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  <title>Abberley &amp; Malvern Hills Geopark</title>
  <link>http://www.geopark.org.uk/blog</link>
  <description>The Abberley and Malvern Hills Geopark covers 1250 square kilometres in Gloucestershire, Herefordshire, Shropshire and Worcestershire in the UK. Here you will find outstanding geology that spans 700 million years of our Earth&#39;s history, dramatic landscapes and a wealth of ecological, historical, and cultural gems. We seek to celebrate our geological heritage, promote excellence in geoconservation and also achieve sustainable development through geotourism.</description>
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  <lastBuildDate>Mon, 26 Jul 2010 19:07:17 +0100</lastBuildDate>
  <category domain="http://www.geopark.org.uk/blog/Geology/AreaGeology">Area Geology</category>
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  <item>
    <dc:creator>astinton</dc:creator>
    <title>Geology of the Geopark</title>
    <link>http://www.geopark.org.uk/blog/_archives/2009/7/3/4243566.html</link>
    <guid>http://www.geopark.org.uk/blog/_archives/2009/7/3/4243566.html</guid>
    <pubDate>Fri, 03 Jul 2009 10:07:00 +0100</pubDate>
    <description>&lt;p align=&quot;justify&quot;&gt;The geology of the Geopark varies considerably. Within the Geopark, there are several areas that are notable for their geology and landscape. The articles below reveal more about these features in a number of different areas, starting with the Abberely Hills.&lt;/p&gt;</description>
    
    <category domain="http://www.geopark.org.uk/blog/Geology/AreaGeology">Area Geology</category>
    
    
    
    
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  <item>
    <dc:creator>astinton</dc:creator>
    <title>The Abberley Hills</title>
    <link>http://www.geopark.org.uk/blog/_archives/2009/7/12/4252627.html</link>
    <guid>http://www.geopark.org.uk/blog/_archives/2009/7/12/4252627.html</guid>
    <pubDate>Sun, 12 Jul 2009 16:18:00 +0100</pubDate>
    <description>&lt;p align=&quot;justify&quot;&gt;The Abberley Hills are comprised of eight hills. These are Walsgrove hill, Cockshot Hill, Rodge Hill, Pudford Hill, Penny Hill, Berrow Hill and Ankerdine Hill. Along with the Malvern Hills, there are the most importnat landscape features of the geopark.&lt;/p&gt;</description>
    
    <category domain="http://www.geopark.org.uk/blog/Geology/AreaGeology">Area Geology</category>
    
    
    
    
  </item>
  
  <item>
    <dc:creator>astinton</dc:creator>
    <title>The Malvern Hills</title>
    <link>http://www.geopark.org.uk/blog/_archives/2009/7/12/4252612.html</link>
    <guid>http://www.geopark.org.uk/blog/_archives/2009/7/12/4252612.html</guid>
    <pubDate>Sun, 12 Jul 2009 16:12:00 +0100</pubDate>
    <description>&lt;p align=&quot;justify&quot;&gt; The Malvern Hills form a north-south range about 14km (9 miles) long. They are probably the most recognisable landscape feature in the geopark. Click more to read about their geological history.&lt;/p&gt;</description>
    
    <category domain="http://www.geopark.org.uk/blog/Geology/AreaGeology">Area Geology</category>
    
    
    
    
  </item>
  
  <item>
    <dc:creator>astinton</dc:creator>
    <title>The Bridgnorth Area</title>
    <link>http://www.geopark.org.uk/blog/_archives/2009/7/11/4251714.html</link>
    <guid>http://www.geopark.org.uk/blog/_archives/2009/7/11/4251714.html</guid>
    <pubDate>Sat, 11 Jul 2009 17:07:00 +0100</pubDate>
    <description>&lt;p align=&quot;justify&quot;&gt;The Bridgnorth area is underlain by Permian Bridgnorth Sandstone. These rocks represent fossilised sand dunes and were part of a vast desert that existed around 299 million years ago.&lt;/p&gt;</description>
    
    <category domain="http://www.geopark.org.uk/blog/Geology/AreaGeology">Area Geology</category>
    
    
    
    
  </item>
  
  <item>
    <dc:creator>astinton</dc:creator>
    <title>The Teme Valley</title>
    <link>http://www.geopark.org.uk/blog/_archives/2009/7/11/4251583.html</link>
    <guid>http://www.geopark.org.uk/blog/_archives/2009/7/11/4251583.html</guid>
    <pubDate>Sat, 11 Jul 2009 16:02:00 +0100</pubDate>
    <description>&lt;p align=Justify&quot;&gt;The River Teme is one of the larger tributaries of the River Severn in the Geopark. The area is generally underlain by Old Red Sandstone mudstones, but also contains some unique recent tufa deposits.&lt;/p&gt;</description>
    
    <category domain="http://www.geopark.org.uk/blog/Geology/AreaGeology">Area Geology</category>
    
    
    
    
  </item>
  
  <item>
    <dc:creator>astinton</dc:creator>
    <title>The Severn Vale</title>
    <link>http://www.geopark.org.uk/blog/_archives/2009/7/11/4251563.html</link>
    <guid>http://www.geopark.org.uk/blog/_archives/2009/7/11/4251563.html</guid>
    <pubDate>Sat, 11 Jul 2009 15:46:00 +0100</pubDate>
    <description>&lt;p align=&quot;justify&quot;&gt;The River Severn marks the eastern boundary of the Geopark and dominated the geology and landscape of Worcestershire. The majority of the vale is underlain by mudstones from the Permian. Click more to find out more.&lt;/p&gt;</description>
    
    <category domain="http://www.geopark.org.uk/blog/Geology/AreaGeology">Area Geology</category>
    
    
    
    
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  <item>
    <dc:creator>astinton</dc:creator>
    <title>The Frome Valley</title>
    <link>http://www.geopark.org.uk/blog/_archives/2009/7/11/4251554.html</link>
    <guid>http://www.geopark.org.uk/blog/_archives/2009/7/11/4251554.html</guid>
    <pubDate>Sat, 11 Jul 2009 15:30:00 +0100</pubDate>
    <description>&lt;p align=&quot;justify&quot;&gt;The geology of the Frome Valley, between bromyard and Castle Frome, is dominated by the Old Red Sandstone. Click more to read on.&lt;/p&gt;</description>
    
    <category domain="http://www.geopark.org.uk/blog/Geology/AreaGeology">Area Geology</category>
    
    
    
    
  </item>
  
  <item>
    <dc:creator>astinton</dc:creator>
    <title>May Hill</title>
    <link>http://www.geopark.org.uk/blog/_archives/2009/7/11/4251541.html</link>
    <guid>http://www.geopark.org.uk/blog/_archives/2009/7/11/4251541.html</guid>
    <pubDate>Sat, 11 Jul 2009 15:17:00 +0100</pubDate>
    <description>&lt;p align=justify&quot;&gt;May Hill is the southern most expression of the Malvern Hills complex and occupies an area of around seven square miles on the border of Gloucestershire and Herefordshire.&lt;/p&gt;</description>
    
    <category domain="http://www.geopark.org.uk/blog/Geology/AreaGeology">Area Geology</category>
    
    
    
    
  </item>
  
  <item>
    <dc:creator>astinton</dc:creator>
    <title>Huntley Quarry, Gloucestershire</title>
    <link>http://www.geopark.org.uk/blog/_archives/2009/7/11/4251536.html</link>
    <guid>http://www.geopark.org.uk/blog/_archives/2009/7/11/4251536.html</guid>
    <pubDate>Sat, 11 Jul 2009 15:07:00 +0100</pubDate>
    <description>&lt;p align=&quot;justify&quot;&gt;The Huntley Quarry Geology Reserve was officially opened in 2007, and is the first geology reserve in Gloucestershire. The reserve, and its surrounding woodland, cover an area of 0.87 hectares and is owned and managed by Gloucestershire Geology Trust. Three quarries, as well as the &lt;a href=&quot;http://www.glosgeotrust.org.uk/images/bluebells.jpg&quot;&gt;bluebell&lt;/a&gt; and daffodil woodland can be visited at the reserve.&lt;/p&gt;</description>
    
    <category domain="http://www.geopark.org.uk/blog/Geology/AreaGeology">Area Geology</category>
    
    
    
    
  </item>
  
  <item>
    <dc:creator>astinton</dc:creator>
    <title>The Quaternary</title>
    <link>http://www.geopark.org.uk/blog/_archives/2009/7/3/4243583.html</link>
    <guid>http://www.geopark.org.uk/blog/_archives/2009/7/3/4243583.html</guid>
    <pubDate>Fri, 03 Jul 2009 10:23:00 +0100</pubDate>
    <description>&lt;p align=&quot;Justify&quot;&gt;The Quaternary contains the youngest rocks in the Geopark and was a time of fluctuating climate, varying from cold glacial periods to warm, integlacial periods.&lt;/p&gt;</description>
    
    <category domain="http://www.geopark.org.uk/blog/Geology/AreaGeology">Area Geology</category>
    
    
    
    
  </item>
  
  <item>
    <dc:creator>astinton</dc:creator>
    <title>Hydrology and Fluvial Geomorphology</title>
    <link>http://www.geopark.org.uk/blog/_archives/2009/7/3/4243579.html</link>
    <guid>http://www.geopark.org.uk/blog/_archives/2009/7/3/4243579.html</guid>
    <pubDate>Fri, 03 Jul 2009 10:19:00 +0100</pubDate>
    <description>&lt;p align=&quot;justify&quot;&gt; Water plays a key role in developing and shaping the physical landscape. The effects of surface erosion, water emerging from sub surface sources (i.e springs and seeps) and the development and movement of steams and river channels can create a rich and complex array of geomorphic features. &lt;/p&gt;</description>
    
    <category domain="http://www.geopark.org.uk/blog/Geology/AreaGeology">Area Geology</category>
    
    
    
    
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