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Hunstanton Cliff Assessment

Hunstanton cliff failureExample of a medium sized cliff failure eventSince 1996, Mott MacDonald has been responsible for monitoring and reviewing past and present cliff recession rates at Hunstanton for the Borough Council of Kings Lynn and West Norfolk. This project has involved detailed analyses of cliff failure information to develop a GIS based cliff behaviour model, providing both temporal and spatial predictions for future recession rates at critical structure locations.

The Hunstanton cliffs extend for about 1.3km north from the northern end of Hunstanton promenade and are internationally recognised as a geological site of importance. The cliffs are some 18m high at their highest point, in the vicinity of Hunstanton lighthouse and coastguard station. The cliffs have historically been subjected to continued erosion by the sea and have retreated locally by up to 30m since 1885. Individual failure events can involve large volumes of material and therefore represent a significant safety concern both to the public and to cliff top amenities.

An initial study was undertaken which highlighted the failure mechanisms involved in cliff regression and estimates of future recession rates. It was following these results that Mott MacDonald was appointed to carry out further annual monitoring surveys between 1997 and 2004, which culminated in the production of a detailed review report in 2005.

Each survey covered the measurement of the line of the cliff top from a static baseline at point locations, as well as the visual observations of engineering geologists coupled with production of an annual photographic montage of the cliffs viewed from the beach. The use of both techniques meant that failures of all sizes, including those not resulting in regression of the cliff top, were recorded.

Cliff profileTypical cliff profile of Chalk, Red Chalk and Carstone depositsThis data along with cliff top recession information from historical maps and plans were compiled onto a computerised geographical information system to support the spatial and temporal assessment presented in the review report. The review report was able to achieve the following objectives:

  • Presentation of the spatial and temporal distribution of failure types through cliff behaviour zone mapping and a reassessment of the regression analyses
  • Assessment of the sensitivity of the cliff system in relation to environmental changes, sediment input/output and the influence of man
  • Development of a revised model of predicted
    cliff regression, particularly with reference to elements at risk
  • Assist the Council in understanding, with more certainty, the timescale within which mitigation measures would have to be implemented to prevent loss of properties and other assets to the rear of the cliffs.
A particular success of this project was the collection and analysis of high resolution cliff behaviour data which enabled predictions of future recession rates to be developed for particular locations along the cliffs.


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