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| Our own desert sandstone on the Fenwick's
arch |
Fenwick's Arch:
on your left on the corner of Market Street. Look at the Red stone stripes
in the arch. 230 million years ago it was a desert all around here. This
stone, called Triassic Desert Sandstone, was very probably quarried in the
East Midlands and would have been formed then.
Before the road junction: Welford House has Norwegian Larvakite (the polished
black stone).
At the road
junction: The statue of John Biggs shows you the difference between polished
Shap Granite (right under Mr Bigg's feet), and unpolished Shap Granite
(holding up the polished bit).
Outside Newarke
Street car park: The cobbles were made round by ice sheets and water thousands
of years of years ago. In the square outside Phoenix Arts, you will pass
pollution-busting plane trees which absorb fumes from cars and other human
activity and store these in their bark.
On your right,
De Montfort University's Crown Building: here you can feel the different
layers of sediments in the yellow Millstone Grit at the bottom of the
building, and see how they were laid down under the sea. Sometimes you
can see changes from flat layers to diagonal layers in the same stone.
The diagonal layers are called-cross bedding and were formed in ripples
on the sea floor.
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| Traffic from inside The Magazine |
The castly
thing: This is the Magazine. It was built in the 14th century as a decorative
gateway to the castle, and was lived in, rather than used for defence.
It is called the magazine because it was used to store arms during the
English Civil War. It is made of Millstone Grit, and probably has the
original chisel marks in the stones.
Today, the
Magazine is surrounded and cut off by Leicester's inner ring road. This
has definitely brought advantages to motorists and the modern users of
the city, but a heavy price has been paid in terms of loss of open space
for people and wildlife.
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