Geological Sites | Leeds
| Bradford | Calderdale
| Kirklees | Wakefield
STATUS: RIGS
OTHER DESIGNATIONS: SSI
COUNTY: West Yorkshire
DISTRICT: Kirklees
OS Grid Square SE 1810
OS 1:50,000 Landranger 110 Sheffield and Huddersfield
OS 1:25,000 Explorer 288 Bradford and Huddersfield
BGS 1:50,000 Sheet 86 Glossop
FIRST DESIGNATED by West Yorkshire RIGS Group in 1996
DATE OF MOST RECENT SURVEY Winter 2004 by West Yorkshire RIGS Group
SCIENTIFIC INFORMATION produced by Ian Chisholm
SITE DESCRIPTION:
The woods cover a steep-sided clough cut by Stone Wood Dike, which rises
near Fulstone and joins Shepley Dike in Thunderbridge. The woods contain
some exposures of solid rock, particularly along the stream bed to
the west of Stone Wood Lane.
Upper Carboniferous Greenmoor Rock is found in the stream beds and shows
gentle folding in places. Most of the stream bed is incised into shales
and silts, which in some places dip at steep angles. The spring line
on the eastern side of the clough marks the junction between the Grenoside
sandstone, which forms the dip slope on which Shepley stands, and the
underlying shales.
HISTORICAL ASSOCIATIONS:
Fireclay workings are recorded in the Holmfirth Memoir written in 1933
and at least one old quarry is clearly seen at (SE 1840 1018). There
are several walled tracks which lead into the wood and may have been
tracks for hauling fireclay or flagstones, which are exposed in the
stream bed in the upper section of Stocks Wood.
EDUCATIONAL IMPORTANCE:
The site has limited value for school groups because there are steep
and muddy footpaths in the woods and access to the stream bed is not
easy. However for small groups of adults, there are interesting and
varied exposures along the stream on either side of the Stone Wood
Lane bridge.
ACCESS AND SAFETY:
Parking for 3 or 4 cars is available on either side of the Stone Wood
Lane bridge. There are many footpaths through the woods, which allow
access to most of the localities, though many of them are covered with
leaves and vegetation in the summer. The stream bed localities at the
east end of the woods are hard to access, as the stream flows in a
steep incised valley.
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