<rdf:RDF xmlns:rdf="http://www.w3.org/1999/02/22-rdf-syntax-ns#" xmlns:dcterms="http://purl.org/dc/terms/">
<rdf:Description rdf:about="https://openvirtualworlds.org/omeka/items/show/1262">
    <dcterms:title><![CDATA[Pano 9.jpg]]></dcterms:title>
</rdf:Description><rdf:Description rdf:about="https://openvirtualworlds.org/omeka/items/show/1267">
    <dcterms:title><![CDATA[EG Lapithos Vrysi tou Barba Tomb]]></dcterms:title>
</rdf:Description><rdf:Description rdf:about="https://openvirtualworlds.org/omeka/items/show/1268">
    <dcterms:title><![CDATA[Lapithos Vrysi tou Barba Tomb Pic]]></dcterms:title>
</rdf:Description><rdf:Description rdf:about="https://openvirtualworlds.org/omeka/items/show/1269">
    <dcterms:title><![CDATA[Lapithos MAP]]></dcterms:title>
</rdf:Description><rdf:Description rdf:about="https://openvirtualworlds.org/omeka/items/show/1270">
    <dcterms:title><![CDATA[Iceland Photosphere]]></dcterms:title>
    <dcterms:subject><![CDATA[Glacier Story]]></dcterms:subject>
    <dcterms:description><![CDATA[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.<br />
]]></dcterms:description>
</rdf:Description><rdf:Description rdf:about="https://openvirtualworlds.org/omeka/items/show/1271">
    <dcterms:title><![CDATA[Drumlin diagram]]></dcterms:title>
    <dcterms:subject><![CDATA[Glaciation]]></dcterms:subject>
    <dcterms:description><![CDATA[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. <br />
]]></dcterms:description>
</rdf:Description><rdf:Description rdf:about="https://openvirtualworlds.org/omeka/items/show/1272">
    <dcterms:title><![CDATA[Moraine]]></dcterms:title>
    <dcterms:subject><![CDATA[Glaciation]]></dcterms:subject>
    <dcterms:description><![CDATA[<br />
 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. <br />
]]></dcterms:description>
</rdf:Description><rdf:Description rdf:about="https://openvirtualworlds.org/omeka/items/show/1273">
    <dcterms:title><![CDATA[Squirrel Glacier Audio]]></dcterms:title>
    <dcterms:subject><![CDATA[Glacier Story]]></dcterms:subject>
    <dcterms:description><![CDATA[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!<br />
 ]]></dcterms:description>
</rdf:Description><rdf:Description rdf:about="https://openvirtualworlds.org/omeka/items/show/1274">
    <dcterms:title><![CDATA[Evidence for raised beaches]]></dcterms:title>
    <dcterms:subject><![CDATA[Sea Level Change]]></dcterms:subject>
    <dcterms:source><![CDATA[Source: Ritchie, W. 1978. Beaches of Fife. Commissioned by Countryside Commission for Scotland. (p12)<br />
<br />
]]></dcterms:source>
</rdf:Description><rdf:Description rdf:about="https://openvirtualworlds.org/omeka/items/show/1275">
    <dcterms:title><![CDATA[Lateral meltwater channels]]></dcterms:title>
    <dcterms:subject><![CDATA[Glaciation]]></dcterms:subject>
    <dcterms:description><![CDATA[This is a channel that runs alongside the edge of the glacier, draining away any water that has melted. It can sometimes be seen after glaciation, and helps us to understand how big the glacier was at different times.<br />
]]></dcterms:description>
</rdf:Description><rdf:Description rdf:about="https://openvirtualworlds.org/omeka/items/show/1276">
    <dcterms:title><![CDATA[Transition tool noise ]]></dcterms:title>
</rdf:Description><rdf:Description rdf:about="https://openvirtualworlds.org/omeka/items/show/1277">
    <dcterms:title><![CDATA[Squirrel Cartoon]]></dcterms:title>
</rdf:Description><rdf:Description rdf:about="https://openvirtualworlds.org/omeka/items/show/1278">
    <dcterms:title><![CDATA[changing coastline map]]></dcterms:title>
    <dcterms:subject><![CDATA[Sea level change]]></dcterms:subject>
</rdf:Description><rdf:Description rdf:about="https://openvirtualworlds.org/omeka/items/show/1279">
    <dcterms:title><![CDATA[Explanation: evidence of raised beaches map]]></dcterms:title>
    <dcterms:subject><![CDATA[Sea level change]]></dcterms:subject>
    <dcterms:description><![CDATA[This map shows the raised beaches which have been identified behind Tentsmuir, reflecting the fact that the beach used to much further inland compared to its present point. These beaches were identified due to their long flat shape, and due to the sediments that were found on them. <br />
<br />
<br />
]]></dcterms:description>
</rdf:Description><rdf:Description rdf:about="https://openvirtualworlds.org/omeka/items/show/1280">
    <dcterms:title><![CDATA[Lateral Meltwater Channels Fife]]></dcterms:title>
</rdf:Description><rdf:Description rdf:about="https://openvirtualworlds.org/omeka/items/show/1281">
    <dcterms:title><![CDATA[Explanation: evidence of sea level change map]]></dcterms:title>
    <dcterms:subject><![CDATA[Sea level change]]></dcterms:subject>
    <dcterms:description><![CDATA[The above map shows how coastal processes are continually changing the coast line of Tentsmuir. Tentsmuir’s location at the bottom of the Tay estuary means it receives huge quantities of sand each year. When the sediment is deposited, it slowly accumulates and causes the beach to grow. The map also highlights that not all of the beach has been growing - some parts have been eroded more rapidly. The combination of waves, wind and tides eroding and depositing sediment cause Tentsmuir’s coast to change rapidly and unevenly over time. <br />
]]></dcterms:description>
</rdf:Description><rdf:Description rdf:about="https://openvirtualworlds.org/omeka/items/show/1282">
    <dcterms:title><![CDATA[Squirrel Mesolithic Interview]]></dcterms:title>
</rdf:Description><rdf:Description rdf:about="https://openvirtualworlds.org/omeka/items/show/1283">
    <dcterms:title><![CDATA[Squirrel Tsunami Interview]]></dcterms:title>
</rdf:Description><rdf:Description rdf:about="https://openvirtualworlds.org/omeka/items/show/1284">
    <dcterms:title><![CDATA[Squirrel Neolithic Interview]]></dcterms:title>
</rdf:Description><rdf:Description rdf:about="https://openvirtualworlds.org/omeka/items/show/1285">
    <dcterms:title><![CDATA[Squirrel Sea Level Audio]]></dcterms:title>
</rdf:Description></rdf:RDF>
