of the Potteries (Stoke-on-Trent)
and Churnet Valley:
Characteristics at the end of the 20th Century.
of North Staffordshire:
Showing coal and clay deposits, faults and waterways.
of subsidence in Stoke-on-Trent
There is large scale subsidence in the city - equivalent to that experienced in earthquake zones. This is caused by the collapse of mining workings.
Structure of Stoke-on-Trent:
The City of Stoke-on-Trent is formed from an amalgam of towns and villages that have expanded and merged.
List of all areas of interest in and around the city.
questions/comments/contributions? email: Steve Birks