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The Stiperstones is a very distinctive hill in the county of Shropshire, England. It is a quartzite ridge formed some 480 Million years ago. During the last Ice...
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The Stiperstones is a very distinctive hill in the county of Shropshire, England. It is a quartzite ridge formed some 480 Million years ago. During the last Ice Age the summit stood out above the glaciers and was subject to constant freezing and thawing which shattered the quartzite into a mass of jumbled scree surrounding several residual rocky tors. At 536 meters above sea level it is the second highest hill in the county, surpassed only by Brown Clee Hill (546 m). Stiperstones five-mile (8 km) long summit ridge is crowned by several rugged, jagged outcrops of rock silhouetted against the sky.
The Stiperstones ridge is a good place to view the upland landscape of the Shropshire Hills, particularly the Long Mynd to the east, and also gives extensive views towards the North Shropshire plain and the hills of Mid Wales
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The Stiperstones ridge is a good place to view the upland landscape of the Shropshire Hills, particularly the Long Mynd to the east, and also gives extensive views towards the North Shropshire plain and the hills of Mid Wales
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