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Ratlinghope

Civil parishes in ShropshireUse British English from October 2013Villages in Shropshire
Ford, Ratlinghope geograph.org.uk 1112765
Ford, Ratlinghope geograph.org.uk 1112765

Ratlinghope (, locally also RAT-chəp) is a hamlet and civil parish in Shropshire, England. The population of the civil parish at the 2011 census was 138. It is situated four miles (6 km) west of Church Stretton and twelve miles (19 km) south of Shrewsbury. Historically it was located in the hundred of Purslow. In the Church of England it is in the rural deanery of Bishop's Castle, archdeaconry of Ludlow, and diocese of Hereford. The village is scattered around a valley in the hills of the Long Mynd and Stiperstones, an AONB (area of outstanding natural beauty). Nearby is the hamlet of Bridges, which falls within Ratlinghope civil parish, and where there is a youth hostel and a public house. Castle Ring, the earthwork of Ratlinghope Hill, is the fort described by Mary Webb in her novel Golden Arrow.

Excerpt from the Wikipedia article Ratlinghope (License: CC BY-SA 3.0, Authors, Images).

Ratlinghope
Shrewsbury Road,

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Latitude Longitude
N 52.566 ° E -2.883 °
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Shrewsbury Road
SY5 8DS
England, United Kingdom
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Ford, Ratlinghope geograph.org.uk 1112765
Ford, Ratlinghope geograph.org.uk 1112765
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Longmyndian Supergroup

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. The supergroup consists of two major geological groups, the Stretton Group and the overlying Wentnor Group. The successions represented by these two groups have also been referred to as the Eastern Longymndian and Western Longmyndian respectively, forming as they do the bedrock of the east and west parts of the Long Mynd in Shropshire. The rocks are a generally regressive sequence from basinal facies to clastic sedimentation. The rocks are thought to be derived from Uriconian mountains that were formed during the southward subduction of an oceanic plate beneath a continental block (ocean closure). The rocks have since been folded due to fault movements and plunge gently to the south. The Longmyndian rocks were deposited in northeast–southwest trending faulted rift basins. These were deposited on top of the Uriconian volcaniclastic deposits. Subsequent ocean closure squeezed these rocks together to provide sub-vertical bedding in the synclinal sequence seen in exposed rocks today. The deposited rocks of the Longmyndian show a variety of depositional facies that tell a story of ocean closure. The Longmyndian deposits rest upon Uriconian rocks but different sections are exposed exclusively between the Church Stretton Fault and the Pontesford-Linley Lineament.