Boundary stone on the south bank of Rising Brook, approximately 75 metres south east of Dutton's Pool is a Grade II listed building in the Cannock Chase local planning authority area, England. First listed on 21 February 2011. Boundary stone.
Boundary stone on the south bank of Rising Brook, approximately 75 metres south east of Dutton's Pool
- WRENN ID
- grey-kitchen-thistle
- Grade
- II
- Local Planning Authority
- Cannock Chase
- Constituency
- Cannock Chase MP: Josh Newbury (Lab)
- Country
- England
- Date first listed
- 21 February 2011
- Type
- Boundary stone
- OS grid reference
- SK 030 170
- Coordinates
- 52.75104, -1.9567
- Source
- Historic England listing
Description
A boundary stone dating from the late 18th or early 19th century is located on the south bank of Rising Brook, approximately 75 metres south east of Dutton's Pool. The stone is constructed from local stone and is rectangular in plan, with a rounded top. It is roughly hewn and noticeably weathered, particularly on its west face, which is oriented downstream. A diagonal fissure is visible across the west face, extending also to parts of the south and east faces, likely caused by a hole created in the centre of the east face. The stone forms a pair with another boundary marker on the opposite bank of the brook, though they face in different directions. This stone is associated with the historic nail-making industry of Slitting Mill, which operated alongside the Rising Brook. It marks part of the historic boundary between the parishes of Rugeley and Horton, established in the late 18th and early 19th centuries, and is one of a pair of markers positioned on either side of the brook. It retains its original location, illustrating the administrative development of the region, and possesses group value with the other surviving boundary stone.
Local climate
Boundary stone on the south bank of Rising Brook, approximately 75 metres south east of Dutton's Pool receives an average of 820 mm of rain a year. This makes it wetter than 52% of listed buildings in the UK. Its exposure to wind-driven rain is lower than that of 68% of listed buildings.
It experiences an average of 40 freeze-thaw cycles a year, more than 77% of listed buildings. Of these, 21 follow at least 1 mm of rain in the preceding 48 hours. Average temperatures at this location have risen by 0.3°C per decade since 1991.
Averages for 1991–2020; temperature trend 1991–2025. Figures describe the wider area (a grid cell of roughly 10 km), not the individual site. Contains modified Copernicus Climate Change Service information 2026.
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