Southwell landslip has a deep natural cleft caused by slippage with an eastward leaning mass. There is some evidence of quarrying on top of this mass on the seaward side. No obvious marks in a small quarry. Evidence of coastal quarrying is visible as earthworks on aerial photographs of 1968.
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Southwell landslip has a deep natural cleft caused by slippage with an eastward leaning mass. There is some evidence of quarrying on top of this mass on the seaward side. No obvious marks in a small quarry. (1)
Evidence of coastal quarrying in the area of Southwell landslip, described above in (1-3), is visible as an earthwork on aerial photographs of 1968. The quarrying is visible over an area measuring approximately 140 m by 65 m. (2) This site was digitally plotted during the South West Rapid Coastal Zone Assessment Survey (Dorset).
Sources/Archives (2)
<1> SDO10260
Unpublished document: AC Archaeology. 2002. The Isle of Portland Review of Mineral Planning Permissions Stage 1: archaeological baseline study for Hanson Bath & Portland Stone, document no. 4299/1/4..
<2> SDO13065
Aerial Photograph: Meridian Air Maps Ltd. 26-JAN-1968. MAL 68002/011-12.
Centred SY 6945 7061 (120m by 133m) (3 map features)
Map sheet
SY67SE
Unitary Authority
Dorset
Protected Status/Designation
None recorded
Other Statuses/References
None recorded
Record last edited
Dec 3 2013 3:21PM
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