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A view of Storrs Hill Quarry |
From the time that I alighted from the No. 126 bus in Horbury to finishing my British Listed Buildings Photo Challenge at Sowood House, I had spent just over 4 hours looking at the Church of St. Peter and St. Leonard, the historic architecture of Horbury and Ossett and the granite monuments and Commonwealth War Graves Commission headstones in Holy Trinity churchyard.
My plan for the last leg of a walk was to follow the escarpment of the Horbury Rock and then drop down to the Horbury Quarry, which is listed by the West Yorkshire Geology Trust as a Local Geological Site and has been used by the Leeds Geological Association (LGA) and other geology groups for their field trips.
After photographing Sowood Farmhouse, I followed the public footpath path across a field and was interested to see Rock House (c.1881), which although not a listed building has its roofline dominated by large Dutch gables on each elevation and Tudor style chimney stacks.
The house was built for George Harrop, who made his fortune in woollens manufacturing and owned the Albion Mills at nearby Horbury Bridge. His son John, one of 10 children, is buried with other members of his family at Holy Trinity church in Ossett.
Following the badly eroded path as it dropped down the escarpment, I noticed a very small exposure of flaggy Horbury Rock but, not having my Estwing hammer with me to break off a small piece, I didn’t try and obtain a specimen.
Turning sharply to the south-east, I was very surprised to see the expensive exposure of the Horbury Rock in the old Storrs Hill Quarry, which for some strange reason I had not noticed when undertaking online research for my day out using various maps.
When looking through various websites on the history of Ossett, it is asserted that stone from this quarry was used to build Sowood Farmhouse and for the rebuilt but since demolished Holy Trinity church in Market Place. Zooming in to the photo that I took of Rock House, the sandstone used for the rear of the house, at least, looks like it has probably come from this quarry.
Access to the quarry face was prevented by a sturdy fence topped with barbed wire and I only took a few general photos from a distance. LGA had visited the quarry back in 2016 and the field report refers to the well developed cross-bedding, which is considered to be indicative of a low energy braided river system.
The general physical characteristics of colour and texture could be clearly seen and many parts of the exposure exhibit pronounced orange iron staining. As I have seen in many exposures of Pennine Coal Measures Group (PCMF) sandstones, the lower sections are composed of thick massive beds, with flaggy beds in the upper parts.
This change in bedding reflects differences in the flow regime between the lower and upper parts of the river channel in which the sandstone was deposited. The flaggy beds have been subjected to surface physical and biological weathering that lead to the formation of the soil profile.
Looking on old Ordnance Survey (OS) maps, it can be seen that there is a substantial quarry face to the north side of the path from Sowood Farmhouse, with the area to the south of the section of the path along which I had been walking shown as large mounds of waste rock, which are now thickly covered in gorse.
Although a brief description accompanies a photo of graffiti in the Ossett Picture Gallery, I haven’t seen any documentation that records the history or production at this quarry, but it seems to have been quite substantial and I presume that many buildings in Ossett were built with this stone.
Continuing past the boundary wall to Rock House, I came to a small exposure of flaggy Horbury Rock exposed beneath waste rock, where I was able to obtain a loose piece of sandstone and break it into smaller pieces by smashing it against the outcrop.
Except for the lack of feint iron banding, the fine grain size and muddy grey brown colouration are essentially identical to the specimen of sandstone that I had retrieved from a section of an old dilapidated boundary wall in Horbury.
Stopping briefly to take in the panoramic view across the lower Calder Valley, with the gently undulating landscape underlain by PCMF strata, which included the Emley Moor transmitting station in the distance, I carried on down the path to Jenkin Road.
I stopped briefly to photograph the Grade II Listed early C19 Jenkin House, with its elegant 2-storey bow windows, before looking for the public footpath down to Horbury Quarry. I saw a snicket that seemed to coincide with the position of the footpath as marked on my copy of the 1:25,000 scale OS map, but I didn’t see the usual distinctive green signpost at its start.
Since arriving in Horbury, I had been on the constant move for 4½ hours and had walked over 8 km. Although it was still only 2:30 pm, I had managed to see a good exposure of the Horbury Rock and decided that I had done enough on my day out to Horbury and Ossett. After photographing another substantial boundary wall, I then slowly walked up Jenkin Road to High Street, where I caught the No. 126 bus back to Wakefield.