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  <title><![CDATA[1A Collections]]></title>
  <subtitle><![CDATA[Rocks, minerals and fossils collections for Part 1A students]]></subtitle>
  <author>
    <name><![CDATA[Department of Earth Sciences]]></name>
  </author>
  <updated>2024-04-09T21:16:02+01:00</updated>
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    <id>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/25</id>
    <title><![CDATA[<h2><strong>L326<br /></strong></h2>
<h2>Sandstone, ferruginous arenite</h2>]]></title>
    <summary><![CDATA[<div class="element">
<div class="element">
<h3>Hand Specimen</h3>
<div class="element-text">Reddish brown rock. Medium sand grade.<br />Round to sub-round grains of quartz, often with a thin rim of red hematite. Mainly reddish and pink-brown grains, fewer white grains and very few black grains. Well sorted and well cemented.<br />No fizzing with acid, so does not contain significant carbonate.<span> </span><br /><br />Laminations can be observed in sample L326b. There is an inter-layering of coarser and finer laminae.</div>
</div>
<div class="element">
<h3>Thin-section</h3>
<div class="element-text">
<p>Fine laminations can be seen when the thin-section is held up to the light.<span> </span><br />Moderately well rounded quartz grains with thin rims of hematite, and overgrowths of quartz in optical continuity with the original grain.<span> </span><br />Occasional grains of very fine quartzite, microcline, plagioclase, mica and decomposed fine-grained igneous rocks.<span> </span><br />Siliceous cement and the secondary quartz<span> </span><a href="/p1acollections/items/show/232">overgrowths</a><span> </span>hold this rock together.</p>
<p>The grains are finer as a whole in L326b, and less well rounded.</p>
</div>
</div>
<div class="element">
<h3>Rock History</h3>
<div class="element-text">
<p>Probably deposited in an<span> </span><a href="/p1acollections/items/show/167">aeolian</a><span> </span>environment, since it almost entirely comprises well sorted and well rounded quartz grains.</p>
</div>
</div>
<div class="element"></div>
<div class="element"></div>
<div class="element">
<h3>Rock Name</h3>
<div class="element-text">ferruginous sandstone<br />ferruginous arenite</div>
</div>
</div>]]></summary>
    <updated>2019-07-04T09:52:08+01:00</updated>
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    <category term="lamination"/>
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        <h3>Title</h3>
                    <div class="element-text"><h2><strong>L326<br /></strong></h2>
<h2>Sandstone, ferruginous arenite</h2></div>
            </div><!-- end element -->
        <div id="dublin-core-subject" class="element">
        <h3>Subject</h3>
                    <div class="element-text"><h3>Specimen Age</h3>
<div class="element-text">Permian<br /><h3>Location</h3>
<div class="element-text">Penrith Sandstone<br />Appleby, Westmorland</div>
</div></div>
            </div><!-- end element -->
        <div id="dublin-core-description" class="element">
        <h3>Description</h3>
                    <div class="element-text"><div class="element">
<div class="element">
<h3>Hand Specimen</h3>
<div class="element-text">Reddish brown rock. Medium sand grade.<br />Round to sub-round grains of quartz, often with a thin rim of red hematite. Mainly reddish and pink-brown grains, fewer white grains and very few black grains. Well sorted and well cemented.<br />No fizzing with acid, so does not contain significant carbonate.<span> </span><br /><br />Laminations can be observed in sample L326b. There is an inter-layering of coarser and finer laminae.</div>
</div>
<div class="element">
<h3>Thin-section</h3>
<div class="element-text">
<p>Fine laminations can be seen when the thin-section is held up to the light.<span> </span><br />Moderately well rounded quartz grains with thin rims of hematite, and overgrowths of quartz in optical continuity with the original grain.<span> </span><br />Occasional grains of very fine quartzite, microcline, plagioclase, mica and decomposed fine-grained igneous rocks.<span> </span><br />Siliceous cement and the secondary quartz<span> </span><a href="/p1acollections/items/show/232">overgrowths</a><span> </span>hold this rock together.</p>
<p>The grains are finer as a whole in L326b, and less well rounded.</p>
</div>
</div>
<div class="element">
<h3>Rock History</h3>
<div class="element-text">
<p>Probably deposited in an<span> </span><a href="/p1acollections/items/show/167">aeolian</a><span> </span>environment, since it almost entirely comprises well sorted and well rounded quartz grains.</p>
</div>
</div>
<div class="element"></div>
<div class="element"></div>
<div class="element">
<h3>Rock Name</h3>
<div class="element-text">ferruginous sandstone<br />ferruginous arenite</div>
</div>
</div></div>
            </div><!-- end element -->
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