Salt Subsidence Topography, Cheshire This undulating topography on the otherwise very flat Cheshire Plain near Wade's Green Hall between Winsford and Nantwich is caused by dissolution of the underlying Triassic salt horizons at what is known as "Wet Rockhead".
Salt Subsidence Topography, Cheshire This undulating topography on the otherwise very flat Cheshire Plain near Wade's Green Hall between Winsford and Nantwich is caused by dissolution of the underlying Triassic salt horizons at what is known as "Wet Rockhead".
Freshly mown grass. Looking across farmland in Cheshire! In the distance is Boundary Wood, and just in front of the wood is the River Weaver.
Marlpit at Paradise Farm. Typical mid-Cheshire pond which supports a wide variety of wildlife.
The White House adjacent to Nanneys Bridge. One mile South from the village centre

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