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                  <text>The Bridges Collection was donated to the University of St Andrews by Mrs M Bridges of St Andrews. Several cultural periods of Cyprus are represented by the artefacts of the collection. The Bronze and Iron Ages are very well represented with a variety of terracotta polished ware bowls, jugs, and figurines. The Byzantine period is also represented through a good selection of Sgraffiato ware dishes.&lt;br /&gt;&lt;br /&gt;For more information please visit the &lt;a href="https://arts.st-andrews.ac.uk/bridges-collection/" target="_blank"&gt;St Andrews Arts Reasearch and Teaching Server (ARTS) project&lt;/a&gt; of 3D scanning the collection.</text>
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                <text>22000 years ago this whole area was covered by a thick layer of ice – as was most of Scotland and Ireland, all the way down to the North of England and Wales. The ice started melting 20,000 years ago but didn’t all disappear until about 11,500 years ago. There is lots of evidence showing this all around Fife and Scotland.&#13;
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                <text>DRUMLIN DIAGRAM:  A drumlin forms when a glacier deposits material, more at one end than the other, giving it a characteristic blunt end where the most material was deposited, and a sloping lee side behind. There are often lots of them found together, forming a “drumlin field”. These help us to understand how and where the glacier retreated. &#13;
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                <text>&#13;
 Moraines form when the glacier deposits material that it has been carrying. The material it deposits at the snout (end) form the terminal moraine. If material is deposited along the side of the glacier, this is called a lateral moraine. If the material is deposited from the middle of the glacier, this forms a medial moraine. They record exactly where the glacier was at a certain time, but are sometimes incomplete as they can be eroded by floods and wind over time. &#13;
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                <text>Brrrrrrrr – goodness, it was chilly in Tentsmiur 15000 years ago! Where you are standing right now used to be covered by an enormous glacier, which is like a massive frozen river. It used to cover all of Scotland and Ireland, and go all the way down to the top of England and Wales. It was at its biggest 21000 years ago, but started melting for good about 10000 years ago. It melted from the outside first, so the bit that was over the sea melted and then the ice that was on the land. It was all the ice that was on top of Scotland all that time ago that made the big valleys we see in the highlands today. I’m certainly glad I wasn’t around 15000 years ago – no trees! No nuts! And verrryyyyyy cooollllddddd!&#13;
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        <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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            <description>A name given to the resource</description>
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                <text>Squirrel Sea Level Audio</text>
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