Boundary stone on the north 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 north bank of Rising Brook, approximately 75 metres south east of Dutton's Pool
- WRENN ID
- under-baluster-mint
- 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
- 52.75113, -1.95669
- Source
- Historic England listing
Description
This is a late 18th and early 19th century boundary stone situated on the north bank of Rising Brook, approximately 75 metres south east of Dutton’s Pool, near Rugeley. The stone, constructed of local stone, is rectangular with a rounded top. The south face displays some tool marks in the centre, and the stone is roughly hewn, especially on its broader south face. The broader faces are oriented towards and away from the stream.
The stone is one of a pair marking the boundary along the Rugeley and Horton parish border, which follows the course of Rising Brook. An embankment was created alongside the brook in 1809. The area, historically known as Slitting Mill and Stonehouse, was a centre for nail making, specifically involving mills and forges producing iron nails for ironworks in the Cannock Chase area. Iron bars were flattened and 'slit' into rods. The hamlet was in operation under Walter Chetwynd before 1646, with documented milling and forging continuing through the 18th and 19th centuries. Although the stones are not depicted on any historic or modern maps, they retain their original locations. The stone has group value with another surviving boundary stone located on the opposite bank of Rising Brook, which faces in a different direction.
Local climate
Boundary stone on the north 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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