The Rush

This linear site, which is called The Rush on the 1:25000 Ordnance Survey map, is on a steep slope with a south-westerly aspect. The lower break of slope is at about 20m above mean sea level rising to 45m at the top. The site is approximately 100-120m wide. The Rush is one of a series of fields on a band of Lower Jurassic oolitic limestone which extends in a north-south direction from just north of North Cliffe to Hotham Hill in the south.

Resources available for this area are as follows: