lt;p&gt;Deposited in an aqueous environment, since it is not clean enough to be&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/167"&gt;aeolian&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;&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 yellow colour of this rock is probably produced by limonite.&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;ferruginous sandstone&lt;/div&gt;
&lt;/div&gt;
&lt;/div&gt;</text>
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            <name>Title</name>
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                <text>&lt;h2&gt;&lt;strong&gt;L325&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Sandstone, calcareous cement&lt;/h2&gt;</text>
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&lt;div class="element"&gt;
&lt;div class="element-text"&gt;
&lt;h3&gt;Age&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;Jurassic&lt;br /&gt;&lt;br /&gt;&lt;div class="element-set"&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Location&lt;/h3&gt;
&lt;div class="element-text"&gt;Portland Group, Shotover Hill, Oxford&lt;/div&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;/div&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;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;Pale grey rock, mainly medium to coarse grained quartz sand. Poorly sorted.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Small amounts of lithic fragments up to 10 mm across, and shell fragments.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Contains &amp;lt;15 vol% clay, making it an arenite.&lt;br /&gt;Pale grey cement fizzes with acid, indicating that it is carbonate.&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;Quartz grains, sub-angular to sub-rounded, occasionally rounded, displaying&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/263"&gt;undulose extinction&lt;/a&gt;.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Lithic fragments including flint and quartzite.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Some grains of feldspar.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Rare small&lt;span&gt; &lt;/span&gt;&lt;span&gt;green clasts&lt;/span&gt;.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Grain supported.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Cemented by a sparry calcite cement. The cement crystals are large, each enclosing a number of sedimentary grains.&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;
&lt;p&gt;Deposited in an aqueous environment; grains are not rounded enough to have been deposited in an&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/167"&gt;aeolian&lt;/a&gt;&lt;span&gt; &lt;/span&gt;environment.&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 rare&lt;span&gt; &lt;/span&gt;&lt;span&gt;green clasts&lt;/span&gt;&lt;span&gt; &lt;/span&gt;are made up of a&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/184"&gt;cryptocrystalline&lt;/a&gt;&lt;span&gt; &lt;/span&gt;material, which may be a type of amphibole called glauconite, and some rather decomposed rhyolite or andesite.&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;Calcareous sandstone&lt;br /&gt;Calcareous arenite&lt;/div&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;/div&gt;</text>
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                <text>&lt;h2&gt;&lt;strong&gt;L324&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Sandstone, feldspathic arenite&lt;/h2&gt;</text>
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                <text>&lt;h3&gt;Age&lt;/h3&gt;
&lt;div class="element-text"&gt;Precambrian&lt;br /&gt;&lt;h3&gt;Location&lt;/h3&gt;
&lt;div class="element-text"&gt;Torridonian Group, North West Scotland&lt;/div&gt;
&lt;/div&gt;</text>
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&lt;div class="element"&gt;
&lt;div class="element-text"&gt;
&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;
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&lt;div class="element-set"&gt;
&lt;div class="element"&gt;
&lt;div class="element-text"&gt;Reddish brown rock made up of pinkish feldspar, colourless quartz, and some dark grey grains. Medium to coarse sand. Moderately rounded. Fairly well sorted.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Contains &amp;lt;15 vol% clay, so this is an arenite.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;No fizzing with acid, so does not contain significant carbonate.&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;Quartz (~65%)&lt;span&gt; &lt;/span&gt;&lt;br /&gt;- Includes fresh quartz grains with&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/263"&gt;undulose extinction&lt;/a&gt;, quartzite grains with internal&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/257"&gt;sutures&lt;/a&gt;, and quartz vein material. Some quartz grains have opaque rims.&lt;/p&gt;
&lt;p&gt;Feldspar (~35%)&lt;span&gt; &lt;/span&gt;&lt;br /&gt;- Mainly microcline, some plagioclase. Some&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/228"&gt;microperthite texture&lt;/a&gt;&lt;span&gt; &lt;/span&gt;and decomposition to clays.&lt;/p&gt;
&lt;p&gt;All grains are moderately rounded and fairly well sorted. The rock is well compacted. A thin film of cement mainly hematite and clay coats the grains.&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;
&lt;p&gt;This rock contains too much feldspar, and the grains are not sufficiently well rounded nor well sorted to have been deposited in an&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/167"&gt;aeolian&lt;/a&gt;&lt;span&gt; &lt;/span&gt;environment. The sediments were deposited in an aqueous environment.&lt;br /&gt;&lt;br /&gt;&lt;br /&gt;&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Rock Name&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;sandstone&lt;br /&gt;feldspathic arenite&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;/div&gt;</text>
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        <name>aqueous</name>
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        <name>compacted</name>
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        <name>sorting</name>
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      <name>Physical Object</name>
      <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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        <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;&lt;strong&gt;L323&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Sandstone, arenite&lt;/h2&gt;</text>
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          <element elementId="49">
            <name>Subject</name>
            <description>The topic of the resource</description>
            <elementTextContainer>
              <elementText elementTextId="72">
                <text>&lt;h3&gt;Age&lt;/h3&gt;
&lt;div class="element-text"&gt;Jurassic&lt;br /&gt;&lt;br /&gt;&lt;h3&gt;Location&lt;/h3&gt;
&lt;div class="element-text"&gt;Estuarine Series, North Yorkshire&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;Pale yellow grey rock, almost entirely made up of medium sand quartz grains. These are sub-rounded, very well sorted, and are held together by a matrix of siliceous silt. Contains a significant amount of clay, but &amp;lt;15 vol%, so it is an arenite.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;No fizzing with acid, so does not contain significant carbonate.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Weakly laminated.&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;Sub-round grains of quartz, some opaque grains and a few flakes of white mica.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Siliceous, silty matrix.&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;
&lt;p&gt;This rock was deposited in a moderate energy, aqueous environment. The grains are not well rounded enough to be&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/167"&gt;aeolian&lt;/a&gt;&lt;span&gt; &lt;/span&gt;sediments.&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Rock Name&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;sandstone&lt;br /&gt;arenite&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;/div&gt;</text>
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        <name>aqueous</name>
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        <name>sorting</name>
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