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The Stiperstones is a 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 above sea level it is the second-highest hill in the county, surpassed only by Brown Clee Hill (). Stiperstones' summit ridge is crowned by several rugged, jagged outcrops of rock silhouetted against the sky. ==Geography== The Stiperstones is noted for its tors of quartzite. The principal ones are named as follows, from north-east to south-west: * Shepherd's Rock () * Devil's Chair () * Manstone Rock () * Cranberry Rock () * Nipstone Rock () * The Rock () Manstone Rock is the highest of these at , and is topped with a trig point. The Devil's Chair is the largest and best known. 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. 抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)』 ■ウィキペディアで「Stiperstones」の詳細全文を読む スポンサード リンク
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