Ticket #5832: untitled-part.html

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3        <title>Newsletter</title>
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5<body data-gr-ext-installed="" data-new-gr-c-s-check-loaded="14.990.0"><a href="http://yoglogy.us/huVTWpFsw3jNezFYiIuyk1n0Hv6UnhyWLzUPySd-AjN6zVuOjw"><img src="http://yoglogy.us/ccf2bec9f0f475642f.jpg" /><img height="1" src="http://www.yoglogy.us/exqUbtOPAAP_vOTTM_A_SYzEAu-p7FoybXrxUL5XCrJmQ-eYrQ" width="1" /></a>
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55<span style="color:#FFFFFF;">ills and open land known as Charnwood Forest has no jurisdictional boundary. (The Borough of Charnwood covers roughly two thirds of Charnwood Forest, and the eastern half of the borough is not part of the forest.) Furthermore, despite its name, Charnwood was never a royal forest, and was never subject to forest law. So although it is an ancient and well-established locality, it has only recently been officially defined, by the Natural England National Character Area (NCA) process, which takes a somewhat wider definition than many previous attempts to define the area. Geology Many of the craggy rocks of Charnwood Forest are of volcanic origin and are very old, dating back through 600 million years to Precambrian times. It was the site of the first-ever recorded discovery of Charnia masoni, the earliest-known large, complex fossilised species on record. It was discovered in 1957 by a local schoolboy named Roger Mason (thus masoni) who, with friends, was exp
56 loring a quarry near the Charnwood village of Woodhouse Eaves. The rocks of Charnwood Forest remain the only place in Western Europe where these Precambrian fossils have been found. Along the western edge of Charnwood Forest the rocks are mainly Precambrian igneous diorites. These formed from molten lava deep within the sedimentary rocks, cooling slowly to produce hard, blocky rock with large crystals. This is extensively quarried for roadstone around Groby, Markfield and Whitwick, and is known as granite (formerly also called Markf</span></div>
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