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Pedrocut's photos
Handsome horse in field near Pipehay Farm
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Well at Draycott in the Clay
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"While cover waters here ye drink Rest not your thoughts below Look to the sacred sign and think Whence living waters flow."
We settled for a cup of tea on the bus seat opposite!
"St. Augustine's is a lovely little black & white,…
View towards the Church of St. Werburg at Handbury…
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"St. Augustine's is a lovely little black & white,…
"St. Augustine's is a lovely little black & white,…
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Stubby lane nearing the A515
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Detached house in Stubby Lane near Draycott in the…
Gathering silage near Marchington Cliff
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House at Marchington Cliff
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View from the edge of Banktop Wood
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A small working water wheel near Cliff Farm
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Near Cliff Farm we took a wrong turning, but it was worth it to see this small working waterwheel.
The river Dove below the Stepping Stones in Doveda…
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Path down Lin Dale towards the River Dove
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We had travelled this path nearly 17 years earlier in August 1989, for a picture see here...
www.ipernity.com/doc/2254674/49364238/in/album/1251472
Approaching Lin Dale with Thorpe Pasture to the ri…
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Track leading up to Hamston Hill
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We had travelled this path nearly 17 years earlier in August 1989, for a picture see here...
www.ipernity.com/doc/2254674/49364234/in/album/1251472
Looking up to Thorpe Cloud from the road at Thorpe
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Thorpe Cloud (left)
The limestone that forms the White Peak was formed about 325 million years ago when it was placed a few degrees south of the Equator and a tropical lagoon. Reefs were mostly formed from corals and they became pure white limestone. Reefs were mostly found in a fringe or barrier around the lagoon. A good example of a barrier reef is the hill behind Castleton on which Peveril Castle was built. There is reef limestone in Middleton Dale and in the Dove Valley, where Thorpe Cloud and Parkhouse Hill stand as isolated reefs
Church of St Leonard at Thorpe
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