The local geology of the Swainswick valley around Sopers Wood, in the south Cotswolds, has been investigated because of the presence of landslides since the work of William Smith in 1799. These are caused by the over-steepened topography downslope of the cap rock formed by the Great Oolite where water egresses around the plateau at the junction between the Great Oolite and the Fuller’s Earth formation and through the more permeable limestone bands within the Fuller’s Earth. Known locally as the Woolley Valley, there has been a dispute about development of green belt land.

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About this map

Name: Charlcombe topographic map, elevation, terrain.

Location: Charlcombe, Bath and North East Somerset, West of England, England, United Kingdom (51.39490 -2.41655 51.43411 -2.34405)

Average elevation: 131 m

Minimum elevation: 17 m

Maximum elevation: 235 m

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Number 1 (Bathwick Lodge) is a 2-storey villa with a steep Mansard room, built in 1825, extended in 1840 and the late C19. Probably by John Pinch the Elder.[4] Number 2 is from the early 19th century and has shutters over the windows.[11] Number 3 includes a porch which is elaborately enriched with carving,…

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