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The Long Mynd is a heath and moorland plateau that forms part of the Shropshire Hills in Shropshire, England. The high ground, which is common land and designated as an Area of Outstanding Natural Beauty , lies between the Stiperstones range to the west and the Stretton Hills and Wenlock Edge to the east.
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View from below the Stiperstones looking NE towards the Hollies. The Shropshire Hills are a dissected upland area and one of the natural regions of England. They lie wholly within the county of Shropshire and encompass several distinctive and well-known landmarks, such as the Long Mynd, Wenlock Edge, The Wrekin and the Clees.
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The principal tributary of the Quinny is the Byne Brook, which flows through Ape Dale at the foot of Wenlock Edge.Its source is near Rushbury, where it is known as Lakehouse brook, and it is also known as Eaton brook as it passes the village of Eaton-under-Heywood.
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The Longmyndian Supergroup is a 6,000-metre-thick (20,000 ft) sequence of Ediacaran (late Precambrian) rocks that outcrop between the Pontesford–Linley Fault System and the Church Stretton Fault System in the Welsh Borderland Fault System of England and Wales. [1]