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Lizzie Dripping 'Twiglets'
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Angular unconformity at Horton-in-Ribblesdale
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Coastal erosion near Skipsea, East Yorkshire.
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Beningbrough Hall - Rhubarb Chard 1
Beningbrough Hall - Rhubarb Chard 2
Beningbrough Hall - unknown flower 2
Beningbrough Hall - White Cornflowers 1
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Beningbrough Hall - unknown flower 3
Beningbrough Hall - Californian poppies
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Beningbrough Hall - Walled Garden path
Beningbrough Hall - Gatehouse 1
Beningbrough Hall - wild flower verge 2
Beningbrough Hall - White Cornflowers 2
Beningbrough Hall - unknown flower 1
Beningbrough Hall - Rhubarb Chard 3
Drinking basin 32 near Stanage End
Drinking basin 8 near High Neb on Stanage Edge
Drinking basin 14 on Stanage Edge
Drinking basin 24 near Stanage End
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Lizzie Dripping at Holmfirth Folk Festival
Spurn Point and the Humber Estuary
Pig Dyke Molly dancing in Harrogate
Dancing at Keighley Station
April shower over Rud Hill
1/100 • f/9.0 • 10.0 mm • ISO 200 •
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Grouse drinking basin 22, Stanage Edge, Yorkshire
Originally uploaded fro the Guesswhere UK group.
This is one of many numbered grouse drinking basins dating from the early 20th century carved into gritstone slabs on the northern part of Stanage Edge in the Peak District. Most are beautifully carved with strategically designed feeder grooves to channel rainwater into the basin.
More information here:
www.sheffield.ramblers.care4free.net/SCW historical notes.htm
"They are a product of local grouse-moor management, and were carved all over nearby Hallam Moors from 1907 onwards at the request of the owner, William Wilson, with the purpose of providing drinking troughs for the grouse. There are 108 in total, and the first ones carved are near Stanage Pole."
The Yorkshire/Derbyshire county boundary runs along the extremity of Stanage Edge in its northern part. This stone basin is in Yorkshire - just. A few metres to the west (right) is the gritstone edge and Derbyshire.
Stanage Edge is comprised of Rivelin Grit (aka Chatsworth Grit), Namurian age, Upper Carboniferous. The coarse-grained gritstone was deposited in a series of delta distributary channels. The gritstone is normally strongly cross-bedded.
This is one of many numbered grouse drinking basins dating from the early 20th century carved into gritstone slabs on the northern part of Stanage Edge in the Peak District. Most are beautifully carved with strategically designed feeder grooves to channel rainwater into the basin.
More information here:
www.sheffield.ramblers.care4free.net/SCW historical notes.htm
"They are a product of local grouse-moor management, and were carved all over nearby Hallam Moors from 1907 onwards at the request of the owner, William Wilson, with the purpose of providing drinking troughs for the grouse. There are 108 in total, and the first ones carved are near Stanage Pole."
The Yorkshire/Derbyshire county boundary runs along the extremity of Stanage Edge in its northern part. This stone basin is in Yorkshire - just. A few metres to the west (right) is the gritstone edge and Derbyshire.
Stanage Edge is comprised of Rivelin Grit (aka Chatsworth Grit), Namurian age, Upper Carboniferous. The coarse-grained gritstone was deposited in a series of delta distributary channels. The gritstone is normally strongly cross-bedded.
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