Alport Castles
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One of the outcrops known as "The Tower"
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 Alport Castles
 Alport Castles shown within Derbyshire |
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| Coordinates | 53°25′15″N 1°47′18″W / 53.4209°N 1.7884°WCoordinates: 53°25′15″N 1°47′18″W / 53.4209°N 1.7884°W |
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The Alport Castles are a landslip feature in the Peak District National Park in Derbyshire. At over half a mile long, it is thought to be the largest landslide in the United Kingdom. The name "castles" comes from the debris from the landslide, which has produced several protruding grit-stone mounds which tower over the valley and appear from the distance to look like castles. Viewed from a distance the largest of these, the "Tower", resembles a full-scale motte and bailey castle.
The Alport Castles are situated on the Eastern side of the River Alport Valley, and is part of the National Trust's High Peak Estate; they lie north of the Snake Pass and north west of Ladybower Reservoir.
300 million years ago, the broad area was part of a river delta that flowed into the sea which covered the area now known as the Peak District. The deposits from the ocean are structured such as the finest material travel the furthest and are deposited in the deep ocean as black shales. Further deposits accumulate on the slopes of the oceans and collapse resulting Turbidite deposits. Further turbidite flows erode into previous ones resulting in the type of deposit which is seen at Alport Castle. As the delta progrades (mouth of the river moving further out to sea), the deposits become coarser. For the Peak District this coarse material is the Gritstone which caps topographic highs around the area and protects them from erosion.
The exact cause of the landslide is unknown, but similar if less dramatic landslips occur all around the Dark Peak, notably on Mam Tor.
One theory is that the river eroded the softer layers, causing the landslide.
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Wikipedia